1A01 Spontaneous fission measurements for nuclei around neutron-rich Fm region
produced by using an 254Es target
ASAI, M.1, TSUKADA, K.1, HIROSE, K.1, TOYOSHIMA, A.1, TOMITSUKA, T.1, CHIERA, N.
M.1, ITO, Y.1, MAKII, H.1, NAGAME, Y.1, NISHIO, K.1, ORLANDI, R.1, RATHA, K. K.1, SATO,
T. K.1, SUZUKI, H.1, TOKOI, K.1, VERMEULEN, M. J.1, YANAGIHARA, R.1, NISHINAKA,
I.2, KAMADA, H.3, SHIBATA, M.3, GOTO, S.4, HIROSE, H.4, HAYASHI, H.5, SAKAMA, M.6(1JAEA, 2QST, 3Nagoya Univ., 4Niigata Univ., 5Kanazawa Univ., 6Tokushima Univ.)
Spontaneous fissions of the nuclei around neutron-rich Fm region, 256Fm, 258Fm, and 259Lr, havebeen measured using an 254Es target at the JAEA Tandem Accelerator Facility. These three nuclei
show different fission properties: the asymmetric fission, the high total-kinetic-energy (TKE)symmetric fission, and the low TKE symmetric fission. The mechanisms of these three fissions
should be very different, and it is of great interest to elucidate how these differences occur. We
have produced 256Fm and 258Fm in multinucleon-transfer reactions with a 254Es target and 18O
projectiles, and produced 259Lr in the 248Cm(15N,4n) fusion-evaporation reaction. The reaction
products were mass-separated with a gas-jet-coupled on-line isotope separator, and weredelivered into a rotating wheel alpha- and fission-fragment detection system equipped with 4pairs of Si detectors, where the fission fragments were measured in coincidence. By comparing
the mass and TKE distributions deduced from the present experimental data, we will discuss thedifferences in fission mechanism among 256Fm, 258Fm, and 259Lr.
1A02 Formation and thermochemical properties of oxychlorides of Nb and Ta - Towards
the gas-phase investigation of the Superheavy Element dubnium (Db) oxychloride.
CHIERA, N. M.1 、SATO, T. K.1 、ASAI, M. １ 、SUZUKI, H. １ , 2 、TOKOI, K. １ , 2 、
TOMITSUKA, T.１, 3、TOYOSHIMA, A.１、TSUKADA, K.１, NAGAME, Y.１, 2(1JAEA, 2Ibaraki Univ., 3Niigata Univ.)
The adsorption of single molecules (i.e., tracer-amount scale) of NbOCl3 and TaOCl3 on quartz
surfaces was explored by applying an isothermal gas-chromatographic method. Thermochemical
information was obtained, in good agreement with literature data. The future accomplishment ofcomparative studies with DbOCl3 under the same experimental conditions will provide a direct
information on the volatility trend in Group-5 elements, and hence, on the magnitude ofrelativistic effects on dubnium’s electronic structure.

1A03
Development of a slow atomic beam source for Superheavy elements
TOMITSUKA, T.1,2, TOKOI, K.1,3, SATO, T. K.1, ITO, Y.1, SUZUKI, H.1,4, ASAI, M.1,
TSUKADA, K.1, TOYOSHIMA, A.1, CHIERA, N. M.1, GOTO, S.2, NAGAME, Y.1,3(1ASRC, JAEA, 2Graduate School of Science and Technology, Niigata Univ., 3Graduate School of
Science and Engineering, Ibaraki Univ., 4College of Science, Ibaraki Univ.)
In order to experimentally determine the ground state electronic configurations of Superheavy
element atoms, we have developed a slow Atomic Beam Source (ABS) using a high-temperaturenozzle type cavity. In this study, we conducted an off-line experiment using stable isotopes of Cd
to examine the extraction of the Cd beams. A symmetrical beam distribution with respect to theatomic beam edge was obtained. The obtained results, together with Monte-Carlo simulations foratomic beam profiles, will be presented.
1A04 The Study on Carbonyl Complexes of Group VII Elements
WANG, Y.1,2, QIN, Z.2, FAN, F.2, CAO, S.2, ZHANG, J.2, YANG, J.2, HABA, H.1, KOMORI, Y.1,
YOKOKITA, T.1, MORIMOTO, K.1, KAJI, D.1(1 Nishina Center for Accelerator-Based Science, RIKEN, 2Institute of Modern Physics, Chinese
Academy of Sciences)
Towards chemical characterization of the superheavy element bohrium (Bh), experiments withlighter its homologues Tc and Re are necessary to be investigated in advance. Online gas-phasechemistry study with single-atom quantities of Tc and Re carbonyls were carried out at RIKEN
and IMP. Short-lived Tc and Re isotopes were produced via the spontaneous fission of 252Cf andthe natGd(23Na,xn)172-177Re reactions, respectively. Volatile carbonyls of Tc and Re weresynthesized and their gas-phase properties were systematically studied using an online lowtemperature isothermal chromatography. For both Tc and Re carbonyls, the adsorption enthalpies
on the Teflon surface were about ΔHads = –43±1 kJ/mol, and the highest relative chemical yieldsof about 25% were measured. Moreover, the laser-ablation time-of-flight mass-spectrometry
technique was employed to deduce the species of the Re carbonyls formed with a small amount of
stable Re atoms and CO gas in the gas phase. Combined with density functional theory
calculations, for mononuclear Re carbonyls, the most stable species were suggested to be thecarbonyls with the coordination number of 6 and 5 for Re+ and Re neutral atoms, respectively.

1A06 Hydration Structure of Einsteinium by Synchrotron Radiation Based Analysis
YAITA, T.1, SUZUKI, S. 1, KOBAYASHI, T. 1, SHIWAKU, H. 1, DOI, R. 1, YAMAGAMI,
H. 2, TSUKADAS, K. 3, TOYOSHIMA, A. 3, ASAI, M. 3
(1JAEA-MSRC, 2Kyotosngyo Univ., 3JAEA-ASRC)
The ionic radii of trivalent actinide and lanthanide systematically shrink with an increase inatomic number. This tendency, namely Actinide or Lanthanide Contraction”, have been observedby the interatomic distances in oxide, the hydration bond distance and so on. Especially, a
breaking point due to hydration number change often appears in lanthanide solution system. In
contrast, regarding actinides, such a breaking point has not been observed by Cf (III); therefore,
motivation of this study is to determine the hydration bond distance of Es(III). Hydration
structure of Es(III) was determined using synchrotron radiation based EXAFS analysis. Observed
hydration bond distance of Es(III) was unexpectedly shorter than the expected from an
extrapolation up to systematic actinide contraction from U(III) to Cf(III), we could first observe,
namely “Einstein Break”. It suggests that this breaking observation strongly could correlate with
an electronic configuration in the inner core of Es(III) on the comparison with lanthanide series
result, rather than hydration number change, according to the theoretical calculation and an
estimation from atomic volume results.

1A07 Production of carrier-free RI tracer of alkali metal using bemsstrahlung
IKEDA, H.1,2, KIKUNAGA, H.2, WATABE, H.1(1Cyclotron and Radioisotope Center, Tohoku University, 2Research Center for Electron Photon
Science, Tohoku University)[Introduction] Alkali metals are very important elements for plant research. Behavior ofalkali metals in plants can be traced using carrier-free RI without affecting plant activity.
We established a method for producing K tracer (K-42, 43) by irradiation with braking
radiation and made it possible to investigate the dynamics of plants. Cesium (Cs),rubidium (Rb) and sodium (Na) tracers can also be produced by irradiation withbremsstrahlungs. In this study, we decided to individually examine the production
amount and separation condition of carrier-free alkali metal RI.
[Experiment]The CaO, BaO or SrCO3 target was irradiated with bremsstrahlung
radiation. Pure water and oxalic acid aqueous solution were added to the irradiated target
to precipitate Ca, Ba or Sr as oxalate. The supernatant was charged to a column filled withcation exchange resin. After washing with 0.01 M HCl, the alkali metal RI was eluted
with 1-1.5 M HCl.

[Results] Alkali metals coprecipitated when the target substance was precipitated wereabout 15-30%. Thus, the total chemical yields of Cs-136 and Rb-86 were about 60-80%.
We drew the elution curves of Cs-136 and Rb-86. This result suggested that Cs-136 andRb-86 could be supplied as multitracers at the same time.

1A08

Development and evaluate of the α-ToF detector for MRTOF-MSNIWASE, T.1,2, WADA, M.3, SCHURY, P.3, ITO, Y.1,4, KAJI, D.1, ROSENBUSCH, M.1,
KIMURA, S.1, MORIMOTO, K.1, HABA, H.1, ISHIZAWA, S.1,5, MORITA, K.1,2, MIYATAKE,
H.3, WOLLNIK, H.6(1RIKEN Nishina Center, 2Kyushu Univ., 3KEK, 4JAEA, 5Yamagata Univ., 6NMSU)
The atomic mass is a unique quantity for each nucleus. Precise mass measurement allows us to
identify the atomic number as well as the mass number.
Recently, we succeeded in measuring the masses of fusion evaporation products provided fromthe GARIS-II with a multi-reflection time-of-flight (MRTOF) mass spectrograph. Next
experimental plan is the measurement of the masses of superheavy nuclei (SHN) for identificationof the mass number and atomic number. In the SHN region, the expected rate of reaction products
is less than one event per day due to small reaction cross sections.
We developed an α-ToF detector to accurately distinguish a true event from large background
events such as molecular ions. The time correlation between the time-of-flight signal and α decay
signals can discriminate the background events. We have tested the α-ToF detector with an alphasource and confirmed that the correlation between the timing signal and the decay energy can be
successfully measured using the α-ToF detector.
I will talk about the result of the α-ToF detector performance test, and also about the future
experimental plan with our MRTOF devices for simultaneous mass and decay-property
measurements.
1A10 Compton Camera(ETCC) imaging experiment using technetium isotopes.
HATSUKAWA,Y.1, HASHIMOTO,K.1, KABUKI, S.2, KUSHIDA2, J., TSUKADA,K.3, ASAI,
M.3, TOYOSHIMA, A.2, NISHIJIMA, K.2, KUNIEDA, E2.
(1QST, 2Tokai Univ., 3JAEA)

Technetium-99m is used in radioactive medical diagnostic tests, for example as aradioactive tracer that a nuclear medicine gamma camera can detect in the human body.
It is well suited to the role because it emits readily detectable 141 keV gamma-rays, andits half-life is 6.01 h (meaning that about 94 % of it decays to 99Tc in 24 h).
In recent years, the Compton camera which is originally developed for the astrophysicalstudies was applied for medical diagnostic usage. For the Compton camera imaging
require technetium isotopes emitting higher energy gamma-rays. A Tc isotope, 95Tc (T1/2= 20 h; Eγ = 765.8 keV) is a candidate for tracer of the Compton camera imaging.
In this study, Technetium-95 was produced by the natMo(p,n)95Tc reaction. The feasibility
study of Compton camera imaging using gamma rays emitted from 95Tc was carried out.

1A11 Calculation of Nuclear Reaction Cross Section in In-Flight Muon Catalyzed Fusion
Cycle
KINO, Y. 1,2, YAMASHITA, T. 1, SATO, M. 2
(1Department of Chemistry, Tohoku University, 2Faculty of Engineering, Chubu University2)
The muon catalyzed fusion (µCF) has been expected to be a new energy source andmono-energetic neutron source. In the µCF, a muonic molecule formation is a rate determining
process, and the obtained energy from the nuclear fusion reaction cannot exceed the energy formuon production. We newly propose an in-flight muon catalyzed fusion (IFµCF) cycle which
avoids the rate determining process. In the IFµCF cycle, nuclear fusion reaction occurs duringmuon atomic collisions.
In this study, nuclear fusion reactions (dµ + t → α + n + µ + 17.6 MeV, d↔t) are calculatedwith a non-adiabatic coupled channel method [1]. The nuclear reaction cross sections are morethan three orders of magnitude higher than typical cross sections used in the thermonuclear fusion
study, but the temperature in the IFµCF is one order of magnitude lower than the thermonuclear
fusion. Thus, if a high intensity muon beam is obtained, the IFµCF can be maintained by
self-ignition.
[1] E. Hiyama, Y. Kino, M. Kamimura, Prog. Part. Nucl. Phys. 51, 223 (2003)
1A12 Development of a retarding-field magnetic-bottle electron spectrometer andmeasurements of the internal conversion electrons from U-235m (JNRS)SHIGEKAWA, Y.1, KASAMATSU, Y.1, YAMAKITA, Y.2, YASUDA, Y.1, KONDO, N.1,
WATANABE, E.1, SHINOHARA, A.1(1Graduate School of Science, Osaka University, 2Graduate School of Informatics andEngineering, The University of Electro-Communications)
As 235mU and 229mTh have extremely low excitation energies, the nuclei interact with outer-shellelectrons in the internal conversion (IC) process. Therefore, the half-lives of these nuclides varydepending on the chemical environments. We are aiming to elucidate the deexcitation process of
235m

U and 229mTh by measuring the IC electron energy spectra in addition to the half-lives forvarious chemical environments. In order to precisely record the IC electron energy spectra ofthese nuclides, high detection efficiency as well as high energy resolution is required for the
spectrometer. In this work, we designed and fabricated a retarding-field magnetic-bottle electron
spectrometer. Moreover, we evaluated the collection efficiency of electrons to the channeltron
detector under various magnetic fields. It was found that the collection efficiency of electrons
becomes 100% on the appropriate magnetic condition. Next, the half-lives and the energy spectraof 235mU were measured for 235mU on the surface of Cu and for 235mU that reacted with HF or HCl

gas. With the high detection efficiency of this magnetic-bottle spectrometer, we were able tomeasure the half-lives and the energy spectra with high S/N and energy resolution. Especially, weclearly observed the difference of the half-lives and the energy spectra between 235mU that reactedwith HCl gas and 235mU on the surface of Cu.

1B01 Existence forms of radiocesium in waters from river systems in Hama-Dori area inFukushima Prefecture, JapanNAGAO, S.1, YAMAGISHI, E.2, MOROKADO, T.2, SHIMAMURA, A.3, TOMIHARA, S.3,
OCHIAI, S.1(1INET, Kanazawa Univ., 2College of Science and Engineering, Kanazawa Univ., 3Aquamarine
Fukushima)
Nuclear accident at the Fukushima Daiichi Nuclear Power Plant occurred after the 2011
Tohoku Earthquake and Tsunami. To estimate the impacts of radiation dose to human health, it isimportant to understand dynamics of radionuclides, especially 134Cs and 137Cs, in river watershedenvironments. The aim of this study is to investigate radioactivity of 134Cs and 137Cs in river
systems in Fukushima Prefecture, and discuss with the transport of radiocesium from the surface
soil to the river waters. The 20-100 L of river water samples were collected at monitoring stations
in five river systems (Abukuma River, Niida River, Iwasawa River, Kido River and Natsui River)in Hama-Dori area from Fukushima Prefecture during 2015-2017. The 134Cs and 137Cs wereseparated by co-precipitation with AMP and measured by gamma-ray spectrometry using low
BKG Ge detectors at the Low Level Radioactivity Laboratory, Kanazawa University. The
particulate phase of 137Cs ranged from 54% to 92% for the river waters from the Abukuma, Niida,
Kido and Natsui River. On the other hand, the Iwasawa River has less than 10% for the waters
with higher conductivity and DOC concentration. This indicates watershed condition is important
to existence forms of radiocesium in the Fukuhsima river waters.

B02 Seasonal variation of the activity concentration of radioactive cesium in sediment
sampled at Tamagawa River Watershed
AKIYAMA, M.1, HAGIWARA, K.2, KOIKE, Y.2(1 Grad. Sch. of Sci. and Tech., Meiji Univ., 2 Sch. of Sci. and Tech., Meiji Univ.)
Monitoring of radioactive cesium is crucial for investigation of activity distribution andvariation tracing of radioactive substances. In this study, radioactive cesium in sediments
sampled at 45 points in Tamagawa River watershed, concluding main and tributary stream, were
determined for behavior analysis of radioactive cesium at low dose areas. In the mainstream at
Tamagawa River watershed, the activity concentrations of radioactive cesium in sediment
sampled at downstream were higher than that at upstream and midstream. On the other hand, theconcentrations of radioactive cesium in sediment sampled at Nogawa river, Hirase river, andNikaryo carnal were high compared to the mainstream. The flow rate of the tributaries at
Tamagawa River Watershed is slower than that of the mainstream. These results indicated that theactivity concentration of 137Cs in sediment increased by locally accumulating 137Cs in slowly
flowing river water.

1B03 Contribution of groundwater discharge to bottom water of Nanao West Bay basedon 222Rn horizontal distribution.
FUJITA, A.1, NAGAO, S.2, OCHIAI, S.2, SUGIMOTO, R.3,MATSUNAKA, T.2, M. Charette4,
P. Henderson 4(1Graduate School of Natural Science and Technology, Kanazawa Univ., 2Institute of Nature andEnvironmental Technology, Kanazawa Univ., 3Reseach Center for Marine Bioresources, Fukui
Prefectural Univ.,

4

Department of Marine Chemistry and Geochemistry, Woods Hole

Oceanographic Institute)
Biological production is more active in coastal areas than open sea because large amount of
nutrients from terrestrial areas are carried by rivers. On the other hand, contribution of nutrientsfrom groundwater to coastal areas is also important, but identification of submarine groundwater
discharge (SGD) is tedious work. Many scientists have been using 222Rn to specify thecontribution of groundwater. 222Rn is a daughter nuclide of 226Ra, water-soluble and noble gas.
The sedimentary layer is rich in 238U and 226Ra which belong among Uranium series, so theconcentration of 222Rn is higher in groundwater than surface water. Moreover 222Rn has a half‐life of 3.83 days and is used to specify the contribution of groundwater with short residence time.
In this study, research was carried out at Nanao West Bay in October of 2017 and April and Julyof 2018. In October of 2017, the higher concentration is observed at the center-east area in thebay. But the higher concentration site is detected at the southwest area in April of 2018 and are
the northeast and southwest areas in July of 2018. It is necessary to continue the survey to grasp
the actual condition of SGD through the year.
1B04 Evaluation of Analytical Method forInterlaboratory Comparison
MIURA, T.1, OTA, T.2, TERADA, A.3

210

Po/210Pb in Marine Product using(1National Metrology Institute of Japan, 2Japan Chemical Analysis Center, 3National Institute of
Public Health)Marine products such as marine fish are well known to contain 210Po at relatively highconcentrations. It is important to precisely measure 210Pb which is a substantial parent nuclideof 210Po and 210Po in marine products from the viewpoint of internal exposure dose evaluation
attributable to food. We verified the analytical method applied to the measurement of 210Po/210 Po
in food samples using a freeze-dried powder of fish meat (flounder) 5 years after collection and a210

Po solution and a 209Po standard solution separated from a commercially available metallic leadreagent. The loss of Po for each chemical separation step (acid decomposition, extraction
chromatography, measurement source preparation by electrodeposition) of the analysis method
was examined. As a result, there was no significant loss of Po in the chemical separation operation.
Therefore, as a next step, we tried to evaluate the performance of the 210Po/210Po analysis methodby conducting a interlaboratory comparison in which participate several laboratories analyze test
samples based on the standard analysis procedure document.

