AHW24-01

Room:301A

Time:May 25 09:00-09:30

Microbial methane production and denitrification in deep aquifer associated with the accretionary prisms
KIMURA, Hiroyuki1∗ ; MATSUSHITA, Makoto1 ; ISHIKAWA, Shugo1
1

Shizuoka University

To understand microbial potential of degradation of organic compounds, fermentation, methanogenesis, and denitrificationin deep aquifer associated with the accretionary prism, the deep groundwater and natural gas samples were collected from 14
deep wells that were drilled to the aquifer. We performed a series of geochemical and microbiological analyses of the samples.
Consequently, methane was the predominant component of the natural gas (51.4 to 99.4%). On the other hand, the natural gas
samples containing N2 (0.6 to 48.6%) were found in some samples. Stable carbon isotopic analysis suggested that the methane
was derived from both biogenic processes and thermogenic reaction. Phylogenetic analysis targeting bacterial 16S rRNA genes
indicated the dominance of H2 -producing fermentative bacteria in the groundwater. In addition to the fermentative bacteria, 16SrRNA genes related to denitrifying bacterium were identified at the sites where N2 was detected from the natural gas. Phylogenetic analysis targeting archaeal 16S rRNA genes revealed the dominance of hydrogenotrophic methanogens in the groundwater.
Anaerobic incubations using the groundwater amended with organic substrates indicated H2 accumulation and rapid methane
production. These results suggested that methane in the deep aquifer is produced by a syntrophic consortium of H2 -producing
fermentative bacteria and hydrogenotrophic methanogens in a wide range of deep aquifer associated with the accretionary prismin Southwest Japan. In addition to methane production, microbial denitrification using methane or organic matters as electron
donors seems to be present in the deep aquifer associated with the accretionary prisms.
Keywords: accretionary prisms, groundwater, subsurface microorganisms, methane production, denitrification

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AHW24-02

Room:301A

Time:May 25 09:30-10:00

Atmospheric circulation controls on the inter-annual variability in precipitation isotope
ratio in Japan
KURITA, Naoyuki1 ; FUJIYOSHI, Yasushi2∗ ; NAKAYAMA, Tomoki3 ; MATSUMI, Yutaka3 ; KITAGAWA, Hiroyuki1
1
3

Graduate School of Environmental Studies, Nagoya University, 2 Institute of Low temperature science, Hokkaido University,
Solar-Terrestrial Environment Laboratory, Nagoya University

This study explored the primary driver of variations of precipitation isotopes at multiple temporal scales (event, seasonal andinter-annual scales) to provide a greater depth of interpretation for isotope data in Japan. Using a new one-year record of theisotopic composition of event-based precipitation and continuous near-surface water vapor at Nagoya in central Japan, we identify the key atmospheric processes controlling the storm-to-storm isotopic variations through an analysis of air mass sources andrain-out history during transport of moisture to the site, and then apply the identified processes to explain the inter-annual isotopic
variability in the historical 17-year long Tokyo station record in the Global Network of Isotopes in Precipitation (GNIP).
An event-based one-year record of HDO in precipitation at Nagoya in Japan showed less seasonal variations, but there is large
variability in HDO on a storm-to-storm basis. In summer, southerly flows transported moisture with relatively higher HDO fromsubtropical marine regions, and the warm rainfall type was relatively enriched in heavy isotopes compared with the other rainfall
events. In contrast, low HDO were observed when northerly winds brought relatively cold air to the observation site. Some ofthe observed isotopic variability can be explained by changes in air mass sources, however this is not enough to have a large
storm-to-storm isotopic range. The additional source of variability is attributed to rainfall amounts occurring both at the site andprior to the site. A clear decreasing trend in HDO with cumulative rainfall over nine-hour back trajectories demonstrates thatrainout history plays a dominant role on the storm-to-storm isotopic variability in the summer. The more isotopically depleted
precipitation is from large-scale weather systems accompanied by prolonged rainfall over wide areas. In winter, low HDO occurred when a cold frontal rainband associated with extra-tropical cyclones (Nangan cyclones) passed south of the Japan coast.
Easterly or northeasterly winds north of the cyclone transport relatively cold air from the mid- or high-latitude regions to the site,
and feed the cold frontal rainband. Therefore, the precipitation related to the Nangan cyclone is characterized by relatively lower
isotopic values than those from another type of cyclone. It follows that the occurrence of Nangan cyclones is the most likely
contributor to changes in winter mean precipitation HDO.
Using the historical record of monthly isotopes in precipitation at GNIP Tokyo station, we explored if factors controllingstorm-to-storm isotopic variability can account for inter-annual isotopic variability. The 17-year variation of summer precipitation H2 18 O was independent of the variation in regional-scale summer precipitation, which is a substitute for cumulative rainfall
along the trajectories. On the other hand, year-to-year variation of H2 18 O related closely to changes in air mass sources. The
relatively higher H2 18 O in summer precipitation corresponded to the higher contribution of warm rainfall to the total summer
precipitation, whereas the inter-annual variation of winter precipitation H2 18 O correlated to the relative ratio of the rainfall from
Nangan cyclones to the total winter precipitation. The activity and storm track of intensified Nangan cyclones were responsiblefor increasing the contribution of cold frontal rainfall fed by northerly winds, and for further decreasing H2 18 O in winter precipitation. These indicate that inter-annual isotopic variability in winter and summer precipitation in the central Japan is primarily
related to changes in meridional moisture transport due to the distinctive difference in isotopic composition between low- andhigh-latitude moisture.
Keywords: Stable water isotopes, East Asian monsoon, Baiu, Southern coastal cyclone

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AHW24-03

Room:301A

Time:May 25 10:00-10:15

Stable isotopes in precipitation all over Japan observed in 2013
ICHIYANAGI, Kimpei1∗ ; TANOUE, Masahiro2 ; YOSHIKUNI, Tsukasa1
1

Graduate School of Science and Technology, Kumamoto University, 2 School of Engineering, The University of Tokyo

Stable isotopes in precipitation (Oxygen-18 and Deuterium) are useful natural tracers for understanding the hydrologicalcycle and reconstructing paleo-climates. There are a lot of observational studies of stable isotopes in precipitation in Japan.
However, most observations on the local scale were conducted only one point or less than several points. The Isotope Mapping
Working Group of the Japanese Association of Hydrological Sciences (JAHS-IMWG) conducted the intensive observation of
stable isotopes in precipitation across Japan throughout 2013 (IOP2013). In this study, seasonal variation and spatial distributionof Oxygen-18 and d-excess at 57 stations across Japan were shown from the preliminary result of the IOP2013. Annual meanvalues in Oxygen-18 show the strong altitude effect from -13permil in the north part to -6permil in the southwest part of Japan.
The Oxygen-18 values along the Pacific coast and the Japan Sea coast of Japan are more and less than -8permil, respectively.
Annual mean values in d-excess ranged from 7permil in the southwest part to 22permil in the northeast part of Japan. The
d-excess values in the north part and along the Japan Sea coast are relatively higher than those along the Pacific coast of Japan.
The differences in d-excess values between the Pacific coast and the Japan Sea coast are mentioned in the previous studies. Mostof the monthly Oxygen-18 values ranged from -15permil to -5permil observed in the north part of Japan, and those values wererelatively high in the spring months (March-June) and low in the winter months (December to February). Most of the monthly
Oxygen-18 values ranged from -10permil to -5permil in the southwest part of Japan, the seasonal variation is small. On theother hand, the monthly d-excess values show strong seasonal variations observed both in