1B05 Elucidation for production scenario of insoluble Cs particles from Unit 1 using
multifaceted analysis
SATOU, Y.1, KOBATA, M.1, OKANE, T.1, SUEKI, K.2, MATSUO, K.2,ISHIII, K.2, Martin, P. G.3,
Scott, T. B.3(1JAEA, 2Graduate School of Pure and Applied Science, Univ. of Tsukuba, 3Interface Analysis
Centre, Univ. of Bristol)In order to disclose production process of insoluble Cs particles ejected from the Unit 1 of
Fukushima Dai-ichi Nuclear Power Station (“Type B” particles), we employed laboratory X-ray
computed tomography (Lab. CT), synchrotron-µ-X-ray tomography (XRT), and Hard X-ray
Photoelectron Spectroscopy (HAXPES). Type B particles were isolated from ground dust sample
obtained from 3km north from the Fukushima Daiichi Power Station. Type B contain bubbles inthe body and detected fragments of heavier material – steel, caesium, fuel. These elements are
spread outer side, also high-absorption area of X-ray is surrounding of the particle. Someelements such as Fe showed metallic and low oxide state using a HAXPES. Elements except
silicon in Type B were expected that impurities of source material. However, above results showsthe elements were attached on the particle during solidification process.

1B06 Quantity of trace element in insoluble particle including radioactive Cs found in
Okuma town, Fukushima prefecture by destruction analysis
IGARASHI, J.1, ZHANG, Z.1, NINOMIYA, K.1, SHINOHARA, A.1, SUEKI, K.2, SATOU, Y.3(1Graduate School of Science, Osaka University., 2Graduate School of Pure and Applied Sciences,
Tsukuba University., 3JAEA.)
Insoluble radioactive Cs particles(insoluble particles) made of mainly SiO2 were released by theaccident of Fukushima Dai-ichi Nuclear Power Plant. It was considered that the insoluble
particles were formed in the reactor during the accident. In the previous studies, the insoluble
particles can be classified to at least two types from the properties and radioactivity concentrationof Cs. In this study, the insoluble particle which was approximately 100 µm in diameter and low
radioactivity concentration of Cs was found in Okuma town, Fukushima prefecture. It wasestimated that this insoluble particle was derived from unit 2 or 3 reactor by its radioactive ratio,
134

Cs/137Cs.To investigate the formation process of this insoluble particle in the reactor, we

focused on the amount of the non-volatile element, Sr in the insoluble particle. In this study, we
dissolved the insoluble particle by the alkali fusion method and extracted Sr by the Sr-Rad Disk.
Finally, we quantified the amount of the Sr by measuring the 90Sr using the Cherenkov lightmeasurement. As a result of the analysis, it was found that the radioactive 90Sr of the insoluble
particle was approximately 0.04 Bq.

1B07 Development on the Determination Method of Radioactive Antimony and the
Obtained Distribution of Its Soil Deposition near Fukushima Daiichi Nuclear Power Plant
MIYAZAWA, N.1, UESUGI, M.2, YOKOYAMA, A.3,
(1Graduate School of Natural Science and Technology, Kanazawa University, 2Advanced Science
Research Center, Kanazawa University, 3Institute of Science and Engineering, Kanazawa
University)
A large amount of radionuclides were released into the atmosphere and deposited on soil due tothe accident of Fukushima Daiichi Nuclear Power Plant (FDNPP) in 2011. Lots of studies focusedon isotopes of cesium and iodine. However, behaviors for the other radioactive elements are notwell unknown. For such study on a nuclide of interest, we have researched for 125Sb (T1/2 = 2.75 y).
Antimony, a volatile element like cesium, is seldom reported, because the deposited amount of
125

Sb, its long-lived isotope, is relatively small and counting photons in peak area is interferedwith γ-rays from abundant radioactive cesium. In our previous study, we established adetermination method of 125Sb with a removal process of cesium by using ammonium
phosphomolybdate adsorption method or an anion exchange resin method. In this work, we
obtained the analytical results under some leaching conditions for antimony in soil, and showed
the distribution of 125Sb near the FDNPP.
1B08 Atmospheric Radiocesium Concentrations in East Japan just after TEPCO FDNPP
Accident by Analysis of Tape Filters Used at Automatic SPM Monitors.
OURA, Y.1, TSURUTA, H.2, EBIHARA, M.3, MORIGUCHI, Y.4, OHARA, T.5, NAKAJIMA., T.
6 1( Tokyo Metropolitan Univ., 2RESTEC, 3Waseda Univ., 4Univ. of Tokyo, 5NIES, 6JAXA)
We have been determining 134Cs and 137,Cs in suspending particulate matters (SPM; aerosols

less than 10 μm in diameter) collected hourly from Mar. 12 to 23, 2011 at SPM monitoring
stations in eastern Japan to reveal spatio-temporal trajectory of radioactive plumes caused by
TEPCO FDNPP accident, and the dataset for 99 monitoring stations was reported. After that,radiocesium concentrations at additional 48 stations from Aomori prefecture to Shizuoka
prefecture were determined. In Aomori prefecture, no radiocesium was detected from Mar.12 to
25. In Iwate prefecture 137Cs with max. about 4 Bq/m3 was detected at some stations on Mar.13
and 21. In Nagano prefecture, radioactive plume with 137Cs of max. about 30 Bq/m3 was observedon Mar.15 at west side of Kanto-Santi but no plume was observed at northern area on same period.
In shizuoka prefecture, radioactive plume with 137Cs of max. 0.8 Bq/m3 was observed at westernarea on Mar. 21 but was not at eastern area. It seems that the plume went through on the ocean andreach at western area.

1B09 Transfer behavior of Sr-90 from environment to cattle teeth after the Fukushima
Daiichi Power Plant accident.
KOARAI, K.1, KINO, Y.1, NISHIYAMA, J.1, KANEKO, H.1, ONO, T.1, OKA, T.1,2,
TAKAHASHI, A.3, SUZUKI, T.4,5, SHIMIZU, Y.4, CHIBA, M.4, OSAKA, K.4,5, SASAKI, K.4,
URUSHIHARA, Y.6, FUKUDA, T.7, ISOGAI, E.8, SEKINE, T.1,2, FUKUMOTO, M9. and
SHINODA, H4.
(1Department of Chemistry, Tohoku University, 2IEHE, Tohoku University, 3Tohoku University
Hospital, 4Graduate School of Dentistry, Tohoku University, 5IRIDeS, Tohoku University,
6

Tohoku University School of Medicine, 7Faculty of Science and Engineering, Iwate University,

8

Graduate School of Agricultural Science, Tohoku University, 9Tokyo Medical University)
We have investigated transfer behavior of Sr-90 from soil to cattle teeth after the Fukushima

Daiichi Power Plant (FNPP) accident. The cattle and soil were collected in Okuma town, which
was in the ex-evacuation area of the FNPP accident. The soluble fractions of the soil wereextracted by milli-Q water or 1M CH3COONH4 solution. Radio activity of Sr-90 in the samples
was determined after the chemical separation (fuming nitric acid method or Sr resin method).
Stable Sr and Ca in the samples were determined by ICP-MS or ICP-AES. Solubility of Sr-90 waslarger than those of stable Sr and Ca. The result implies that the nuclide could easily migrate fromthe soil to the teeth. The specific activity of the soluble fraction was similar to that of the teeth
developed after the FNPP accident. The result indicates that the soluble Sr-90 in the soil would be
the source of the Sr-90 in teeth. The ratio of Sr-90 to Ca of the soluble fraction was higher thanthat of the tooth. This indicates that Sr-90 was discriminated from Ca in the incorporation process.
1B10 Systematics of adsorption structure of various hard metal ions on phyllosilicates:
comparison of strontium and cesium
YAMAGUCHI, A.、KURIHARA, Y.
(Graduate School of Science, The Univ. of Tokyo)
Extend X-ray adsorption fine structure (EXAFS) spectra of some alkaline ions, alkaline earth ions,and rare earth ions adsorbed on clay minerals were obtained in this study. Theses systematic
results revealed that ions larger than barium (Ba2+) forms inner-sphere (IS) complex and smallerouter-sphere (OS) complex, during the adsorption on clay minerals. This implication is helpful toexplain and predict the behavior of various ions in environment. This study aimed to reveal local
structures of strontium (Sr) and cesium (Cs) adsorbed on clay minerals (vermiculite andmontmorillonite) and understand stabilities of the adsorbed species of 90Sr and 137Cs on the clay
minerals in the environment. In this study, adsorption experiments for determination ofsolid-water distribution, XRD for interlayer distances of Sr or Cs adsorbed clay minerals, andEXAFS for speciation of the adsorbed Sr and Cs were conducted. They showed that Sr and Cs
formed outer and inner-sphere complexes, respectively, in the interlayer, which explains thedifferent degree of mobility of 90Sr and 137Cs in the environment.

1B11 Fixation of Ra by specific adsorption on clay minerals based on analyses of coresamples in Ningyo-toge uranium deposit
YAMAGUCHI, A. 1, KURIHARA, Y. 2, TANAKA, K. 3, OHARA, Y. 2, KOZAI, N. 3,
TAKAHASHI, Y. 1
(1Graduate School of Science, The Univ. of Tokyo, 2JAEA NEEC, 3JAEA ASRC)
Our previous study suggested that cations with large ionic sizes have strong affinity as
adsorbed species into the interlayer of clay minerals, which suggested that radium (Ra2+) isstrongly adsorbed on clay minerals. However, actual adsorption behavior of Ra2+ in theenvironment has not been well understood. Therefore, the purpose of this study is to clarify therole of clay minerals in the migration of Ra2+ in geosphere using core samples collected in
Ningyo-toge uranium deposits. Ningyo-toge is an appropriate site for this purpose, because (i) thesite contains large amounts of uranium (U) and Ra and (ii) weathered granite layer is found under
the uranium ore-bearing layer. These factors enable us to study the migration of Ra2+ in terms offixation of Ra2+ by clay minerals in natural environment. Activity ratio of 226Ra/238U measured by
gamma-ray spectrometry showed that Ra2+ was selectivity fixed in the weathered granite layer.
Furthermore, XAFS analyses of iron (Fe), manganese (Mn), and barium (Ba) suggested that thehost phase of Ba2+ is clay minerals rather than Fe-Mn oxides and carbonate, which is likely thecase for Ra2+. These results indicated that Ra2+ leached into groundwater from U concentrated
layer was selectivity fixed on clay minerals, which supports the effectiveness to estimate
adsorption behavior of various metal ions depending on the ionic radius.
1B12 Application of simple and rapid radiostrontium analysis to natural seawater
MINOWA, H.1, KATO, Y.2, KOJIMA, S.3, OGATA, Y.4(1Radioisotope Res. Facility, Jikei Univ., 2Healthcare BU, Hitachi Ltd., 3Aichi Medical Univ.,
3

RIC Medical Division, Nagoya Univ.)
A safe, simple and rapid analysis method of radiostrontium in environmental sample wasdeveloped and was applied to natural seawater. Surface seawater at the coast of Fukushima andMie prefecture was examined. One litter of seawater was passed through a column (CV=60 mL)
with a cation exchange resin (Dowex 50W-X8). Ammonium acetate-methanol solution was
flowed through the column to eluate Ca, etc., and then Sr was eluted with 4M-HCl. Sr wascollected as carbonate precipitate on a membrane filter. Immediately after the chemical separation,the β-rays were measured by a low background liquid scintillation system (AccuFLEX LSC-LB7,
Hitachi, Ltd.) using a plastic scintillator bottle. The same sample was intermittently measured forthe growth of 90Y until radiation equilibrium (about 3 weeks later). 90Sr concentration wasdetermined with Sr yield of 70% based on the prior tracer experiments. The 90Sr concentrations inthis work were all below the minimum detectable concentration （MDC）. The 90Sr MDC of thesesamples were 0.02-0.6 Bq L-1. It took 2 days (operation time about 10 hours) for chemical
separation. It became possible to analyze more quickly than the conventional method (20 days).
This is a useful method that can be used for screening of radiostrontium in seawater.

1B13 Spectrum analysis of plastic scintillator bottle via liquid scintillation counter
KATO, Y.1, MINOWA, H.2, KOJIMA, S.3, OGATA, Y.4(1Healthcare BU, Hitachi Ltd., 2Radioisotope Res. Facility, Jikei Univ., 3Aichi Medical Univ.,
4

RIC Medical Division, Nagoya Univ.)
Conventional methods of radiostrontium analysis are complex procedures, require time forchemical separation together with large amounts of deleterious substances. Safe, simple and rapid
analytical method is desired. We tried to develop a new method to analyze radiostrontium
concentration in seawater. A measurement method using a plastic scintillator bottle (PSB) is
reported, especially the spectral analysis. Filter samples obtained by a chemical separation (seethe former report) were measured using PSBs via a low background liquid scintillation system,
LSC-LB 7 (Hitachi Ltd.). The minimum detectable concentration was 0.02 Bq L-1, which was
obtained with 1-L sample, background 0.14 cps, counting efficiency of 70%, and chemical yield
70%. It was 1/1500 of the legal concentration limit of 90Sr in the wastewater. Therefore thismethod is proved to be effective as a screening method. In addition, from the spectrum analysis of90

Sr - 90Y to be measured and 210Pb considered to be an interfering substance, the possibility of

nuclide identification by using the PSB was suggested.
2A01 Development of non-destructive isotope analysis method using negative muon
KUDO, T.1, NINOMIYA, K.1, KUBO, K.2, SHINOHARA, A.1, TAMPO, M.3, MIYAKE, Y.3(1Graduate School of Science, Osaka Univ., 2College of Liberal Arts, International Christian
Univ.,

3

Institute of Materials Structure Science, High Energy Accelerator Research

Organization)
When a negative muon stops in a material, a muonic atom that has the muon in the atomic
system instead of an electron is formed. The captured muon releases muonic X-ray by muonde-excitation process. Due to a large mass of a muon, muonic X-ray has high energies and very
hard. Using these properties, development of non-destructive elemental analysis by muon has
been on going.
In this study, we focused on the isotopic shift of muonic X-ray for developing non-destructive
isotope analysis method. The muon irradiation experiment for natPb and enriched 208Pb metal
samples was carried out at D2 beam line in J-PARC/MLF, and emitted muonic X-rays were
measured by five Germanium detectors.
From muonic X-ray spectra, we observed isotopic shift of muonic Pb KX-ray and determinedmuonic X-ray intensity of 208Pb, 207Pb and 206Pb, respectively. From muonic X-ray intensity, we
determined isotopic abundance of 208Pb as 51.5±5.8%, 207Pb as 24.5±5.4% and 206Pb as 22.2±
4.8% for natPb, these values are consistent with the reported isotopic abundance.

2A03 Composition of Fe-bearing minerals in Antarctic meteorites MIL 07710 and
Y-790272
SATO, W.1,2, NAKAGAWA, M.2, SHIRAI, N.3, EBIHARA, M.4(1Institute of Science and Engineering, Kanazawa Univ., 2Graduate School of Natural Science andTechnology, Kanazawa Univ., 3Graduate School of Science and Engineering, Tokyo Metropolitan
Univ., 4Faculty of Education and Integrated Arts and Sciences, Waseda Univ.)
57

Fe Mössbauer spectroscopy was applied to compositional studies of Fe-bearing minerals in

two different ordinary chondrites, Miller Range 07710 (MIL 07710) and Yamato 790272(Y-790272), collected in Antarctica. For both samples, spectral analysis revealed that there are
five quadrupole doublets and two magnetic sextets in the room-temperature spectra, suggesting
the presence of olivine (M1 and M2), pyroxene (M1 and M2), a high-spin Fe3+ containing phase,
antiferromagnetic FeS (troilite), and ferromagnetic Fe-Ni alloy. The large relative area of theoxidized Fe3+ phases and the small intensity of the metal phases signify a possible effect ofterrestrial weathering especially for Y-790272 (H4). In the session, we discuss the unknown Fe3+phases based on low-temperature Mössbauer spectra.
2A05 Structure of Solubility-limiting Solid Phase in M(IV) Hydroxide System using X-ray
Spectroscopy
KOBAYASHI, T.1, NAKAJIMA, S.1, MOTOKAWA, R., MATSUMURA, D., SAITO, T.,
SASAKI, T.1(1Graduate School of Engineering, Kyoto Univ., 2Japan Atomic Energy Agency, 3School ofEngineering, The University of Tokyo)
The structure of zirconium(IV) hydroxide solid phase after aging at elevated temperatures wasinvestigated by extended X-ray absorption fine structure (EXAFS), wide- and small-angle X-ray
scattering (WAXS/SAXS) to elucidate a process on the transformation of solubility-limiting solid
phase. Sample solutions with amorphous Zr hydroxide (Zr(OH)4(am)) were prepared at certain
pH and stored at 25, 40, 60 and 90°C. Aliquots of the solid phases after aging were then examinedby Zr K-edge (18.00 keV) EXAFS at BL14B1 of SPring-8, and WAXS/SAXS at BL8S3 of Aichi
Synchrotron Radiation Center. The SAXS profiles after aging at 25°C to 60°C suggested that thesolid phases were comprised of primary particles having a size of approximately 3 nm and theiraggregates. After aging at 90°C, the solid phase consisted of those with the size larger than 30 nm
in the acidic pH and the size altered depending on pH. The WAXS spectra indicated that the
crystallization occurred after aging at 90°C. In the EXAFS, all spectra exhibited intense
Fourier-transfomred peaks at ~1.7 Å and 3.0 Å, representing O and Zr atoms in the coordinationsphere. The intensities of these peaks suggested that the primary particles after aging at 25°C to
60°C consisted of tetrameric hydrolysis species and a further polymerization proceeded at 90°C.

2A07
Synthesis, structure, and electronic configuration of the luminescentnitridotechnetium complex with a tridentate ligand coordination site
YOSHIMURA, T.1, NAGATA, K.1, SHIROYAMA, T.2, KINO, Y.3, TAKAYAMA, T.4, SEKINE,
T.5, SHINOHARA, A.1,2（1Institute for Radiation Sciences, Osaka Univ., 2Graduate School of Science, Osaka Univ.,
3

Graduate School of Science, Tohoku Univ., 4Daido Univ., 5Institute for Excellence in Higher

Education, Tohoku Univ.）
Technetium has been widely used as a radiopharmaceutical for diagnosis. Recently, an interestis growing in a molecule having bimodal imaging ability by photoemission and radiation from anucleus. In this study, we synthesized a cis-dicyanonitridotechnetium(V) core which is small insize, has low molecular weight, and is luminescent. Moreover, the core has the sites to which atridentate ligand coordinates. Treatment of an orange solution of (n-C4H9)4N[99TcNCl4] with 3
equiv. bpa gave [TcNCl2(bpa)] (1). The reaction of 1 with 2 equiv. CN− yielded[TcN(CN)2(bpa)] (2). The shift of the d-d transition energies in UV-vis spectra would be inaccordance with the number and nature of the equatorial ligands; the ligand strength of aspectrochemical series (Cl− < pyridine < CN−) affects to the d-d transition energy, and increasing
the number of the ligands contributing to a larger ligand field splitting parameter increases theelectronic transition energy in the d2 nitrido Tc complexes. Photoemission with a maximum
wavelength at 666 nm was observed for 2 in the solid-state at 298 K. The trend of the emission
energies suggests that the ligand strength of the spectrochemical series for the equatorial ligands
is important for the emission energy.
2B01 Measurement of high-energy prompt γ-rays from neutron induced fission of 235U
MAKII, H.1, NISHIO, K.1, HIROSE, K.1, ORLANDI, R.1, LÉGUILLON, R.1, OGAWA, T.1,
SOLDNER, T.2, HAMBSH, F.-J.3, AÏCHE, M.4, ASTIER, A.5, CZAJKOWSKI, S.4, FROST, R.6,
GUO, S.4, KÖSTER, U.2, MATHIER, L.4, OHTSUKI, T.7, PETRACHE, C.M.5, POLLITT, A.2,
SEKIMOTO, S.7, TAKAMIYA, K.7, TSEKHANOVICH, I.5(1JAEA, 2ILL, 3JRC, 4CENBG, 5CSNSM, 6Univ. of Manchester, 7KURNS)
The Japanese government has a plan to remove the fuel debris for the full deconstruction of
Fukushima I Nuclear Power Plants. The fuel debris must be removed without reaching criticality.
The criticality of the system must be monitored by detecting the fission rate in the debris. The
fission rate should be measured by detecting radioactivity from fission, which has different
characteristics from background γ rays coming from long-lived fission products. One plausible
idea is to measure the high-energy prompt fission γ rays, whose energies are high enough to be
separated from the background γ rays. However, the measured γ-ray spectra for neutron induced
fission of 235U are limited below the γ-ray energy of about 7 MeV. This prompted us to make a
new measurement to extend γ-ray spectrum limit to higher energies. The measurement has been
carried out at the PF1b cold-neutron beam facility of the Institut Laue-Langevin (ILL), Grenoble,
France. We have successfully measured the γ-ray spectrum up to energies of about 20 MeV. In

this contribution we will present the results obtained the measurement.

2B02 Simulation of bremsstrahlung gamma ray from winter thunderclouds which weretilted along the slope of low mountains
KUROSAKI, H.
(Niigata Prefectural Institute of Environmental Radiation Monitoring)
Several detection of bremsstrahlung gamma ray from winter thunderclouds along the coast of
the Sea of Japan had been reported. We observed bremsstrahlung gamma rays four times by using
the NaI(Tl) scintillator at an altitude of 207 m, about 8 km inland from the coast, between from
Jan. to Mar. 2018., under the weather conditions that wind directions were south ~ southwest andthe wind speed of 3.3 ~ 6.7 m / s were blowing. However, these were different from the condition
that thunderclouds were tilted by strong winter storm along the coast, such as the condition of useof the model that we have named“Tilted searchlight radiation model”, which was invented in
2011. But, results of count rate calculated from this model were in good agreement withmeasurement data. Accordingly, we thought that bremsstrahlung gamma ray emissions from thetilted thundercloud were occurred. Since the thunderclouds height of 313 ~ 371 m and the low
mountain height of 351 m was almost same, the thunderclouds bumped into the mountain andtilted along the slope of the mountain by the weak wind of southerly. It was first observation of
gamma ray emission from thunderclouds which were tilted along the slope of low mountains.
2B03 Reduction of radiocesium concentration from soil and ash using
chlorination-vaporization process
KINOSHITA, N.1, JIAO, F.2, ASADA, M.1, KAWAGUCHI, M.1, HONDA, M.3, SUEKI, K.3,
NINOMIYA, Y.2(1Shimizu Co., 2Chubu Univ., 3Univ. Tsukuba)
The reduction of amount of waste discharged from decontamination work is one of theimportant issues. We applied the chlorination-vaporization process to soil samples collected in
Fukushima prefecture and clinker obtained by burning rice straw. These samples mixed withknown amount of CaCl2 or NaCl were heated at 900 - 1200 °C using an electric furnace for 30 min.
The vaporization ratio and feature of radiocesium distribution were measured with gamma-ray
spectrometry using a HPGe and imaging plate, respectively. Significant difference was notobserved in the vaporization ratio from samples mixed with NaCl+CaO and CaCl2+CaO. The
vaporization ratio of radiocesium reached up to 95% when the samples were heated at higher than
1100 °C. On the other hand, hot particles were observed in the soils. When the soil heated at
900 °C, radiocesium showed homogeneous distribution once. Then, the cesium vaporized.

2B04 A new technique for removing radioactive nuclides from aqueous solution bycoprecipitation with barite
TOKUNAGA, K., KOZAI, N., and TAKAHASHI, Y.
(1Ningyo-, 2ASRC-JAEA, 3Univ. of Tokyo)
In the present study, we explore a new application of barite (BaSO4) as a sequestering phase forselenite (Se(IV)) and selenate (Se(VI)) ions from aqueous solutions. Barite is a common phasein many geological environments, and it can be used to remove toxic and/or radioactive elementsfrom aqueous solutions, but it has not been widely used in environmental studies.

This study

describes the mechanisms of Se distribution between barite and water, thus providing a good
estimate of its ability to effectively remove Se(IV) and Se(VI) from aqueous solutions (more than80%) using the optimized experimental parameters examined here.
2B05 129I/131I ratios for the FDNPP-derived radioactive aerosol materials transported to theTokyo metropolitan area
EBIHAEA, M.1, OURA, Y.2, SHIRAI, N.2, NAGAKAWA, Y.3, SAKURAI, N.3, HABA, H.4,
MATSUZAKI, H.5, TSURUTA, H.6, MORIGUCHI, Y.7(1Waseda Univ., 2Tokyo Metropolitan Univ., 3Tokyo Metro. Indus. Tech. Res. Inst., 4RIKEN,
5

Univ. Museum, Univ. of Tokyo, 6RESTEC, 7Grad. School of Eng., Univ. Tokyo)

A large amount of radioactive materials were dispersed in the environment by the FDNPP
accident in 2011. To retrieve the diffusion trajectory of 131I, airborne particulate matters(APMs) collected in the Tokyo metropolitan area just after the accident and measured fortheir 131I activity were analyzed for their 129I contents by AMS. In evaluating blank levelsof chemicals and filters used for collecting APMs, we established the analyticalprocedure for determining 129I activity of as low as 10-8 Bq for a small piece of filter
samples (about 0.1 cm2). Coupled with 131I data, activity ratios of 129I/131I were obtainedfor 43 APM samples and a mean value of 2.18 x 10-8 (±34% for 1s) was obtained. Thisvalue is smaller than a mean value of soil samples (by 25-30%) and the inventory data (by40%). Such a difference can be explained in terms of desorption loss of 129I from APMs.
The same procedure was applied to suspended particulate matter (SPM) samples
collected at an SPM monitoring station located at the nearby APM-collecting site, andconsistent results with those of APMs in terms of 129I concentration were obtained. The
new approach developed in this study for estimating 131I contents in particulates bymeasuring 129I in APM/SPM samples can be the first step for evaluating the internalradiation exposure by inhalation of 131I.

2B06 Study on ocean circulation in the Japan Sea using iodine-129
MATSUNAKA, T.1, NAGAO, S.1, INOUE, M.1, OCHIAI, S.1, SASA, K.2, MORITA, T.3, MIKI,
S.3, HONDA, N.3, KUDO, I.4, TAKIKAWA, T.5, ARAMAKI, T.6, HONDA, M.2, SUEKI, K.2(1Kanazawa Univ., 2Univ. of Tsukuba, 3Japan Fisheries Research and Education Agency,
4

Hokkaido Univ., 5Nagasaki Univ., 6National Institute for Environmental Studies)
Oceanographic observation revealed that warming and oxygen decrease of the Japan Sea

Bottom Water (JSBW) are responding to air temperature raise in winter. The investigation of water
dynamics in the Japan Sea using radioactive tracer is essential for elucidating the interaction
between climate change and the convection systems. Anthropogenic 129I (T1/2 = 15.7 million years)
produced from the thermal neutron fission, is dominated by release from nuclear fuel reprocessing
plant. To illuminate the availability of 129I as a tracer of surface circulations and verticalconvections in the Japan Sea, we investigated the horizontal and vertical distributions of the 129I
at the large area in 2017–2018. The dissolved 129I in surface water varied from 17.8 to 23.8 nBq
L–1 at the area of 38–46°N and 135–141°E, and was negatively correlated with salinity (R2 = 0.82).
This distribution revealed that the dissolved 129I in the area was controlled by mixing of watermass from the Liman Current and the Tsushima Current. Meanwhile, the dissolved 129I in the
JSBW of the Japan Basin in 2017 was 4.2 nBq L–1, which increased by 1.2 nBq L–1 in comparison
to that in 2007. The 129I is considered to be a tracer for the surface subarctic front and JSBW in
the Japan Sea.
2B07 Searching for the origin of the Santan trade from radiocarbon dating andhistorical study
ODA, H. 1, NAKAMURA, K. 2
(1ISEE, Nagoya Univ., 2National Institute of Technology, Hakodate College)
In Japan, silk fabrics called Ezo-nishiki are distributed throughout Hokkaido andnortheastern Honshu. They were originally made in China, but they were also given to thechieftains of tribes and villages in the Amur Basin and imported to Sakhalin Island over theMamiya Strait. They were then spread southward into Hokkaido by Ainu people living on
Sakhalin Island and Hokkaido. The trade called the Santan trade peaked in the latter half of the
18th century to the early 19th century, but the origin was not clarified. Ezo-nishiki was the main
merchandise of the Santan trade. However, there is no remaining Ezo-nishiki confirmed to havebeen made before the 18th century. We thus applied radiocarbon dating to Ezo-nishiki samples todetermine their age and to clarify the origin of the Santan trade. We analyzed 34 samples of Ezonishiki by accelerator mass spectrometry. Calibrated radiocarbon ages of 33 of the samples
indicated fabrication since the middle 17th century, confirming that the Santan trade peaked
during the Qing Dynasty (1644–1912). One sample indicated fabrication between the first half ofthe 14th and the early 15th century. Ezo-nishiki thus provides evidence showing that the Santan
trade originated at least as early as that time.

3A01 Development of dry-distillation method of 211At for targeted alpha therapy
TOYOSHIMA, A.1, ZHANG, Z.2, KANDA, A.2, IKEDA, T.2, ICHIMURA, S.2, OOE, K.3,
NAGATA K.1,4, YOSHIMURA, T.1,4, SHINOHARA, A.1,2(1Institute for Radiation Sciences, 2Graduate School of Science, Osaka Univ., 3Graduate School of
Medicine, Osaka Univ., Radioisotope Research Center, Osaka Univ.)
In recent decades, targeted alpha therapy (TAT) has an increasing attention. TAT is expected toenable the effective cancer treatment by accumulating α-emitter-labelled compounds in tumor. At
Osaka University, we are conducting the TAT project with 211At in the collaboration among
Research Center of Nuclear Physics (RCNP), Graduate School of Science, and Graduate Schoolof Medicine. In this project, we need to prepare purified 211At solution which is of sufficiently
high quality to perform pharmaceutical developments and animal tests with 211At. In this study,
we examined separation conditions using our developed dry-distillation apparatus of 211At.
Astatine-211 was produced in the 209Bi(α, 2n)211At reaction at RCNP. After the irradiation, dry
distillation was carried out. In a typical procedure, He and O2 mixed gas was used and a small
amount of water was included in the system. The Bi target was heated at 840oC. Vapored 211At
was transferred to the cyrotrap through Teflon capirally. After 30-45 min, trapped 211At was
stripped with 100 µL of distilled water. The effluent was collected in a small vial and thensupplied to the following experiments. At present, chemical yield of 211At was 80 - 90% under
optimum conditions. In the symposium, details of separation experiments will be presented.
3A02 The difference of 211At species obtained by dry distillation depends on the elapsed
time after separation
IKEDA, T.1, TOYOSHIMA, A.2, KANDA, A.1, ICHIMURA, S.1, ZHANG, Z.1, YOSHIMURA,
T.1,3, NAGATA, K.1,3, OOE, K.4, SHINOHARA, A.1,2（ 1Graduate School of science, Osaka Univ., 2Institute for Radiation sciences, Osaka Univ.,
3Radioisotope Research Center, Osaka Univ., 4Graduate School of medicine, Osaka Univ.）
Astatine-211 (211At) attracts a lot of attention as an alpha-emitting radionuclide suitable fortargeted alpha therapy. In purification of 211At, a dry distillation method is often utilized. However,
little is known about chemical species of 211At in finally obtained aqueous solution after the
distillation. Thus, we studied extraction and thin-layer chromatography (TLC) behavior of 211At
obtained by the dry distillation and also investigated the dependence of species ratios on theelapsed time after separation. After the irradiation of α beam on a 209Bi target, 211At was purified
by the dry distillation. In the extraction experiment, after shaking for 2 min – 2 h, 350 µL of bothof its phases (hexane and 1 M HClO4) were precisely taken and the distribution ratio D was
evaluated. As a result, some of the 211At in distilled water exists as a neutral species which is
extractable by hexane. The TLC analysis was also performed for the 211At samples in distilledwater. In the experiments, different 3 spots of 211At with Rf values around 0, 0.5 and 0.9 wereobserved. It was also found that the percentage of cationic species with Rf = 0 increased as anincrease of the elapsed time after separation. These results suggest that the relatively slow
reaction of 211At proceeds in aqueous solution just after dissolution.

3A03 Evaluation of At-211 Labeled Amino Acid Derivative for Targeted Alpha Therapy
ZHANG, Z.1, KANEDA. K.1, TOYOSHIMA, A.2, SHINOHARA, A.1, FUKASE, K.1,2(1Graduate School of Science, Osaka Univ, 2Institute for Radiation Science, Osaka Univ)
Targeted alpha therapy (TAT) is an approach to selective delivery of an alpha emitter to tumor
for killing cancer cells with its high linear energy transfer (LET) alpha-particle, while minimizing
damage to surrounding cells. Astatine-211 has been recognized one of the most promisingradionuclides for the TAT. Our group has developed L-[211At]-α-Methyltyrosine (211At-AAMT).
The 211At-AAMT is an analog compound of 18F-FAMT which is an amino acid tracer for PET
imaging and is accumulated in tumor cells via the L-type amino-acid transporter 1 (LAT1).
The

211

At-AAMT was synthesized in one-step reaction from L-α-methyltyrosine via

mercuration, and then purified with ion-exchanges column chromatography. Isolated
211

At-AAMT was smoothly decomposed by oxidation, whereas the in vitro stability wasenhanced by addition of reducing agent, sodium ascorbate. The LAT1 specificity of 211At-AAMT
was confirmed through cell experiments. After tissue distribution of 211At-AAMT wasinvestigated in normal mice, the 211At-AAMT (0.4 Bq/mouse) was injected to nude mice
(BALB/c-nu) bearing PANC-1 tumor. The tumor growth was dramatically suppressed by the
injection of 211At-AAMT. Thus, we demonstrated the usefulness of the 211At-AAMT for cancer
treatment.
3A05
Astatine chemical species in solutions prepared by dry distillation
NISHINAKA, I.1, HASHIMOTO, K.2, SUZUKI, H2(1Tokai Quantum Beam Science Center, QST, 3Graduate School of Pharmaceutical Sciences,
Chiba Univ.)
211

At, an astatine radionuclide, with half-life of 7.2 h is one of the prospective candidates fortargeted alpha therapy of cancers. Astatine shows some different chemical behaviors incomparison with its homologue iodine. In this work, astatine chemical species have been studied
by thin layer chromatography.
The astatine radionuclides 208,209,210,211At and iodine ones 120,121,123I were simultaneously
produced by 7Li beam irradiation of a stack of lead and tin targets at the JAEA tandem accelerator
facility. The astatine and iodine radionuclides were each separated from the irradiated target witha dry distillation method. No-carrier-added astatine and iodine solutions were prepared using
ethanol or water as a solvent. Astatine in the aqueous solution was reacted with an oxidizing or areducing agent. Separation of the astatine and the iodine ions in the solutions was conducted bythin layer chromatography with an ethanol/water solution. Astatine was separated and identified
as anions of At-, AtO3- and AtO4-, while iodine was I-, compared with the standard iodine species.

3A06 Production and distribution of At-211 at RIKEN
SATO, N.1, HABA, H.1, YOKOKITA, T.1, GHOSH, K.1, WANG, Y.1, KOMORI, Y.1, MORI, D. 1,
TAKAHASHI, K.1, KIMURA, T.2, MATSUMOTO, M.2(1RIKEN Nishina Center, 2Japan Radioisotope Association)
Astatine-211 (211At, T1/2 = 7.2 h) is one of the promising radionuclides for targeted α-particle
therapy. Since 2015, we have produced purified 211At and distributed them to researchers in Japan.
In this presentation, we will describe the production technology of 211At and the present status of
the 211At distribution at RIKEN.
211

At was produced via the 209Bi(α,2n)211At reaction by irradiating a metallic 209Bi target with a

29-MeV α beam from the RIKEN AVF cyclotron. After the irradiation, 211At was purified by a dry
distillation method. Radioactivities of 211At were evaluated by γ-ray spectrometry with a Ge
detector.
Our thick target yields of 211At are 6.2–7.1 GBq/C at 27.8–28.0 MeV, respectively and they agreewith the IAEA recommended values. We confirmed the quantitative 211At production up to the
30-μA beam intensity. The chemical yield of 211At was about 80% with the 0.2-mL methanol as an
example. Our 211At products are distributed to about ten research groups in Japan and used inradio-labeling and animal experiments for drug developments.
3A07 Measurement and Estimation of the 99Mo Production Yield by the Acceleration
Neutron
TSUKADA, K.1,2 NAGAI, Y.2, HASHIMOTO, K.2, KAWABATA, M.2,3, MINATO, F.1, SAEKI,
H.3, MOTOISHI, S.3, WATANABE, S.2, ITO, M.4(1JAEA, 2QST, 3Chiyoda technol., 4Tohoku Uiv..)
We have measured the yield of 99Mo, the mother nuclide of 99mTc used in nuclear medicine
diagnostic procedure, produced by accelerator neutrons.

99

Mo was produced by the100

Mo(n,2n)99Mo reaction using neutrons provided by the C(d,n) reaction at the deuteron energyof 40 MeV. The measured yield of 99Mo from a large sample mass of MoO3 agrees well with thenumerical result estimated with the latest neutron data. This result establishes an important
finding for the domestic production of 99Mo: approximately 50% of the demand for 99Mo in Japan
could be met using a 100 g 100MoO3 sample mass with a single accelerator of 40 MeV, 2mA
deuteron beams.

3B01

Photoactivity of glass samples characterized by Mössbauer spectroscopy〇 ALI Ahmed 1, NOMURA Kiyoshi 1, AKIYAMA Kazuhiko 1, KUZMANN Ernő 2，
HOMONNAY Zoltán 2, KUBUKI Shiro 1(1 Graduate School of Science， Tokyo Metropolitan University，2 Faculty of Science，
Eötvös Loránd University )Slag from municipal household combustion plants acts an environmental problem. Almost all
slag is used in road constructing and concrete. Photocatalytic activity has many applications inwater splitting and decomposition of organic contaminations. Slag contains iron oxide which isone of the candidate materials for photocatalysis by visible light. The original slag contains 11%
of Fe2O3. The Fe2O3 added slag were prepared by a melt quenching method. The samples wereabbreviated as xFe(100-x)WS (x=10,30 and 50%). The prepared slag glass samples were further
heated at 800oC for 100min. The degradation test of methylene blue dye was used for estimationof photocatalytic activity.
XRD indicate the amorphous structure and crystalline structure before and after heat treatment,
respectively. Mossbauer parameters measured at room temperature indicate the presence ofiron3+ after heat treatment Mossbauer spectra of 50% Fe2O3 + Slag showed magnetic
components in addition to the paramagnetic components, whereas less than 30% Fe2O3 + Slagshowed only paramagnetic doublet.
The photoactivity measurements showed the first order rate constant, K=3x10-3min-1, while thefirst order rate constant increased to 17x10-3min-1 after adding hydrogen peroxide. These results
are promising for decomposing organic compound in waste water by using slag as by-productmaterials.
3B02 Defects formed in ZnO and their contribution to electroconductivity
SHIMIZU, H.1, SATO, W.1,2(1Grad. Sch. Nat. Sci. Tech., Kanazawa Univ., 2 Inst. Sci. Eng., Kanazawa Univ.)
Zinc Oxide (ZnO) is highly expected for applications to functional devices because of its
wide band gap. Commercially available ZnO shows n-type conductivity due to different native
lattice defects formed during various treatments. It is mentioned that interstitial zinc atoms andoxygen vacancies act as donor defects and zinc vacancies as acceptor defects, and the differenceof concentration of each defect corresponds to the net density of charge carriers in the sample;
however, little is known about their relationship. In order to investigate the states of latticedefects formed during heat treatment and their contribution to electroconductivity of ZnO
samples, in this work, positron annihilation lifetime spectroscopy and conductometry were
employed. For the sample annealed at 1,473 K for 1 h in air, positron lifetime was unchanged,
whereas electroconductivity was increased compared to the case before the treatment. In spite of
the treatment of longer annealing time for 12 h, similar tendencies were observed. From theresults for the sample annealed in an oxygen-rich atmosphere, we discuss the mechanism of theoccurrence of charge carriers formed in ZnO.

3B03 Nuclear spin relaxation of (111In→)111Cd in Ga-doped Fe3O4
SUGIMOTO, T.1,TAKENAKA, S.1, FUJISAWA, T.1, SATO, W.1,2(1Grad. Sch. Nat. Sci., Tech. Kanazawa Univ., 2Inst. Sci. Eng., Kanazawa Univ.)
In the same way as In ions, impurity Ga ions are also expected to show site-to-site hopping
motion in Fe3O4, which may lead to charge transportation in the ferromagnetic phase. Thus, we
synthesized 0.5 at. % Ga-doped Fe3O4, and it was doped with radioactive 111In ions. Their
hyperfine fields were investigated in a wide temperature range from 298 to 1073 K by the
perturbed angular correlation (PAC) method with the (111In→)111Cd probe. The PAC spectra at
873 to 1073 K (>TC) show relaxation patterns, and it is considered that this nuclear spin relaxationreflects the relative dynamic behavior of the probe nuclei and the extranuclear fields. In thesession, this nuclear spin relaxation phenomenon is discussed in relation to the presence of
impurity Ga ions.
3B04 Mössbauer Spectroscopic Study on the Chemical Factors Controlling the Electron
Hopping Rate in Mixed-valence Trinuclear Iron Complexes
SAKAI, Y.1, NAKAMOTO, T.2, OGISO, R.1, TAKAYAMA, T.1, KAWASAKI, T.3,
KITAZAWA, T.3, TAKAHASHI, M.3(1Daido Univ., 2Toray Research Center, 3Toho Univ.)
In mixed-valence trinuclear complexes Fe3+Fe3+Fe2+O(C6F5COO)6(C5H5N)3 ･ S (hereafter,
expressed as “Fe3O(C6F5COO)6(C5H5N)3 ･ S”), where S is a crystal solvent, iron-valencefluctuation (FeVF) phenomenon was studied mainly by 57Fe Mössbauer spectroscopy, having atime window of ~10-7 s, in order to clarify the chemical factors controlling FeVF. In the present
work, it was assumed that FeVF would be caused by hopping (or itinerant) of an excess electron
among three Fe3+ cations in the mixed-valence complexes.
Fe3O(C6F5COO)6(C5H5N)3 ･ S-complexes were prepared by an exposure method;
Fe3O(C6F5COO)6(C5H5N)3 powders were exposed in a vapor of organic compound S including
benzene, toluene, cumene, pyridine dichloromethane and so on.

Temperature-dependent

Mössbauer spectra for different Fe3O(C6F5COO)6(C5H5N)3･S complexes were analyzed on thebase of electron hopping relaxation to estimate the hopping rates. A Nowick and Wickman’s
model on the commercially available software, Moss Winn 4.0 pre, was applied in the present
analysis. The relationship between the chemical property of S and the hopping rate was discussed.
It was suggested that the high-rate FeVF in the benzene solvate could be facilitated by a molecularrotation of the solvent. The activation energy of electron hopping was estimated to be 3.0 kJ/mol
for dichloromethane solvate.

3B05

57

Fe Mössbauer Analysis of Nb doped SrTiO3 Perovskite Oxides

1,2

NOMURA, K. ,KUBUKI, S.1, YAMAKAWA, S.2, KASARI, M.2 , IZUNUMA, T2, KOIKE, Y.2(1 Tokyo Metropolitan University, and 2 Meiji University)
Perovskite oxides are used to control various physical properties such as semiconductor,
ferromagnetism, ferroelectricity, superconductivity by element substitution and are therefore
candidate materials for next generation devices of spintronics. It is known that the perovskite
oxide, SrTiO3(STO), has a band gap of 3.2 eV and a large relative dielectric constant of 300, andthat semiconductor characteristics of STO is improved by doping Nb5+. Further doping withmagnetic Fe ions is expected to improve the photocatalytic activity in the visible light region
and to use as dilute magnetic semiconductor (DMS) at room temperature. STO doped withseveral % Fe and Nb was prepared by sol-gel synthesis and pyrolysis. The magnetic properties
were clarified by a vibration sample magnetometer (VSM). The nanostructure states of thedilute Fe doped STO samples were characterized by 57Fe Mössbauer spectrometry. It is foundthat the ferromagnetic hysteresis and magnetic relaxation peaks appear with decrease of doped
Fe concentration.
3B06
In-Beam Mössbauer Spectra of 57Mn implanted into LiAlH4
1
SATO, Y. , YAMADA, Y.1, KOBAYASHI, Y.2,7, KUBO, M.K.3, MIHARA, M.4, SATO, W.5,
MIYAZAKI, J6., NAGATOMO, T.7, ANDO, T.2, TAKAHAMA, N.2, SOME, K.2, SATO, M.2,
SATO, S.8, KITAGAWA, A.8(1Tokyo Univ. of Science, 2The Univ. of Electro-Communications, 3ICU, 4Osaka Univ.,
5

Kanazawa Univ., 6Hokuriku Univ., 7RIKEN, 8NIRS)
In-beam Mössbauer spectra of 57Mn implanted into LiAlH4 were measured at 17, 35, 70,

135, 200, and 300 K to investigate the chemical form of Fe atoms trapped in the LiAlH4 lattice.
The experiment was performed using the heavy ion synchrotron accelerator facility (HIMAC) at
the National Institute of Radiological Science (NIRS). The Mössbauer spectrum measured at 17
K showed two sets of doublets. The major doublet A (δ = −0.22 mm/s, ∆EQ = 0.65 mm/s)
was assigned to FeH4−, in which the Fe has an Al substitutional position. The Mössbauer
parameters were in agreement with the results estimated by density functional calculations.
Another minor doublet B (δ = −1.5 mm/s, ∆EQ = 1.1 mm/s) was assigned to the Fe atom having
a Li substitutional position or a position associated with lattice defects. With increasing thetemperature of the sample, the intensity of the doublet B decreased. This result indicated that the
Fe atom was preferentially stabilized at the Al substitutional position having the FeH4− form.
The intensities of Mössbauer emission changed according to the temperature, and the Debye
temperature of the Fe atom trapped in LAH was estimated to be D = 170 K.

3B07 Mössbauer Spectroscopic Study on the Chemical States of Iron in Chlorite
HAMASAKA, Y.1, KAWATA, S.2, SATO, W.1,3(1Grad. School Nat. Sci., Tech. Kanazawa Univ., 2Fac. Sci., Fukuoka Univ., 3Inst. Sci. Eng.,
Kanazawa Univ.)
Chlorite has a structure of layers composed of metal ions and silicates, and its chemical formulais generally expressed as (Mg,Al)6(Si,Al)4O8(OH)10. Although it is known that Fe2+ and Fe3+
substitute for Mg and Al in the lattice, there are few reports on their chemical states. In order toelucidate the chemical state of Fe ions in chlorite, in this research, we obtained information on
the hyperfine field at the Fe site by 57Fe Mossbauer spectroscopy. Distinct spectra were obtainedfor chlorite samples taken at different production sites: one has a magnetic component, and theother does not. Assignment of the magnetic component is now underway.

P01
Isothermal gas chromatography of zinc chloride with zinc-65 tracer
MORIYAMA, T.1, GOTO, S.1, KUDO, H.2(1Grad. Sch. of Sci. and Tech., Niigata Univ., 2Fac. of Sci., Niigata Univ.)
To clarify chemical properties of superheavy elements, gas chromatography of their volatile
species has been studied. In general, the chemical properties of superheavy elements are discussed
on the basis of the relation between adsorption enthalpies, ∆ads 𝐻𝐻, at tracer scale and sublimation

enthalpies, ∆subl 𝐻𝐻. However, it is difficult to estimate the sublimation enthalpies of superheavy
elements accurately because this relation has a large variation. In our laboratory, an adsorption
enthalpies of group-4 elements, Zr and Hf, have been measured using isothermal gas
chromatography. In this study, an adsorption enthalpy of zinc chloride was measured with thesame method for group-4 elements in order to obtain the relation between ∆ads 𝐻𝐻 and ∆subl 𝐻𝐻

more precisely. Before gas chromatography experiments, evaporation behavior of zinc chloride
was researched. First, small quartz wool permeated natZn solution of 2 M HCl was placed in aquartz tube. The tube was evacuated, and dried He gas was flushed at about atmospheric pressure.
The quartz tube was heated with an electric tube furnace at 100 ˚C for 15 minutes to dry up zincsolution. After that, volatile zinc compound evaporated at higher temperature, and was caught at
a water cooling part set at the exit of the tube furnace. Quantifying Zn and Cl, this volatilecompound was identified as zinc chloride (ZnCl2). In the presentation, the detailed results withzinc-65 tracer will be discussed.
P02 Anion-exchange behavior of Zr, Hf, and Th in nitric acid for the experiment of Rf
WATANABE, E.1, NINOMIYA, H. 1, KONDO, N. 1, SHIGEKAWA, Y. 1, YASUDA, Y. 1, OUCHI,
K. 1, HAYAMI, S.2, KASAMATSU, Y.1, YOKOKITA, T.3, SHINOHARA, A.1(1Graduate School of Science, Osaka University, 2School of Science, Osaka University, 3RIKEN
Nishina Center)
We investigated the time dependence of the anion-excahnge behavior of element 104, Rf, using
automated batch-type solid-liquid extraction apparatus (AMBER) to obtain the distribution
coefficients (Kd) of Rf in hydrochloric acid. We are interested in the formation of Rf nitratecomplex and are planning to obtain the Kd values of Rf by the anion-exchange experiment in
HNO3 using AMBER. In this work, anion-exchange experiments of Zr, Hf (homologues of Rf),and Th (pseudo homologue) in HNO3 were performed by batch method to search the rapid
reaction system and to obtain the comparison data for the chemical study of Rf. Variations of theKd values of Zr, Hf, and Th were investigated as a function of the shaking time and HNO3
concentration by using the resins: Muromac ® 1×8 or Aliquat 336. From these results, in the
Aliquat 336/HNO3 system, the anion-exchange reaction equilibrium was achieved by 1-2 minutes

of shaking, and it is indicated that this reaction system would be appliable for short-lived 261Rf(T1/2 = 68 s) experiment. Based on the present results, we deduced the chemical species of Zr, Hf,
and Th, and propose suitable conditions for the anion-exchange experiment of Rf.

P03 Liquid-liquid extraction of Eu and Am with rapid extraction apparatus forexperiment of lawrencium
NINOMIYA, H.1, WATANABE, E.1, HAYAMI, S.2, KASAMATSU, Y.1, SHINOHARA, A.1(1Grad. Sch. of Sci., Osaka Univ., 2Fac. of Sci., Osaka Univ.)
In our previous study, we systematically investigated the solvent extraction behaviors of alltrivalent lanthanides and actinides except for element 103, laurencium (Lr) in a HDEHP /HNO3 system. It is difficult to investigate the chemical properties of Lr because of the low
production rates and short half-lives of the Lr nuclides. Recently, we developed the flow
Injection Solvent Extraction apparatus for superheavy elements (ISE) for online experiments
and actually succeeded in studying the liquid-liquid extraction behavior of element 104,
Rutherfordium. The purpose of this study is to establish a method to investigate the extraction
behavior of Lr. First, we carried out the liquid-liquid extraction experiments of Am and Eu bybatch method, and investigated the dependence of the distribution ratios (D) on theconcentration of the extractant. In addition, the liquid-liquid extraction experiment of Eu using
ISE were conducted under various conditions (the length of the extraction unit : 10, 20, 30 cm,
the particle size of the packed chips : 250-500, 500-710, 710-1000 μm). As a result, the Dvalues close to those obtained by batch method (at equilibrium) were acquired by theliquid-liquid extraction experiment using ISE in 0.1-0.5 M HDEHP - Benzene.
P04 Production of 236gNp tracer for determination of 237Np by Accelerator Mass Spectrometry
HAYAKAWA. Y1, YAMAMORI. K1, SAKAGUCHI. A2, SEKIGUCHI. K2, YANOU. S3,
KOMORI. Y3, YOKOKITA. T3, HABA. H3, SHINOHARA. A4, YOKOYAMA. A5(1Graduate School of Natural Science and Technology, Kanazawa University, 2Mathmatical andscience, University of Tsukuba, 3RIKEN Nishina Center, 4Graduate School of Science, Osaka
Univ., 5Institute and College of Science and Engineering, Kanazawa University)
A naturally occurring nuclide, 237Np (t1/2 = 2.1×106y), is analyzed with a short-lived
Np isotope or Pu considered similar in a chemical behavior, but there is no other tracer
that is more satisfactory. Because a long lived isotope of 236gNp (t1/2 = 1.5×105 y) can beused stably and applied to Accelerator Mass Spectrometry (AMS), it has been acandidate as a tracer for years. However, the nuclide has no established production
method. In this study, nuclear reactions of U + p and Th + Li ware carried out toproduce Np isotopes and measure their yields in γ-ray spectrometry with a Ge detector.
It was found that the 234Np, 235Np and 236mNp nuclides are produced in the reactions.
Compared to the U + p reaction, cross sections of Np isotopes in the Th + Li reaction aresmaller, but it can be expected that the formation ratio of 236gNp to 237Np interferingwith its measurement in nature is better. Based on the results, we are studying the
optimum condition of tracer production of 236gNp.

P05 Development of a Monte Carlo simulation code for analyses of adsorption anddesorption behavior of short-lived isotopes in a surface ion-source
TOKOI, K.1,2, SATO, T.K.1, EICHLER, R.3, ITO, Y.4, TOMITSUKA, T.1.3, SUZUKI, H.5, ASAI,
M.1, TSUKADA, K.1, TOYOSHIMA, A.1, CHIERA, N.M.1, NAGAME, Y.1,2(1JAEA ASRC, 2Graduate School of Science and Engineering, Ibaraki Univ., 3PSI, 4Graduate
School of Science and Technology, Niigata Univ., 5 College of Science, Ibaraki Univ)
Superheavy elements (SHEs) can be synthesized in heavy-ion nuclear fusion reactions using
accelerators. However, due to the typically low production rates and short half-lives of SHEs, few
information on their electronic structure and on their chemical properties is available.
We developed a new experimental method combining vacuum chromatography and surface
ionization, and applied this to investigate adsorption behavior of lawrensium (Lr,Z =103) on asurface of high temperature metallic tantalum. The adsorption behavior of Lr was similar to thatof lutetium (Lu, Z = 71), showing a low volatility in relation to other lanthanides.
In this work, a Monte Carlo simulation code has been newly developed to study ionization andchromatographic behavior of short-lived atoms. In the presentation, we will report the details of adeveloped simulation code and calculation results.
P06 Hydroxide precipitation experiment of Mg, Ca, Sr, Ba, and Ra for chemical study ofNobelium
NAGASE, M.,1 KASAMATSU, Y.,2 KONDO, N.,2 NINOMIYA, H.,2 WATANABE, E.,2
SHINOHARA, A.2
Nobelium (No) belongs to actinide series, and the most stable ion valence of No in aqueous
solutions is reported to be +2 although those of the other heavy actinide elements (and alllanthanides) are all +3. However, the chemical experiments of No were few because of low
production rates and short half-lives of the No nuclides. It was reported that the chemical
behaviors of alkaline earth metals are similar to that of No in some extraction experiments. The
purpose of this study is to establish the experimental mehod to investigate the precipitation
properties of No by applying the coprecipitation method with samarium (Sm) hydroxide. In thiswork, we investigated the hydroxide precipitation behaviors of alkaline earth metals (macro
amounts) by conventional filtration method. Then, we applyed the coprecipitation method with
Sm hydroxide to 85Sr, 133Ba, and 226Ra carrier-free tracers. The precipitation yields were obtained
from each metal concentration in precipitate, filtrate, cup, and standard samples. The precipitation
yields increased with higher hydroxide ion concentration, and the yield of heavier element
increased at higher hydroxide ion concentration. This tendency is consistent with the order ofsolubility product of these elements: typical properties are observed in the precipitation
experiment. However, the coprecipitation yields with Sm did not show the same tendency.

Polynuclear species might be formed in the precipitation experiment using macro amounts ofmetals.

P07 Development of Si-Ge detector array for identification of superheavy nuclide using
X-ray measurement
KAJI, D. 1, MITSUOKA, S. 1,2, HIRANO, T. 1,2, NIWASE, T. 1,2, MORIMOTO, K. 1
(1RIKEN, Nishina Center for Accelerator-Based Science, 2Kyushu University, Graduate Schoolof Science)Superheavy (SHE) element device development team in RIKEN has developed a new focal
plane detector to study on production and decay properties of SHE nuclide using a gas-filled
recoil separator GARIS-II. Conventional identification method of SHE nuclide was based on thegenetic relation between mother and daughter, was obtained from measuring the α-decay andspontaneous fission (SF) by Si-box detector. So, detailed decay scheme including γ-decay could
not be obtained. The new detector array is also useful as a probe for detection of X-ray coincidedwith α-decay. Observation of X-ray originating from SHE nuclide is one of important criteria thatmust be satisfied for the discovery of a new chemical element to be recognized. We evaluatedbasic properties of the Si-Ge detector array using nuclear reactions of 51V + natLa. In this report,
the results on the first α-γ(X) spectroscopic study at the focal plane of GARIS-II will be given indetail. (152 words)
P08 Extraction behavior of Rf from HCl to Aliquat 336 in CHCl3 or CCl4
KONDO, N.,1 KASAMATSU, Y.,1 NAGASE, M.,2 YASUDA, Y.,1 SHIGEKAWA, Y.,1 OUCHI,
K.,1 KANDA, A.,1 NINOMIYA, H.,1 WATANABE, E.,1 HABA, H.,3 KUBOKI, Y.,3 KOMORI,
Y.,3 YOKOKITA, T.,3 YANO, S.,3 SATO, N.,3 SHINOHARA, A1.
The purpose of this study is to investigate the liquid-liquid extraction behavior of Rf to Aliquat
336 from HCl. In our previous study, we carried out the liquid-liquid extraction experiment of Zr
and Hf as a model experiment of Rf, and developed the flow Injection Solvent Extraction
apparatus for superheavy elements (ISE). Then, the extraction behavior of Rf from HCl to Aliquat
336 CHCl3 solution was also investigated using ISE. In this work, we conducted the extraction
experiment of Rf to Aliquat 336 CCl4 solution. 261Rf (T1/2 = 68 s) and 169Hf (T1/2 = 3.24 min) were
produced in the 248Cm(18O,5n)261Rf and natGd(18O,xn)169Hf reactions, respectively, at the RIKEN
AVF cyclotron. The aqueous phase was 9.3 M HCl. In the experiment, the nuclear reaction
products were transported by the He/KCl gas-jet system to a chemical laboratory, and weredissolved in aqueous solution with a dissolution apparatus. The aqueous and organic solutions
were injected to the ISE. After that, we collected two phases separately on different Ta plates andsubjected to α-particle measurement. As a result, we obtained 55 α counts of 261Rf and 257No andacquired the D values of Rf. Although the D valuse of Rf using CHCl3 showed clearly defferent
behavior from those of Zr and Hf, the D values obtained in this work were similar to those of Zr,

suggesting similar results to that in the previous anion-exchange experiment of Rf.

P09

Cation exchange behavior of lanthanide and actinide using α-HIBAKASHIHARA, A.1, SUEKI, K.1, TSUKADA, K.2, TOYOSHIMA, A.2, NINOMIYA, H.3(1Graduate School of Science, Tsukuba Univ., 2JAEA, 3Graduate School of Science, Osaka
Univ.)
Recently, JAEA obtained einsteinium (Es)-254 from Oak Ridge National Laboratory. The
Es-254 material is required to be separated from its daughter nuclides and impurities to use as atarget for its physical and chemical experiments. Although Es is isolated from lanthanide andother actinides by means of cation-exchange chromatography in α-hydroxy-isobutyric acid
(α-HIBA) solution, its ionic radius, affecting effective charge and thus stability constants, has notbeen determined yet. Thus, in the present study, we carried out cation-exchange chromatographyof heavy actinides in α-HIBA to deduce ionic radius of Es from the relationship between ionicradius and the elution position. We first examined peak positions of lanthanide elements in theelution chromatography to ensure the relationship for lanthanide. Peak positions of Fm, Es, Cf,
and Am were then measured in the chromatography with α-HIBA, and a similar trend as
lanthanides was found in the relationship for actinides. We are now obtaining further elution dataof Cm and Bk to establish the relationship for actinide.
P10 Thermal-chromatography of astatine compounds in gas-phase generated indry-separation process
ICHIMURA, S. 1, TOYOSHIMA, A.2, ZHANG, Z. 1, IKEDA, T. 1, OOE, K.3, NAGATA, K.2,4,
YOSHIMURA, T.2,4, SHINOHARA, A. 1,2（ 1Graduate School of science, Osaka Univ., 2Institute for Radiation sciences, Osaka Univ.,
3

Graduate School of medicine, Osaka Univ., 4Radioisotope Research Center, Osaka Univ.）

Recently, targeted radiation therapy using an α-particle-emitting nuclide, 211 At, is attracting agreat deal of attention. In our research group, experiments such as drug synthesis and animal tests
are conducted using 211At solution prepared by dry distillation. In this method, an irradiated Bi
target containing 211At is first heated in a closed system and then 211At is vaporized and carried bya carrier gas to a cold trap. 211At is accumulated in the cold trap and then dissolved in a small
amount of solution which is then supplied to the following experiments. However, the recovery
yield of 211At is strongly dependent on the composition of the carrier gas. This is probably because
chemical species of 211At and their ratios are different for the gas conditions. In this work, we
newly developed a thermal-chromatography system and investigated the adsorption behavior ofgaseous 211At compounds on quartz surface to study generated chemical species of 211At. As aresult, the adsorption behavior of 211At is different for each gas-composition. This suggests thatseveral types of 211At compounds with different volatilities are produced at the same time. Detailsof the adsorption behavior will be presented in the meeting.

P11 Coincidence measurement of the beta-particle and the electron from Ac-229 forobserving the internal conversion electron of Th-229m
SHIGEKAWA, Y.1, KASAMATSU, Y.1, YASUDA, Y.1, KONDO, N.1, NINOMIYA, H.1,
WATANABE, E.1, HAYAMI, S.1, SHINOHARA, A.1(1Graduate School of Science, Osaka University)
The excitation energy of 229mTh is as low as 7.8 ± 0.5 eV. It has been expected that the decay
process and the half-life of 229mTh varies depending of the chemical environments. Although theinternal conversion (IC) electron of 229mTh was recently detected and the IC half-life was found to
be around 7 μs, the precise excitation energy is yet to be measured. We are aiming to determine
the precise excitation energy by measuring the energy of the IC electron of 229mTh. In this work,
we tried to measure the IC electron of 229mTh with the coincidence measurement of the beta
particle and the electron from 229Ac. With the retarding field between the 229Ac sample and theelectron detector, we can measure the energy of the IC electron. First, we fabricated 229Ac byirradiating 20-MeV proton to 232Th. Then we purified 229Ac and prepared an electrodeposited229

Ac sample. We measured the detection time of the beta particle and the electron from thesample, and obtained coincidence spectra. The purification of 229Ac from 232Th and fission
products well succeeded. However, the signal which corresponds to the disintegration of 229mTh
was not detected. We need to find the method for preparing the extremely thin sample whichenables the IC electron to escape from the surface.
P12 Verification of excitation functions for photonuclear reactions with simple irradiation
systemKIKUNAGA, H.1, KASHIWAGI, S.1, TAKAHASHI, K.1, NANBU, K.1, TSUKADA, K.1,
NODA, S.2, IDA, H.2, IMURA, R.2, OURA, Y.3(1ELPH, Tohoku Univ., 2 JFE Engineering Corporation, 3Graduate School of Science, Tokyo
Metropolitan Univ.)
Radioisotope production by using bremsstrahlung irradiation has been carried out at ELPH,
Tohoku Univ. The production yields of photonuclear reactions are estimated by multiplying
bremsstrahlung spectrum and excitation functions. The former can be reproduced well by particle
transport simulation codes such as PHITS code, while the latter is difficult to obtain bothexperimentally and theoretically. Therefore, even (g,n) reactions, there are not manymeasurements of the excitation functions and its values differ from experiment to experiment. In
this study, we try to verify the literature values of the excitation functions and those obtained by acalculation code by using a simple activation method.

P13 Network calculation of p-nuclei in IaSN using Hauser-Feshbach statistical calculation
KINOSHITA, N(Shimizu Co.)
The type Ia supernovae (IaSN) take place when a mass exceeds the Chandraskhar limit.
Nuclear reactions with photon, proton, and neutron in the explosive environment produce
numerous nuclides including neutron-deficient nuclei, p-nuclei. Cross sections of these nuclear
reactions depend on a theoretical calculation using the Hauser-Feshbach (HF) statistical model.
Some parameters such as optical model potential and level density affect strongly the precision of
the cross sections. The parameters were optimized by comparing experimental cross sections
reported by several researchers with the theoretical cross sections for which different parameters
were applied. Then, cross sections of 3052 nuclei from C up to Cm with photon, proton, andneutron were calculated by applying both default parameter and the optimized parameters in the
HF calculation. The network calculation was done using reaction rate calculated by these 2
different parameters in the HF calculation. Cross sections of alpha emission reaction strongly
depend on the optical potential of alpha particle. Therefore, the cross sections estimated withdefault input parameter are larger than those estimated with the modified input parameter in thetheoretical calculation. The different cross sections result in different pathway for the productionof the p-nuclei. I discuss the production of the p-nuclei affected by the different input parameter.
P14 Concentrations of 129I in river waters of eastern Fukushima, Japan
UEDA, S.1, OCHIAI, S.2, HASEGAWA, H.1, KAKIUCHI, H.1, SATOH, Y.1, OHTSUKA, Y.1
HISAMATSU, H.1(1Department of Radioecology, Institute for Environmental Sciences, 2LLRL, Institute of Natureand Environmental Technology, Kanazawa Univ.)
River waters in the Ukedo, Odaka, Ohta, Niida, Mano Rivers etc. located in the eastern part of
Fukushima Prefecture were collected in August 2016 and August 2017, and concentrations of 129I
in these river waters were measured by AMS. The maximum value of 129I concentration in riverwater was 1.6E-6 Bq L-1 of the Ukedo River, and the minimum value was 2.4E-7 Bq L-1 of theHirose River. The range of 129I/127I atomic ratio in river water was 3.9E-9 to 7.4E-8, and the
maximum value was the Ukedo River both 2016 and 2017. There was also a significant
correlation between 129I/127I atomic ratio and dissolved 137Cs concentration in river water.
Therefore, it is presumed that the amount of 129I and 137Cs deposited in the catchment area of theriver in the eastern part of Fukushima Prefecture has a relatively similar distribution.

P15 Examination of Chemical States Analysis Condition of Heavy Metals in Municipal
Solid Waste Incineration Fly Ash Containing Radioactive Cesium
TAKAHASHI, T.1, MIZUNUMA, T.2, KASARI, M.2, KOIKE, Y.1(1Sch. of Sci. and Tech., Meiji Univ., 2Grad. Sch. of Sci. and Tech., Meiji Univ.)
MSWI fly ash was sampled in Fukushima Prefecture.
Radioactive cesium (134Cs and 137Cs) and toxicity heavy metals were often contained in a
municipal solid waste incineration (MSWI) fly ash. Radioactive cesium was concentrated in the
MSWI fly ash incinerated by high temperature. Several studies reported on radioactive

nuclides including radioactive cesium in MSWI fly ash were focused on its speciation. It
is necessary to investigate the chemical states for the purpose of evaluating the toxicity of
not only radioactive cesium but also other heavy metals. In this study, chemical states
analysis conditions were optimized to understand elution behavior of heavy metals in MSWI fly
ash. Thus, the sequential extraction test based on method of Tessier et al. was conducted using
simulated fly ash samples mixed with silicon dioxide and some lead compounds. For example,
according to the leaching test with pure water for a model sample of fly ash containing lead (II)chloride, a part of lead was not eluted. An optimal sequential extraction procedure for MSWI fly
ash will be proposed by evaluating the analysis result of the model samples of fly ash.

P16 On-site determination of radioactive cesium in environmental sample using portable
NaI scintillation counter.
MOCHIMARU, T.1, AKIYAMA, M.2, HAGIWARA, K.1, KOIKE, Y.1(1 Sch. of Sci. and Tech., Meiji Univ., 2 Grad. Sch. of Sci. and Tech., Meiji Univ.)
An on-site determination method for radioactive cesium (134Cs and 137Cs) in environmental
sample has been developed using a portable NaI scintillation counter combined with solid phaseextraction disk. By using potable measuring equipment, rapid on-site analysis is possible withouttransporting the collected environmental sample to the laboratory. Radioactivity of radioactive
cesium in the disk-shaped radioactive standard materials (IAEA) and solid phase extraction disk
concentrated soil eluate were determined by using NaI scintillation counter, Get Smart XR, and
HP-Ge spectrometer. Radioactive cesium was identified in each of the gamma-ray spectra
obtained by the two spectrometers. Detection efficiencies for Get Smart XR were calculatedusing area of photo peak in gamma-ray spectra and concentration of 137Cs in the soil eluate.
Relative errors between activity concentration of 137Cs by Get Smart XR and HP-Ge spectrometer
were suppressed to ± 5%. The present method using the portable NaI scintillation counter will beapplicable to rapid on-site determination for radioactive cesium in environmental samples.

P17 ICP-MS analysis of river water and treated sewage targeted on gadolinium and iodine
fractions due to contrast mediums of MRI imaging and X-ray CT inspection, andcorrelation of their concentrations and other mental elements and naturally occurring
radioactive nuclides
MATSUMOTO-KAWAGUCHI, E1., IMAGAWA, A1., MIYAMOTO, N1., SAKAMA, M1.,
FUKUSHI, M2., INOUE, K2., SATO, T1., IHARA, T1., IMOTO, S1.
(1Graduate School of Health Sciences, Tokushima Univ., 2Graduate School of Human Health
Sciences, Tokyo Metropolitan Univ.)
A purpose of this study is to investigate the relevance with level characteristics of gadolinium
and iodine concentrations to contain in river waters with the MRI and iodine contrast mediums
such as X-ray computed tomography and the angiography by analyzing the river water samples
which we had collected regionally. We have measured 26 element concentrations among the riverwater samples, which supplied to us at the part of the collaboration program together with
Fukushi and others of Tokyo Metropolitan University and also which they had collected from 30
sampling points of the Tonegawa basin using our ICP-DRC-MS apparatus (Tokushima Univ.),
and investigated those distribution behaviors ranged from the upstream to downstream.
Furthermore, we have examined the correlation between the location of the sewage disposal
plants and the concentration properties of gadolinium and iodine in those river samples. These
results confirmed that the characteristics of the concentration level behavior of gadolinium fromupstream to downstream on the river basin represented similar tendency like the element group of
the artificial pollution such as aluminum and zinc.
P18 The Geochemical cycles at the surface in the Sea of Japan implied from lateral profiles
and seasonal variations of 228Th/228Ra and 234Th/238U activity ratio
MOROKADO, T1., INOUE, M1., SHIROTANI, Y1., FUJITA, A1., HANAKI, S1., MORITA, T2.,
MIKI, S2., HONDA, N3., HIROHASHI, N4., ANDO, H5., SATO, Y6., MORIWAKI, K6., NAGAO,
S1.
(1LLRL, Kanazawa Univ., 2NRIFS, FRA.,3

JSNFRI, FRA., 4Shimane Univ., 5Niigata Univ.,

6

Shimane Prefectural Government., )The radium isotopes (226Ra, t1/2 = 1600 y; 228Ra, t1/2 = 5.75 y) are dissolved in, and circulateswith seawater in marine environment. Those main source of supply are coast sediment andcontinental shelf. Then 228Ra/226Ra ratio in coastal area is higher than open sea influenced by shortlife of 228Ra. On the other hand, the thorium isotopes (228Th; t1/2 = 1.91 y, 234Th; t1/2 = 24 d) are
adsorb suspended particle and scavenged in marine environment. Therefore, compare with eachparent nuclides, 228Th/228Ra and 234Th/238U ratios can be the indexes of particle and adsorption
materials. In this study, we discus on the circulation and scavenging effect of Sea of Japan byhorizontal distribution and seasonal variation of 228Ra/226Ra、228Th/228Ra and 234Th/238U ratioimplying high-resolution spatial researches.
The sea water samples were collected from 2014 to 2018 at the Sea of Japan Honshu coast.
Each samples are 20L non-filtered surface water.

P19 Distribution of I-129 in forest soil from the boundary of Fukushima Daiichi Nuclear
Power Plant
YANG, G.1, TAZOE, H.1, TSUKADA, H.2, YAMADA, M.1(1Institute of Radiation Emergency Medicine, Hirosaki Univ., 2Institute of Environmental
Radioactivity, Fukushima Univ.)
Long-lived 129I (t1/2 = 1.57×107 y) can be used to reconstruct the early dispersion anddistribution of the Fukushima Daiichi Nuclear Power Plant (FDNPP) derived 131I (t1/2 = 8.03 d)in the environment, and to study the behavior of radioiodine after deposition onto terrestrial
system. The core soil samples were collected from forest at about 1.1 km south from the
FDNPP in 2017, and the distribution of 129I from the FDNPP accident was determined by the
combination of TMAH extraction and ICP-MS/MS analysis. The surface soil samples (0–5 cm
depth) were heavily contaminated with 134Cs (262–1,588 Bq g-1) and 137Cs (259–1,570 Bq g-1)
(decay corrected to March 11, 2011). The 129I activities decreased sharply with the soil depth,
from 1,211 to 34.1, 534 to 78.9, and 2,536 to 51.3 mBq kg-1, respectively, for the three sites. In
addition, the 129I inventories were observed to be 35.0±1.0 (0–15 cm depth), 28.2±0.9 (0–17.5
cm depth), and 55.1±1.8 (0–15 cm depth) Bq m-2, respectively.
P20 Low-levels of the FDNPP-derived radiocesium of marine products from coastal
areas in the Sea of JapanINOUE, M.1, YAMASHITA, S.1, TAKEHARA, R.1, MIKI, S.2, NAGAO, S.1(1LLRL, Kanazawa Univ., 2NRIFS-FRA)
Low-background γ-spectrometry combined with the 40K-removal treatment technique wasapplied to marine products collected in coastal areas of the Sea of Japan during 2012–2017. The
radiocesium concentrations in the samples were < 0.005–0.02 Bq/kg-wet for 134Cs and < 0.05–0.17
Bq/kg-wet for 137Cs. The concentration factors (CFs) of 134Cs and 137Cs in fishery products were
estimated to be ~30–100, which approximately agreed with those of 137Cs recorded before the
Fukushima Dai-ichi Nuclear Power Plant (FDNPP) accident around the Japanese Archipelago. The
uptake of 134Cs from local sources (e.g., 134Cs-contaminated coastal sediments and the leakage from
nuclear power plants) along Honshu was not evident in the marine products. Therefore, it was
concluded that marine products have continually taken up 134Cs from the ambient seawater and preyorganisms (through the food chain) in the inhabitant areas after the re-entry of 134Cs with the
Kuroshio Current water from the Pacific Ocean-side (after 2013).

P21
Root Uptake Effect on Cs-137 Concentration in Aquatic Plants
1
TAGAMI, K. , UCHIDA, S.1(1QST-NIRS)
When a nuclear accident occurred, radiocaesium is one of the most important radionuclides
among the discharged radioactive materials to the environment because it can cause a majorradiation source to humans several years after the accident. In the terrestrial environment, soil andwater can be radiocesium sources to plants. Two to three years after the Fukushima Daiichi
nuclear accident, water soluble radiocaesium concentrations in fresh waters became low,
therefore, in the upland conditions, soil is the main source to contribute radiocaesium
concentrations in crops. In freshwater conditions, e.g, rivers and lakes, soluble radiocaesium still
may affect the concentrations in emergent plants because they can take up radiocaesium throughtheir aboveground part. However, it was not clear which is the major source to the plants, soil orwater. In this study, therefore, uptake of Cs-137 by emergent plants (literature data) was examinedby comparing their Cs-137 uptake with those of submerged and floating plants (literature data) as
well as upland herbaceous plants (field observation data). From the results, it was estimated thataround 20% of the total Cs-137 in emergent plants was from water.
P22 Air dose rate monitoring at the portable radiation monitoring stations in Fukushima
Prefecture
MIYATA, S., TANAKA, H., SATO, S., OTA, Y., ISOGAI, K.
(Japan Chemical Analysis Center)Air dose rate monitoring have been carried out with portable monitoring stations (Fuji ElectricCo., Ltd.) at 80 locations in Fukushima Prefecture since April 2012. 60 monitoring stations have 2
detectors, silicon semiconductor detector for high air dose rate and NaI (Tl) detector for low air
dose rate, and 20 monitoring stations have only silicon semiconductor detector. Decreases of air
dose rates were observed at all the monitoring stations due to the decay of artificial radioisotopes(134Cs and 137Cs). In addition to the long-term dose reduction trends, short-term fluctuations in air
dose rates were observed, which were caused by various natural and artificial factors. Artificial
factors include changes in surrounding environment such as “decontamination activity around themonitoring station”. Regarding artificial factors, presence of radioactive wastes around the station
will also cause the increase of air dose. At some monitoring stations, abrupt changes in dose rates
were observed due to this type of factors. Regarding natural factors, it is generally known that therainfall causes the increase of air dose due to the washout and rainout of Radon progenies.
However, decrease of air dose rate while rainfall were surrounded by the area with relatively highradioactivity concentration. This is caused by the water layer formed on the ground surface whichfunctions as a shield against the gamma-rays from 134Cs and 137Cs in the ground, similar to theshielding effect by snow cover.

P23 Determination of platinum group elements of GPt-5 chromitite reference sample byusing INAA and ID-ICP-MS
SHIRAI, N.1, AKHTER, R.1a, EBIHARA, M.1b
(1Graduate School of Chemistry, Tokyo Metropolitan University, Present affiliation: aBangladesh
Atomic Energy Commision, bWaseda University)
Major, minor and trace element (Mg, Al, Ca, Sc, V, Cr, Mn, Fe, Co, Ni, Zn and Ir) abundances
for a chromitite reference sample, GPt-5, were obtained by using INAA. Except for Ni, our INAA
data are in good agreement with literature values. By using ID-ICP-MS coupled with NiS
fire-assay pre-concentration, the same samples previously analyzed by INAA were used for thedetermination of platinum group elements (Ru, Rh, Pd, Os, Ir and Pt) in order to avoid thesampling bias in assessing the effectiveness of the NiS fire-assay pre-concentration. It waspossible to determine Ir abundance by using both the INAA and ID-ICP-MS, and the values
obtained were consistent with each other within the measurement precision. It was confirmed that
the NiS fire-assay pre-concentration applied in this study can digest chromitite and that theaccurate determination of platinum group element for chromite-containing rocks can be
performed by using our analytical method. Based on the Ru/Rh ratio, GPt-5 chromitite reference
sample is classified as a podiform chromitite.
P24 Depth profile of 137Cs concentration in soil collected in 2016 near the Fukushima
Dai-ichi Nuclear Power Plant
NINOMIYA, K.1, KITA, K.2, SHINOHARA, A.1, KAWATSU, K.3, MINOWA, H.4, FUJITA, N.1,
OHTSUKI, T.5, TAKAMIYA, K.5, KINO, Y.6, KOARAI, K.6, SAITO, T.7, SATOU, Y.8, SUEKI,
K.9, TAKEUCHI, Y.10, DOI, T.10, CHIMURA, K.10, ABE, Y.11, INAI, Y.1, IWAMOTO, Y12,
UESUGI, M.13, ENDO, S.14, OKOCHI, H.12, OKUMURA, S.15, ONO, T.11, ONOSAKI, H.11,
KATSUMI, S.12, KANDA, A.1, KINNO, S.12, THANH, N. T.14, KUBO, K.16, KOIKE, Y.15,
MOTOOKA, A.12, SUZUKI, M.6, SUZUKI, K.3, SUZUKI, A.1, TAKASE, T.3, TAKAHASHI,
M.1, TAKENAKA, S.13, ZHANG, Z.1, NAKAI, I.11, NAGAO, S.13, NAKAMURA, S.14, NANBU,
A.1, NISHIYAMA, J.6, NISHIYAMA, Y.5, FUKUDA, D.15, FUJII, K.15, MIYAZAWA, N.13,
MURANOI, T.6, MORIGUCHI, Y.17, YATAGAI, A.18, YAMAMORI, K.13, YOKOYAMA, A.13,
YOSHIDA, G.19, YOSHIMURA, T.1, WATANABE, A.3(1Osaka Univ., 2Ibaraki Univ., 3Fukushima Univ., 4The Jikei Univ. School of Medicine, 5Kyoto
Univ., 6Tohoku Univ., 7Shokei Gakuin Univ., 8JAEA, 9Tsukuba Univ., 10National Institute forEnvironmental Studies,
14

11

Tokyo Univ. of Science,

12

Waseda Univ.,

13

Kanazawa Univ.,

Hiroshima Univ., 15Meiji Univ., 16International Christian Univ., 17The Univ. of Tokyo,

18

Hirosaki Univ., 19KEK)Soil sampling up to 30 cm depth at 31 points near the Fukushima Dai-ichi nuclear power plant
was conducted in 2016. After drying the sample, 134Cs and 137Cs concentration with each 2.5 cm
depth was determined from gamma-ray spectrometry. The depth profiles of the 134Cs and 137Csconcentration were investigated. Most sites have the highest concentration in the surface samples.
The result shows 137Cs still remains near the soil surface region though over 5 years was passed
from the Fukushima Dai-ich Nuclear Power Plant accident.

P25 Decontamination of paddy field soil using a stable isotope
DEZAWA, Y.1, MIYOSHI, H.2, HIGAKI, S.3 , MORI, K.4, SERA, K.5, YANAGA, M.6(1Grad. School of Inte. Sci. and Tech., Shizuoka Univ., 2ARREM, Tokushima Univ., 3ISC, Tokyo
Univ., 4ING Co., Ltd, 5Cyclo. Res. Center, Iwate Medical Univ., 6 Fac. of Sci., Shizuoka Univ.)

A large amount of radioactive material was released into the environment by the
Fukushima nuclear power plant accident. Paddy field soil was also contaminated withradioactive cesium. Although there have been no reports that activity of rice produced in
Fukushima prefecture exceeding the reference value was detected recently,
decontamination is necessary to prevent damage by rumors. We previously reported thatthe absorption of radioactive cesium from artificially contaminated soil into rice plants
increased by adding a stable isotope to irrigation water. In this study, cultivation tests
were conducted by using paddy field soil collected in Fukushima prefecture to examine
whether the absorption of radioactive cesium from really contaminated soil increase ornot. In addition, the test was conducted by changing the amount of the stable isotope to be
added. Harvested brown rice was transferred to a U8 container and radioactivities of 137Cs
and 134Cs in the brown rice were measured with a high purity Ge semiconductor detector.
As a result, in groups which added Cs stable isotope, the absorption amount increased
compared with the group which was not added.
P26 Measurements of Cs-137 activity concentration in individual organs of wild raccoons inNamie town
TAKUMI, O.1, KAZUMA, K.1, YASUSHI, K.1, HIROAKI, T.1, TOSHITAKA, O.1,2, ATUSHI,
T.3, TOSHIHIKO, S.4,5, YOSHINAKA, S.4, MIREI, C.4, YOHEI, F.6, VARERIE GOH SEE
TING.6, KENTARO, A.7, AKIFUMI, N.8, MASATOSHI, S.9, HIDEAKI, Y.10, TOMISATO, M.6,7,
TSUTOMU, S.1,2, HISASHI, S.4(1Depertment of Chemistry, Tohoku Univ., 2Institute for Excellence in higher Education, Tohoku
Univ., 3Tohoku University hospital, Tohoku Univ, 4Graduate school of Dentistry, Tohoku Univ,
5

International Research Institute of Disaster Science, Tohoku Univ., 6School of Health Science,

Hirosaki Univ., 7Institute of Radiation Emergency Medicine, Hirosaki Univ., 8Faculty of
Pharmaceutical science, Hokkaido University of Science. 9Institute for Disaster Reconstruction
and Regeneration Research, Tohoku Univ., 10Faculity of Agriculture, Niigata Univ.)
We measured Cs-137 activity in individual organs of wild raccoons in Namie town toinvestigate Cs-137 distribution in raccoon. We caught twelve raccoons with a box trap, andcollected femoral muscle, liver, kidney, spleen, heart, lung, and blood together with the samples
for biological measurement. We found a weak positive relationship between air dose rate area of

the sampling site and Cs-137 activity concentration in femoral muscle in high air dose rate area,and did not found the correlation in low air dose rate area. Cs-137 activity concentrations infemoral muscle did not always reflect the air dose rate of the sampling site because raccoons canlive in both city and mountain area. This result indicates an importance of the measurements ofindividual raccoons. Activity concentration of femoral muscle was the highest of all the organs
measured, and activity concentration of blood was lowest. Activity concentrations of the otherorgans (liver, kidney, spleen, heart, lung) ware almost half value of the femoral muscle.

P27 Recent in Environmental
Measurements
SHIMA, N.1, TAMARI, T.1

Tritium

Concentrations

andActualAnalytical(1Kyushu Environmental Evaluation Association)
We investigated the tritium concentration in the current environment in Kyushu district. Each
precipitation and monthly atmospheric water vapor were collected at Fukuoka City from Feb
2016. Seawater and river water were collected at Fukuoka, Saga, Oita, Kumamoto, Miyazaki,
Kagoshima in 2017. Every samples were performed electrolytic enrichment and measured by low
background LSC. Tritium concentrations in precipitation and atmospheric water vapor were in
the range of 0.08 to 1.25 Bq / L and 0.19 to 0.88 Bq / L, respectively. The tritium concentrations inthe seawater ranged from 0.05 to 0.15 Bq / L. Tritium concentrations in the river water ranged
from 0.16 to 0.27 Bq / L. In recent years, tritium concentrations in environmental water in the
Kyushu district are very low, and it is suggested that electrolytic enrichment for sample water is
indispensable to evaluate its concentration.
P28 Determination of 134Cs by Sum peak method using Ge semiconductor detector
SUZUKI, K., AKIYAMA, M., OTA, Y., ISOGAI, K.
(Japan Chemical Analysis Center)
An attempt was made to expand the application of the 'sum-peak' method to determine 134Cs inenvironmental samples. Coaxial type Ge detectors and cylindrical sample containers were used
for gamma-ray measurement.
Firstly, 134Cs point source was measured in the vicinity of the Ge detector and the activities
were calculated by 'sum-peak' method. The calculated activities were in good agreement with the
spiked value within 10% in the measurement geometry that the distance between the source andthe detector endcap is less than 5cm. Secondly, 134Cs volume sources with different packing
thickness to the containers were measured on the endcap of the detectors. From the results,
geometry dependence of the calculated values by 'sum-peak' method were evaluated. Finally,
airborne dust samples collected in Chiba city several months after the Fukushima Daiichi Nuclear
Plant Accident on 2011 were measured and 134Cs activities were calculated by 'sum-peak' method.
The results agreed within 10% with the activity values determined by conventional calibration
method. This shows that the 'sum-peak' method is applicable at least under limited measurement
conditions.

P29

Estimation of aerosol attaching to unnamed aerial vehicle body surface

flying in radioactive plume
OSADA, N.1, ISHIZAKI, A.2, NISHIZAWA, Y.3, YUUKI, Y.3, SANADA, Y.2(1Advanced Science Research Center, Okayama Univ., 2Japan Atomic Energy Agency, 3OYO
corp.)
Unmanned aerial vehicle to survey the radioactivity of the ground surface is one of usefulprocedure to environmental radiation. When the aerial vehicle will fly in the radioactive plume,
the radioactive aerosol attach to the aerial vehicle body surface. The attaching radio-materials will
disturb the survey. In this study, we estimated attaching amount of the radioactive aerosol to theaerial vehicle body surface for evaluation of the disturbance. Two model aerial vehicles were set
in constant wind including potassium solution aerosol. The attached radio-materials werecollected by a filter paper, and measured with a Ge-semiconductor detector. The recovered
radio-materials were also analyzed by atomic absorption spectroscopy. The result suggests thatthe velocity of attachment was from 2.0x10-4 to 9.7x10-3m/s.
P30 The variation of atmospheric radioactive ceasium concentration from Fukushima
Dai-ichi nuclear accident in Tsukuba and Iitate, and the factors of high concentration
phenomena
DOI, T.1, TAKAGI, M.1, TANAKA, A.1, KANNO, M.2, DOKIYA, Y.2, TAO, Y.2, MASUMOTO,
K.3(1National Institute for Environmental Studies, 2 Resurrection of Fukushima, 3 High Energy
Accelerator Research Organization)

Radioactive Cs concentration in the atmosphere of Tsukuba and Iitate in about one year
after nuclear accident were levels of 10-5 Bq m-3 and 10-4 Bq m-3, respectively.
Sometimes atmospheric radioactive Cs at two sites of Iitate showed high concentration
due to strong wind and resuspension of soil at the time of local decontamination. The highconcentration phenomenon on August 2013 seemed to be caused by the removal of thedebris at Fukushima Dai-ichi Nuclear Power Plant. The activity median aerodynamic
diameter of 134Cs- and 137Cs-bearing particles were larger than 1.2 µm. Radioactive Cs
aerosol of particle size larger than 1 μm may be taken into the alveoli by respiration, but it
will be removed thereafter. It was thought that the influence of annual internal radiation
exposure by breathing estimated from the atmospheric concentration was low. It wasthought that the influence of annual internal radiation exposure from breathing estimatedfrom atmospheric concentration was low.

P31 Formation of groundwater with high radium in the former mining open-pit at
Ningyo-toge Environmental Engineering Center of the Japan Atomic Energy Agency
TAKEUCHI, E.1, TOMITA, J.1, OHARA, Y.1(1JAEA)To investigate the formation of fresh groundwater with high 226Ra activity, groundwater
samples discharged from uranium mill tailings, weathered granite and sedimentary rocks werecollected from 9 boreholes in a former mining open-pit at Ningyo-toge Environmental
Engineering Center, Japan Atomic Energy Agency. Activities of Ra isotopes (226Ra, 228Ra) ofgroundwater samples were measured along with dissolved cations and anions. Rock samples werealso sampled from 8 boreholes, and the activities of U-series (238U, 234U, 230Th, 226Ra) andTh-series (232Th, 228Ra) radionuclides were determined.
The 226Ra activities of the groundwater samples ranged widely from 26 to 2425 mBq kg-1, andthe highest value was obtained from the borehole of the uranium mill tailings. The 226Ra
concentrations showed an increasing tendency with increase of salinity. In comparison with thegroundwater from other areas in Japan, the groundwater samples in this study showed higher226

Ra activities than those estimated from salinities. The results of both 228Ra/226Ra activity ratioof the groundwater and U- and Th-series radionuclide activities of the rock samples suggested thepossibility that 226Ra was supplied to groundwater by dissolution of the phase containing high226

Ra activity rather than alpha-recoil process for the groundwater sample with the highest 226Ra

activity.

P32 Component Analysis by SEM-EDS on Radioactive Particles Emitted from Unit 1 of
FDNPP
ISHII, I.1, SUEKI, K.1, MATSUO, K.1, HASEGAWA, R.1, SATOU, Y.2, ADACHI, K.3,
IGARASHI, Y.4(1Univ. of Tsukuba, 2JAEA, 3Mteorological Research Institute, 4Ibaraki Univ.)
Radioactive particles were released into the environment by the accident of Fukushima Daiichi
Nuclear Power Plant (FDNPP). They have information to understand the inside of the reactor
during the accident. In this study, we picked up about 50 radioactive particles derived from theUnit 1 and measured them using a Scanning Electron Microscope (SEM) with an Energy
Dispersive X-ray Spectrometer (EDS). For each radioactive particle, several point analyses were
performed and elemental X-ray intensities were calculated. The X-ray intensities werenormalized by that of silicon. Two component plots of the normalized X-ray intensities showedcorrelations among selected elements. For instance, there was a positive correlation between Na
and Mg and also between K and Ca. On the other hand, there was a negative correlation between

the group of Na-Mg and the group of K-Ca. The group of K-Ca also had Ti, Fe, Zn and Pb. We
discuss the formation mechanism of radioactive particles with the elemental correlations.

P33 U-236 and uranium isotope ratios in soil samples from Hunan Province, China
SHAO, Y.1,2, YANG, G.1, TAZOE, H.1, YAMADA, M.1(1 Institute of Radiation Emergency Medicine, Hirosaki Univ., Japan, 2 Institute of High Energy
Physics, Chinese Academy of Sciences, China)
Without significant nuclear accident, presently, 236U far from the nuclear facilities in China may
be mainly from global fallout. In the present study, inductively coupled plasma tandem mass
spectrometry (ICP-MS/MS) was applied to analyze ultra-trace 236U in 48 soil samples from Hunan
Province, China. The 236U concentrations were measured as (1.61–21.3)×107 atoms g-1, and the236

U/238U, 234U/238U and 235U/238U atom ratios were (0.470–4.91)×10-8, (5.10–9.31)×10-5 and(7.11–7.82)×10-3, respectively. Comparing with other studies, 236U concentrations in Hunan
Province were lower than that in forest soils from Ishikawa Prefectures, Japan ((8.92–37.6)×108
atoms g-1), similar to soils from La Palma, Spain ((1.43–8.12)×107 atoms g-1) and soils collectedfrom Fukushima Prefectures, Japan not affected by the NPP accident ((0.953–20.2)×107 atomsg-1). Considering the facts that neither nuclear tests nor nuclear accidents have occurred in Hunan
Province and that the 236U/238U atom ratio results are included in the global fallout value range, thedata of 236U in soil samples from Hunan Province may be mainly from global fallout.
P34 Radiochemical analysis of fission and activation products released by Fukushima
nuclear accident
KOJIMA, S., ARINOBU, T.
(Aichi Medical Univ., School of Medicine)
We reported previously that the radioactivity of the fission products, 127mTe, 129mTe, 125Sb, 137Cs,
140

Ba, 141Ce and 144Ce, and that of the neutron activation products, 54Mn, 58Co, 60Co, 110mAg, 114mIn,

134

Cs and 136Cs in the soil sample collected on May 19 at Namie-cho, 8 km northwest from

Fukushima Daiichi NPP. The purpose of this paper is to determine the radioactivity of 95Nb and113

Sn in the soil sample. The soil sample was separated into the solution and the insoluble residue

by filtration, after it was treated by nitric acid. The gamma-ray of 95Nb was detected in the residue,
as Nb hardly dissolved in nitric acid. The radioactivity of 95Nb was 4.9 Bq/g at the sampling time,and it was less than that of one-300th of 137Cs. The gamma-ray of 113Sn was identified in thefraction removed 137Cs and 110mAg. This means that the atoms of Sn in the cladding tube of
zirconium alloy had been irradiated by neutrons, and the produced radionuclides, 113Sn and 114mIn,
were released from the reactor to the environment.

P36 Study on Migration Behavior of Suspended Solids in the Kumaki River Based on
Carbon-Nitrogen Isotope Ratio and Radionuclides
TAHARA, R., NAGAO, S., OCHIAI, S, HASEGAWA, T., GOTO, A.
(1Grad. School of Natural Sci. and Technol., Kanazawa, Univ., 2INTE, Kaznazawa, Univ.., 3Inst.
Sci. Eng.LEEE, Kanazawa, Univ..)
Suspended solids in rivers are mainly derived from paddy field and forest soil, industrial andlifework wastewater, resuspended bottom sediments, fallout from the atmosphere. The decline of
agriculture and forestry activities has caused the decline of productivity of land and coastal
marine environment. In the previous study, 7 Be / 210 Pbex ratio is used as an indicator of suspended
particle flux due to residence time of recent topography erosion and suspended solids. In thisstudy, we investigated the transport behavior of suspended solids from watershed to river by using
the radioactivity(7Be, 137Cs, 210Pbex)and carbon and nitrogen isotopic ratios of organic matter inthe Kumaki River located in Noto Peninsula during April 2016 to March 2018. The downward
variation of 137Cs/210Pbex ratio shows difference in every month. However, the 137Cs/210Pbex ratio of
rainy samples shows almost similar values among the up stream, middle stream and downstream.
P37 Composition analysis of radioactive particles composed of two kinds of silicatecompounds
MATSUO, K.1, SUEKI, K.1, ISHII, T.1, HASEGAWA, R.1, SATOU, Y.2, ADACHI, K.3,
IGARASHI, Y.4, ABE, Y.5, NAKAI, I.5, SAKAMOTO, T.6, MORITA, M.6(1Univ. of Tsukuba, 2JAEA, 3Meteorological Research Institute, 4Ibaraki Univ.,
5Tokyo Univ. of Science, 6Kogakuin Univ.)
In March 2011, radioactive particles were emitted into the environment by FDNPP accident.

They include much information about the internal reactor building at the time of the accident1). In
this study, we found that the radioactive particles from Unit 11) were composed of two kinds ofsilicate materials. Their surface elemental distribution was measured by SEM-EDS and showedthat they had Na-abundant part and K-abundant parts. We analyzed them by XRF, XANES andXRD at BL37XU in SPring-8. We found that constituent elements of Na-abundant part differedfrom these of K-abundant part and that main components of the both part were silicate glass. By
using FIB-TOF-SIMS with a fine processing function2), it was revealed that Cs abound in thesurface of the particle, and Na-abundant part had more Cs than K-abundant part inside the particle.
We also found a clear border between the two parts. From these results, we conclude that theparticle was presumed to make by two types of silicate glass and that Cs adhered to the particle
after making the matrix of the particle.
1) Y. Satou et al. 2018. Geochem. J. 52, 137 – 143.

2) T. Sakamoto et al. 2008. Appl. Surf. Sci. 255, 1617-1620.

P38 Evaluation on Deposition of Fukushima Derived Radiocesium to Bottom Sediment at
Mountain Lakes in Gunma Prefecture, JapanMIYASAKA, S.1, NAGAO, S.2, OCHIAI, S.2, SUZUKI, K.3, WATANABE, S.3, ARAI, H.3,
KUGE, T.3, MORI, M.4(1Graguate School of Natural Science & Technology, Kanazawa Univ., 2Institute of Nature andEnvironment Technology, Kanazawa Univ., 3Gunma Prefectural Fisheries Experiment Station,
4

Univ. of Kochi.)
The massive Tohoku Earthquake and consequent tsunamis occurred on 11 March 2011 anddamaged the Fukushima Daiichi Nuclear Power Plant (FDNPP) seriously. Through the FDNPP
accident, a large amount of radiocesium was released to the environment. In this study, we
collected sediment cores at Lake Haruna and Lake Onuma, which are located at high altitude in
Gunma Prefecture, Japan. The concentration of 134Cs and 137Cs was determined by germanium
detectors. We also measured the concentration of 210Pb to estimate the sedimentation rate at eachsampling site. At Lake Onuma, the 134Cs/137Cs activity ratio at the upper layer was almost 1.0(decay-collected to 11 March 2011), indicating that radiocesium in the sediment samples wasderived from the FDNPP accident. The highest concentration of 137Cs for the center of Lake
Onuma appeared at 0-2 cm (5.0×103 Bq/kg) for the core collected in 2011 and at 5-6 cm (3.7×103
Bq/kg) depth in core collected in 2017. The sedimentation rate for the center of Lake Onuma in2011 (0.060 g/cm2/y) was similar to that of in 2017 (0.058 g/cm2/y). Based on above results,
sediments associated with 137Cs could deposited from the surface layer (0-2 cm) to deeper layer(5-6 cm) with constant sedimentation rates between 2011 and 2017.
P39 Mössbauer Spectroscopic Characterization of Iron in Iron-loaded Woody Charcoals
SUZUKI, K.1, SUZUKI, T.1, YAMAUCHI, S.2, KURIMOTO, Y.2, TAKAYAMA, T.3, SAKAI, Y.3(1Kitami Inst. of Technology, 2Akita Prefectural Univ., 3Daido Univ.)
Woody charcoal is versatile material and has been used as adsorbent due to its porosity. Some
metal salts serve as an effective catalyst for carbonizing wood. Among the salts, iron salts showhigh catalytic activity for wood carbonization. The iron-loaded woody charcoals we synthesized
have a mesoporous-rich body and high crystallinity compared to charcoals synthesized withoutcatalysts. The charcoals probably contain magnetic iron species when they are carbonized atrelatively high temperature. Thus, it can be expected that the magnetic charcoals adsorb thesubstances that ordinary woody charcoals are incapable of capturing. We attempted to identify themagnetic iron species included in iron-loaded charcoals by Mössbauer spectroscopy, revealingthat the iron species and their production ratio were strongly affected by carbonization method. It
is interesting to note that the magnetic iron species produced by a one-step carbonization wereextremely different from those by a two-step carbonization.

P40 Feasibility study for identification of radioactive materials sealed in container using
negative muon
KUDO, T.1, NINOMIYA, K.1, KUBO, K.2, SHINOHARA, A.1, TAMPO, M.3, MIYAKE, Y.3(1Graduate School of Science, Osaka Univ., 2College of Liberal Arts, International Christian
Univ.,

3

Institute of Materials Structure Science, High Energy Accelerator Research

Organization)
For identification of radioactive materials, many analysis methods have been applied such as
ICP-MS, fluorescence X-ray analysis and radioactivity measurement. Among them, radioactivity
measurement is the most powerful tool because this method can be applied without sample
destruction if the sample is sealed in the container. However, it is difficult to apply radioactivity
measurement for the sample with low gamma-ray branching nuclide and/or existing strong
gamma-ray emission impurities.
Our group has been studying on development of elemental analysis methods using muonic X-ray.
Muonic X-rays emitted from muonic atom has 207 times higher energy than these of electronic
X-rays. In this study, we performed muon irradiation experiment for bismuth metal sealed in thecontainer and examined feasibility of analysis by muonic X-rays for such samples. The muon
irradiation experiment was performed at D2 beam line in J-PARC/MLF, world’s intense pulsed
muon source. Muonic X-rays were measured by germanium detectors.
By selecting the timing of muon beam pulse, background signals were significantly reduced, andwe successfully identified Bi sealed in Aluminum container without sample destruction.
P41 Local Fields in ZnO Codoped with Co and Mn —a 57Co Emission Mӧssbauer
Spectroscopic Study—
MORIICHI, R.1, KANO, Y.1, SATO, W.1, 2(1Grad. Sch. Nat. Sci., Tech., Kanazawa Univ., 2Inst. Sci., Eng., Kanazawa Univ.)
We measured internal fields in 6.25 at.% Co- and 6.25 at.% Mn-codoped ZnO (CMZO) and 11
at.% Co-doped ZnO (CZO) synthesized by a solid state reaction by means of 57Co emissionMӧssbauer spectroscopy. In CMZO, two doublets were observed in the spectrum at room
temperature : one (D1) is assignable to a 57Fe2+ (←57Co) substituting for a defect-free Zn site in
ZnO, and the other to 57Fe3+ (←57Co) in substitutional Zn sites adjacent to a Zn vacancy. However,
below 100 K, the spectrum cannot be fitted only with two doublets, so we assumed the emergenceof an additional magnetic component (M1). We found that the relative intensity of D1 decreases
and that of M1 increases with decreasing temperature. In addition, we carried out magnetization
measurements for CMZO, CZO and 6 at.% Mn-doped ZnO (MZO), and found that only CMZO
shows slightly different trend from that expected for paramagnetism. The results of the 57Co
emission Mӧssbauer spectroscopy and magnetization measurements may imply that codoping Co

and Mn in ZnO can realize the emergence of dilute magnetism.

P42 Effect of molecular structure on the muon transfer process in benzene and cyclohexane
INAGAKI, M.1, NINOMIYA, K.1, KUDO, T.1, TERADA, K.1, SATO, A.1, KAWASHIMA, Y.2,
TOMONO, D.2, SHINOHARA, A.1(1Grad. Sch. Sci., Osaka Univ., 2RCNP, Osaka Univ.)
Formation processes of muonic atoms are influenced by the chemical environments ofmuon-capturing atoms, as it is called chemical effect. Previously, we reported that the chemical
effect on the muon transfer processes in benzene and cyclohexane in the gas phase was smaller
than the detection limit. In this study, to investigate the chemical effect on the muon transfer
processes in the liquid phase, muon irradiation experiments for liquid mixtures of benzene or
cyclohexane and carbon tetrachloride were carried out. The experiments were conducted at the
MuSIC-M1 beamline of the Research Center for Nuclear Physics (RCNP) in Osaka University.
Muonic X-rays emitted after muon-capture by carbon or chlorine atoms were measured with highpurity germanium detectors. The muon capture probabilities of carbon and chlorine atoms were
determined from the muonic X-ray spectra. The model formula for the muon capture was set up,
and the muon transfer rate to carbon atoms in each sample was obtained using the muon capture
probabilities. The result suggested that the muon transfer rate to carbon atoms of benzene
molecules are higher than that to carbon atoms of cyclohexane molecules.
P43

Observation of local structures in perovskite oxide SrTiO3 with the 111Cd probe

KOMATSUDA, S.1, SATO, W.2, OHKUBO, Y3.
(1Nat. Inst. Tech., Ichinoseki College, 2Inst. Sci. Eng., Kanazawa Univ., 3KURNS)
Strontium titanate (SrTiO3) doped with metal ions as impurity donors exhibits a wide variety ofelectric properties. For a practical use of SrTiO3 as a conduction-controlling device, it is of great
importance to study the lattice site location of doped impurities and their surroundings. For that
purpose, the time-differential perturbed angular correlation method (TDPAC) is very suited
because it can directly provide atomic-level information of impurity atoms. From this point ofview, we have applied the TDPAC method to a study of SrTiO3 using the 111In(→111Cd) probe.
Strontium titanate sample doped with the 111In(→111Cd) was synthesized by a solid-state reaction
in air at 1473 K. For the PAC spectrum obtained at room temperature, two electric field gradientswere observed, characterized by the quadrupole frequencies and its fractions ωQ1 = 48.9(1)Mrad/s, f1 = 68(3)%, and ωQ2 = 52.1(2) Mrad/s, f2 = 36(3)%, respectively. In the presentation,
based on the further investigation of TDPAC spectra for SrTiO3 measured at 500~1000 K, we
discuss the site occupation of the 111In(→111Cd) probe and their local structures in perovskite
oxide SrTiO3.

P44 Hydrogen-Induced Defects in Palladium Observed by Means of Gamma-Ray Nuclear
Spectroscopies
FURUMOTO, M.1, SHIMIZU, H.1, OHKUBO, Y.2, SATO, W.1,3(1Grad. Sch. Nat. Sci. Tech., Kanazawa Univ., 2KURNS, 3Inst. Sci. Eng., Kanazawa Univ.)
Palladium (Pd) can dissolve a large amount of hydrogen atoms in the lattice interstitial sites andis expected to be applied as a hydrogen storage material. However, it is widely known that defects
formation induced by hydrogen absorption may decrease its storage performance. Thus,
application of Pd to hydrogen storage metal still has problems in terms of tolerance. Therefore, inorder to obtain more detailed information on the hydrogen storage performance of Pd, it isimportant to investigate the physical state of lattice defects caused by the introduction ofhydrogen. In this study, behavior of lattice defects in Pd associated with hydrogen absorption wasobserved by two different nuclear spectroscopies. Positron annihilation lifetime spectroscopy(PALS) applied to electrochemically hydrogen-introduced Pd suggested existence of latticedefects. Perturbed angler correlation (PAC) measurements using the 111Ag probe revealed thepresence of electric field gradient at the probe site in the electrochemically hydrogen-introduced
Pd. In the poster presentation, we evaluate the hydrogen-induced lattice defects in Pd based on the
results of the nuclear spectroscopic methods.
P45 Production method development of 67Cu using thermoseparation for cancer therapy.
OHTA, A.1,2, KAWABATA, M.1,2, MOTOISHI, S.1,2, SAEKI, H.1,2, HASHIMOTO, K2.,
TSUKADA, K. 2,3, HATSUKAWA, Y. 2, NAGAI, Y. 2
(Chiyoda Technol Corporation1, National Institutes for Quantum and Radiological Science andTechnology2, Japan Atomic Energy Agency3)67

Cu is a promising RI for both cancer therapy and diagnosis in nuclear medicine, yet the large

scale production has not been achieved to satisfy the clinical demand. High quality 67Cu can beproduced via the 68Zn(n,x)67Cu reaction （x=n'p, d）from zinc target where projecting fast neutrons
are generated in carbon converter by stopping 40 MeV deuterons from an accelerator. Separationof 67Cu from 68Zn were previously established1), however it may require a longer hours to obtain a
final product from a large volume of zinc target. Concentration of a large quantity of zinc wastherefore investigated by thermoseparation2) using a difference in vapor pressure between zincand copper. The method also serves the removal any impurity copper in the zinc target before
irradiation.
Natural zinc metal that was irradiated by neutrons at CYRIC Accelerator (Tohoku University) or
Tandem Accelerator (Japan Atomic Energy Agency) was heated under reduced pressure. The
bulk of zinc was sublimated, moved and deposited at lower temperature area. The gamma-rays

from 67Cu and 69mZn within the target were measured with CZT (CdZnTe) semiconductor detector.
The poster discusses the results on separation efficiencies and the behavior of both tracer
elements while they were heated.
Reference
1) Y. Sugo et. al., J. Phys. Soc. Jpn. 86, 023201 (2017)
2) Lu Zhan et. al., Separation and Purification Technology 68, 397 (2009)P46 Development of a Rn-At generator system using radon gas enclosed within a syringe
KAWASAKI, K.1, SHIN, Y.1, AOI, K.2, WASHIYAMA, K.3, NISHINAKA, I.4, HABA, H.5
YANOU, S.5 YOKOYAMA, A2(1Graduate School of Natural Science and Technology, Kanazawa University., 2Institute andCollege of Science and Engineering, Kanazawa University., 3Fukushima Medical University.,4

Tokai Quantum Beam Science Center, QST., 5RIKEN Nishina Center.)

The radionuclide of 211At gathers much attention as a nuclide useful for isotope treatment. Its
chemical species are explored and the solvent extraction of At is investigated for that purpose.
However, its half-life is as short as 7.2 hours and it is difficult to use it in a place remote from anaccelerator. Milking of 211Rn (of 14.6 hours in half-life), the parent nuclide of 211At, makes it
possible to use it at a remote location. In this study, 211Rn gas was stored in a sealed syringe forma dissolved target. 211At produced 211Rn gas with nitric acid or hydrochloric acid. Beside we
investigated on the extraction and back extraction of 211At using ionic liquid as solvent and crownether as extractant. As a result, we succeeded in holding 211Rn gas in a syringe and recovering
211

At from 211Rn gas. The 211At extraction was performed at an extraction rate of about 90％ with

0.1M nitric acid. The back extraction of At was performed with sodium hydroxide and potassiumhydroxide at their higher concentrations than 1M. From the results, we conclude that this method
is promising as a generator system.
P47 Syntheses and stability evaluation of alkaline earth metal complexes for nuclear
medicine
NAGATA, K.1, YAJIMA, T.2, KASAMATSU, Y.3, SHINOHARA, A.3, YOSHIMURA, T.1（1Institute for Radiation sciences, Osaka Univ., 2Materials and Bioengineering, Kansai Univ., 3
Graduate School of science, Osaka Univ.）
Radium-223(223Ra) has a great potential for targeted alpha-ray therapy due to multiple alpha decay
in the decay chain. The maximum value of the stability constants logKML reported in the known
Ra(II) complexes still remains at ~10, and the logKML value is insufficient to apply in nuclear
therapy. We have tried to synthesize a stable Ra complex in vivo to obtain new cancer drugs
applicable to various kinds of tumors. In the present study, we used macrocyclic ligands, L1 andL2, that have two 6-methyl picolinate arms and a diaza-18-crown-6-ether framework.
The alkaline earth metal (Ca, Sr, Ba) complexes were synthesized by the reactions of L1 and L2
with the metal ions, respectively. The stability constants in the Ca(II), Sr(II), and Ba(II) complexes
with L1 and L2 were determined by pH-potentiometric titration in 0.1 M KNO3(aq). In all themetal ions studied, the logKML values in the L1 complexes are high compared with the values inthe L2 complexes. The logKML values follow the order: Ba(II) > Sr(II) > Ca(II) for both the L1
and L2 complexes. It has been found that L1 can provide radionuclide (85Sr, 133Ba and 226Ra)chelate complexes. The reactions detected by the radio TLC method with γ ray spectroscopy. The
complex formation was quantitative in both the cases using 85Sr, 133Ba and 226Ra.

P48
Production of 211At using middle-sized cyclotron, MP-30 and its purification
WASHIYAMA, K.1, AOKI, M.2, SASAKI, S.2, ODA, T.3, NISHIJIMA, K.3, TAKAHASHI, K.1(1Advanced Clinical Research Center, Fukushima Medical Univ., 2SHI Accelerator Service Ltd.,
3

Sumitomo Heavy Industries, Ltd.)
Among the α-emitters that can be used for targeted radionuclide therapy, Astatine-211 with ahalf-life of 7.21 hours is one of the promising isotopes for clinical application. There have been
many institutes and universities reporting to study 211At for production, labeling, preclinicalevaluation in Japan. Fukushima Medical University has also started production of 211At using the
medium-sized cyclotron MP-30 and its vertical irradiation system developed by Sumitomo Heavy
Industries, Ltd. since 2016. We irradiate Bi-metal with 28.6 MeV α beam of 20 eμA to produce
211

At by 209Bi(α, 2n)211At nuclear reaction. The thick target yield is 30.2 MBq/μA·h as almost

same as in the literature. Here we report our evaluation regarding the series of changes the beam
current, energy, Bi-metal amount, target holder design, to find the optimum conditions of ourtargetry.
P50 Investigation on solvent extraction of astatine for 211Rn-211At generator―Comparison to the 131I behavior and investigation on the effect of oxidizing agents inextraction
SHIN, Y1., KAWASAKI, K1., AOI, K2., YOKOYAMA, A2., WASHIYAMA, K3., NISHINAKA,
I4., YANOU, S5., HABA, H5.
(1Graduate School of Natural Science and Technology, Kanazawa Univ., 2Institute and College of
Science and Engineering, Kanazawa Univ., 3Fukushima Medical Univ., 4Tokai Quantum Beam
Science Center, QST., 5RIKEN Nishina Center.)211

At is a promising nuclide among various α-emitters for targeted α therapy. It has high α- particle

energy and the emission probability of α-ray is about 100%. However, 211At is produced by anaccelerator and the half-life of 211At is only 7.2 hour. It is too short to deliver to remote areas fromaccelerator facilities. In order to use astatine in wider ranges we are developing a 211Rn-211At
generator. In a previous study, 211At produced in decaying of 211Rn in dodecane solution can beback-extracted into 90% ethanol aqueous solution with N-bromosuccinimide (NBS), while themechanism of astatine extraction with NBS is not known. In this study we assumed that Br2
generated from NBS oxidizes astatine. We used NCS and NIS instead of NBS to investigate theeffect of redox potential. In addition, we compared the back-extraction ratios of 211At and 131I byusing bromine water as an oxidizing agent. As a result, the order of back extraction ratio is NBS> NCS > NIS. Comparing 211At and 131I, the back-extraction ratio of 211At increases with additionof bromine, but that of 131I does not increase. It shows that 211At is oxidized into species which iseasily extracted.

P51 Synthesis of an astatinated amino acid derivatives via silicon-astatine exchange
reaction
WATANABE, S.1, ANWAR-UL, A.M.1,2, NISHINAKA, I.1, SASAKI, I.1,3, OHSHIMA, Y.1,
YAMADA K.3, ISHIOKA, N.S.1(1QST Takasaki, 2NINMAS, BAEC, 3Graduate School of Science and Technology, Gunma
Univ.)
Astatine-211 (211At) is a promising alpha-emitting radionuclide for the targeted alpha therapy(TAT) and tin-astatine exchange reaction has been used for the synthesis of astatinatedcompounds. However, organotin compound is readily decomposed under high temperature andacidic condition, which makes synthetic routes of precursor complicated. In addition, toxicity ofthe organotin compounds is a potential cause of concern for future clinical applications. We
therefore

focusedonsilicon-astatine

exchange

reaction.

In

thepresent

study,

4-[211At]astato-L-phenylalanine was synthesized via the electrophilic desilylation. HPLC analysis
revealed that a strong radioactive peak was observed at 16.8 min. of retention time, which was
identical to that of corresponding radioiodinated phenylalanine (retention time: 15.8 min.). The

astatinated compound

was time-dependently accumulated into LS180, colon

adenocarcinoma cell, and the uptake was inhibited in the presence of some amino acidderivatives. These results clearly indicated that 4-[211At]astato-L-phenylalanine was
successfully synthesized in this study. Radiochemical yield and purity were 64-75% and over
99%, respectively. We therefore make a conclusion that the silicon-astatine exchange reaction isuseful to synthesize astatinated amino acid derivatives and peptides.
P52
Study on synthesis of Y@C60 by nuclear recoil
1
1
ITO, Y. ,AKIYAMA, K , KUBUKI, S.1, HATSUKAWA, Y.2(1Tokyo Metropolitan Univ, 2QST.)
We have tried to synthesis of Radioactive Endohedral Metallofullerenes (REMFs) using thenuclear recoil induced by nuclear reaction. This method has some advantages from the viewpointof a small amount of by-products and selective production of target REMFs. In the previous study,
we reported the synthesis of 85Sr@C60 using the nuclear recoil 86Sr(n, 2n)85Sr reaction with 14
MeV fast neutron induced by DT reaction. In this study, we will report the synthesis of 88Y@C60
by nuclear recoil of 89Y(n, 2n)88Y reaction with 30 MeV and 50 MeV fast neutron induced by DT
reaction.
Irradiated samples were dissolved into CS2 and filtered to remove a large amount of C60. Afterdryness of the filter, aniline and HClaq was passed through the filter, sequentially. The γ ray fromextracted samples was measured by Ge detector.

As a result, the radioactivity of 88Y observed in the aniline solutions derived from 88Y@C60 for
examined in this work was estimated to be several percents in the total radioactivity of each
irradiated sample.

P53 Preparation of Carrier-free 139Ce Tracer for Endohedral Metallofullerene StudyAMEKURA, K. 1, AKIYAMA, K. 1, 2, KUBUKI, S. １, HABA, H ２(1Tokyo Metropolitan Univ., 2RIKEN, Nishina center.)
We have studied the electronic state for a series of light lanthanide (Ln) metallofullerene, such as
Ln@C82, by analyzing the small difference in the HPLC retention time. For such precise analysis,
the radiochemical method is one of the most effective approach because this method allows thesimultaneous analysis of multiple elements. For further studies, it is necessary to analyze from thedifference between these retention times monitored by gamma ray of reference carrier-free
Ln@C82 and by UV absorption because some heavy lanthanide, such as Er and Dy, only produce
nuclides with short half-life. In this study, we report the chemical separation of 139Ce used as acarrier-free reference material from a target material of La and the result of metallofullerene
preparation using this carrier-free 139Ce.
139

Ce and a target material of La were separated by the solvent extraction method using K2Cr2O7

as an oxidant. The amount of 139Ce was determined by gamma-ray measurement and the residual
amount of Cr and La were estimated to be 2.5% and 0.03%, respectively, from UV/vis absorption
analysis. More than 90% of 139Ce were finally obtained and also EMF is found to be successfully
prepared using this carrier-free 139Ce.
P54 A study on the sedimentary environment of Tokyo-bay sediments under hypoxia.
MATSUO, M.1, KOMIRI, M.1,2, SHOZUGAWA, K.1, OKUMURA, R.3, IINUMA, Y.3,
TAKAMIYA, K.3(1Graduate School of Arts and Sciences, The University of Tokyo, 2Yokohama Environmental
Science Research Institute, 3KURNS)
Hypoxia is a big problem particularly in inner bay such as Tokyo Bay. To understand and solve
the problem, we attempted to estimate the redox environment of Tokyo-bay sediments underhypoxia, assuming that the effect of past hypoxia could be preserved as a difference inconcentrations and/or chemical states of elements in the sediments.
We collected sediment cores off the coast of Yokohama (flat seafloor) and Makuhari (flatseafloor and dredged trench) in Tokyo Bay. The samples were sliced every 2 cm and analyzed byinstrumental neutron activation analysis.
As a result, the concentration of Mn was low in the dredged trench off Makuhari, whereas
there was no significant difference in Fe. It is estimated that the oxidation-reduction potential in
the dredged trench remained to the extent that Fe precipitation occurred but no Mn precipitation
occurred. In addition, the values of Th/U and Ce/U ratios at each site existed in different places ona same line. It is found that the magnitude of the reductive environment increased in the order offlat seafloor off Yokohama < flat seafloor off Makuhari < dreaded trench off Makuhari. This trend
is in good agreement with water quality data and estimation results by 57Fe Mössbauer
spectroscopy.

P56 Production and Purification of 105Ag
KUBOTA, T.1, IWATA, K.2, FUKUTANI, S.1, TAKAHASHI, T.1, TAKAHASHI. S.1(1KURNS, 2Graduate School of Agriculture, Kyoto University)

The Fukushima nuclear accident released a large amount of radioactive nuclides into
the environment. Among them, short half-life radionuclides, for example 110mAg, would
be paid less attention to; however, those are critical for external and internal exposure justafter the accident. In this study we prepare carrier-free radioactive silver, 105Ag, as tracer
nuclide, which is suitable for plant and animal experiment. 105Ag was produced from
cadmium through photo-nuclear reaction. An aliquot of CdCl2 of 2.5 g in a quartz test
tube was dehydrated in a muffle furnace and encapsulated under vacuum. The test tube
was irradiated with photons generated by the bombardment of platinum sheets with 30
MeV-electrons. 105Ag was purified by precipitation and anion exchange chromatography.
Cadmium was removed by precipitation at pH 11 in chloride solution, while silver
remained in the solution as complex ion. Cadmium and silver was once adsorbed onto
anion exchange resin, then cadmium was washed out with 0.1 M HCl and finally silver
was recovered with 0.1 M HNO3. The resulting product showed that the specific activityof 105Ag was 6.8 (kBq/mL) and the concentration of cadmium was 10 ppb.
P57 Non-destructive elemental analysis of Ni based super alloys by using time of flight
prompt gamma-ray analysis
TOH, Y. 1, HUANG, M.1,2, SEGAWA, M.1, MAEDA, M.1, TSUNEYAMA, M.1,3, KIMURA, A.1,
NAKAMURA, S.1(1JAEA, 2IMP, 3NAT.)
The Accurate Neutron-Nucleus Reaction Measurement Instrument (ANNRI) has beendeveloped for measurements of prompt gamma-ray analysis (PGA), nuclear cross-section dataand nuclear astrophysics at BL04 of the Material and Life Science Experimental Facility (MLF)of the Japan Proton Accelerator Research Complex (J-PARC). We have developed an analyticaltechnique which combines prompt gamma-ray analysis with the time-of-flight technique by using
an intense pulsed neutron beam. We have conducted several experiments of Ni-based super alloys
samples, and have analyzed 3 types of spectra PGA, TOF(NRCA) and TOF-PGA. Presentation
will describe the detail of the experimental results and new device (neutron filter), the current
status of the developments and future prospects.

This work was supported in part by Grants-in-Aid for Scientific Research(JP17H01076).

P58 LET Dependence of Reactive Oxygen Species Generations in an Aqueous
Sample Irradiated by Heavy-Ion Beam
MATSUMOTO, K., NYUI, M., UENO, M., OGAWA, Y., NAKANISHI, I.
(Quantitative RedOx Sensing Team, Department of Basic Medical Sciences for Radiation
Damages, National Institute of Radiological Sciences, National Institutes for Quantum andRadiological Science and Technology)
The amounts of reactive oxygen species generated in aqueous samples by irradiation with
X-ray or clinical carbon-ion beams were quantified. Hydroxyl radical (•OH), hydrogen peroxide(H2O2), and the total amount of oxidation reactions were measured by electron paramagnetic
resonance-based methods. •OH generation was expected to be localized on the track/range of the
carbon-ion beam/X-ray, and mM and M levels of •OH generation were observed. Total •OH
generation levels were identical at the same dose irrespective of whether X-ray or carbon-ion
beam irradiation was used, and were around 1.2‒1.3 μmol/L/Gy. However, sparse •OH generationlevels decreased with increasing linear energy transfer, and were 0.61, 0.53, and 0.38 μmol/L/Gy
for X-ray, 20 keV/μm carbon-ion beam, and 80 keV/μm carbon-ion beam sources, respectively.
H2O2 generation estimated by TEMPOL decay was as 0.21, 0.57, and 0.35 μmol/L/Gy, for X-ray,
20 keV/μm carbon-ion beam, and 80 keV/μm carbon-ion beam sources, respectively, whereas the
H2O2 generation estimated by Fenton-reaction-ability was as were 0.22, 0.26 and 0.29 μmol/L/Gy,
respectively. TEMPOL decay may only reflect the dense H2O2 generation. The amounts of total
oxidation reactions were 2.74, 1.17, and 0.66 μmol/L/Gy, respectively. The amounts of oxidation
reaction caused by the low LET beam were reduced in hypoxic atmosphere, but not changed byhigh LET (>80 keV/μm) beam. The generation of reactive oxygen species was not uniform at themolecular level.

P59 Radiocarbon dating of the ancient calligraphy fragments attributed to famous persons
ODA, H. 1, IKEDA, K. 2, YASU, H. 3, SAKAMOTO, S. 4
(1ISEE, Nagoya Univ., 2Faculty of Letters, Chuo Univ., 3Taga High School, 4Ryukoku Univ.)

Kohitsugire are ancient paper sheets containing elegant calligraphy. They wereoriginally pages or parts of ancient manuscripts, pictures or sutras. The old calligraphy
written before the 14th century hardly remain as complete books or scrolls; therefore,
kohitsugire potentially has high academic value. Most of kohitsugire have traditional
certificates which identify the calligraphists. However, recent paleographical study showsthat some of them are not genuine handwriting. Therefore, we applied radiocarbon dating
to such kohitsugire attributed to famous persons: Ono no Tohu (894-966), Saigyo

(1118-1190) and Retired Emperor Gotoba (1180-1239). The radiocarbon dating indicatedthat all of them were not their genuine handwritings. They were written by different
persons in a few century later. It suggested that many copies and counterfeits are in
circulation among kohitsugire attributed to famous persons.

P60
Difference in electrolytic deposition of uranium and neptunium
1
OUCHI, K. , OTOBE, H.1, KITATSUJI, Y.1(1 Japan Atomic Energy Agency)
In the previous studies, we focused on deposition following valence changes and investigatedthe electrolytic reduction of U(VI) in weak acid solutions. We found that U(IV) deposits form on
the electrode surface by the electrolytic reduction of U(VI) to U(V). Also, we proposed thedeposition mechanism that a U(IV) hydroxide formed as an intermediate and transforms to U(IV)oxide as a terminal product. In this study, we investigated the electrolytic deposition of Np(V) by
measuring electrochemical quartz crystal microbalance (EQCM) to understand the difference inelectrolytic deposition among actinides. The changes of the reduction current and deposition
amount with time during -0.75 V was applied to reduce Np(V) were measured. The reaction
stopped when the electrode surface was covered with Np deposits. This behavior is different fromthe deposition of U that the reaction continues even if deposits form on the electrode surface.
From the relationship between the quantity of electricity of electrolytic reduction of Np(V) andthe weight of deposits in the pH 4 solution, we found that the specie of deposits is highly likely to
be Np(IV) dioxide (NpO2) and the NpO2 on the electrode surface prevent from reducing Np(V) to
Np(IV) because of high electrical resistance of NpO2.
P61 Safety verification by experimental data for rational regulation of short-lived α-ray
emitting nuclides and development of radiation safety management and educational
methodSHINOHARA, A.1,2, YOSHIMURA, T.3, TOYOSHIMA, A.2, KANEDA, K.1,2, ZHANG, Z.1,
NAGATA, K.3, WATABE, T.4, OOE, K.4, HATAZAWA, J.4, YAMAMURA, T.5, SHIRASAKI,
K.6, KIKUNAGA, H.7, HABA, H.8, WASHIYAMA, K.9(1Graduate School of Science, Osaka Univ., 2Institute for Radiation Sciences, Osaka Univ.,
3Radioisotope Research Center, Osaka Univ.. 4Graduate School of Medicine, Osaka Univ., 5IRNS,

Kyoto Univ., 6IMR, Tohoku Univ., 7ELPH, Tohoku Univ., 8RIKEN, 9Fukushima Med. Univ.)
Research on short-lived alpha-particle emitting nuclides for medical applications is underway
extensively. It is expected that large scale production and medical use of these nuclides will
become popular in the near future. To ensure reasonable radiation management to support the
research and development while ensuring workers and public safety, it is essential to acquire
experimental data on diffusion rate, exhaustion, waste water and surface pollution, which are thebasis of laws and safety management, and to develop a management method. In this study, someexperiments as models for RI production, purification, labeling (chemical synthesis), and animal

experiments were conducted for the purpose of acquiring the data of 211At, 223Ra and 225Ac andtheir disintegrated nuclides. In addition, it was done to investigate the working situation ofradiation workers and medical workers, and to prepare an effective education and training
program.

P62
An attempt to estimate 111In activity by the sum-peak method
OGATA, Y.1, KOJIMA, S.2(1 RIC Medical Division, Nagoya Univ., 2Aichi Medical Univ., ) 200 words
Indium-111 is used for the bone marrow scintigraphy in nuclear medicine. It decays with ahalf-live of 2.8 days by electron capture mainly emitting 171 keV and 245 keV cascading
gamma-rays. We tried to determine the radioactivity by the sum-peak method and the modified
sum-peak method. A radiopharmaceutical injection solution of 111InCl, 74 MBq mL-1, was diluted
and about 50 kBq of the solution was deposited on a thin grass filter and dried. The source wasmeasured by a HPGe detector. The source was put on an axis of the detector varying thesource-to-detector distance. The calculated activities were 67 MBq and 70 MBq by the sum-peakmethod and the modified sum-peak method, respectively. Although, the source actuary included
114m

In, it did not affect the calculation. It was confirmed that the activity of 111In can be determinedby the sum-peak method.
P64 Non-destructive elemental analysis by using characteristic muonic X-rays
KURODA, A.1, TAMPO, M.2, NINOMIYA, K.3, TAKESHITA, S.2, MIYAKE, Y.2, SAITO, T.4 ,KUDO, T.3 , FUJIO, S.4, UENO, Y4, KUBO, M. K.1(1Internatinal Christian University, 2J-PARC, 3Graduate School of Science, Osaka University,
4

National Museum of Japanese History)
A bronze mirror made in China in 2nd century was analysed using negative muon beamat D2 port in J-PARC MLF in this experiment. The diameter of the mirror was about 12 cm and 6
positions on the mirror side were measured. Making process of bronze mirrors is yet unknown indetail. However, by using negative muon beam, non-destructive elemental analysis becomes
possible with selectivity in depth. This method allows us to ignore the surface rust and analyze theelemental composition of interior part. We used 4 germanium detectors and placed them aroundthe sample. Each position is irradiated for about 10 hours to the negative muon beam. The
intensity of the proton beam was 500 kW and the momentum of the muon bean was 35 MeV,
which makes muon to stop about 400 μm from the surface of the sample.
From the spectrum of muonic characteristic X-rays, peaks of Cu, Sn, and Pb are clearlyobserved. Since this method using characteristic muonic X-rays is sensitive to all of the existingelements in the sample, we confirmed that this bronze mirror consists of Cu, Sn and Pb.

P65 Actinide Molecular Ion Formation in Collision/Reaction Cell of Triple Quadrupole
ICP-MS/MSSUZUKI, T.1, YAMAMURA, T.2, ABE, C.3, KONASHI, K.3, SHIKAMORI, Y.4(1Nagaoka Univ. Tech., 2IIRNS, Kyoto Univ., 3IMR, Tohoku Univ., 4Agilent Technologies
Japan)
Recently, the actinide analysis by using ICP-MS has been developing rapidly. In the present
work, a fundamental studies on actinide analysis by quadrupole ICP-MS/MS, Agilent 8900, werecarried out. The used nuclides were U-238, Np-237, Pu-240, Am-241, and Cm-244, respectively.
Np-237 and Pu-240 were used the daughters of Am-244 and Cm-244, respectively. We confirmed
the formation percentages of ionic species of each actinides in several kinds of collision/reaction
cell modes; no gas, hydrogen gas, helium gas, oxygen gas, and BEC (background equivalent tocounts) and LOD (limitation of detection) of each actinide ion are confirmed in each mode. We
also investigated the formation percentages of molecular ions (monoxide ions and dioxide ions)in the case of oxygen gas mode. We found that the formation percentages of actinide ion,monoxide ion, and dioxide ion depends on the oxygen flow rate and on actinides; the dioxide ionof actinide with lower atomic number is easily formed. These phenomena can be explained from aview point of electron configuration of actinides. The obtained results indicate the feasibility of
discrimination of isobaric interference ions.
P66 Gamma-ray irradiation impact of humic substances on apparent formation constants
with Cu(II)SASAKI, T.1, GOTO, R.1, SAITO, T.2, KOBAYASHI, T.1, SUGIYAMA, Y.3(1Graduate School of Engineering, Kyoto Univ., 2KURNS, 3Department of Applied Science,
Okayama Univ. of Science)
Three humic substances (HSs) in solution were irradiated with 60Co gamma-rays in the dose
range of 0–500 kGy at two dose rates, 0.1 and 1 kGy/h. The brownish solutions discolored with
500 kGy irradiation due to the degradation by radiolysis, and the index of degree of humification
as the absorbance ratio of 400 nm / 600 nm was studied using UV-Vis spectroscopy. Apparent
formation constants of Cu(II) with HSs in 0.1 M NaClO4 were determined at 298 K bypotentiometric titration using commercially available Cu ion selective electrode, and the effect of
gamma irradiation on the constants was discussed. The acid dissociation constants of HSs werealso measured in order to determine formation constants by potentiometric titration. No
significant change in apparent formation constants was found, though the concentration ofcarboxylic groups decreased drastically with high radiation exposure.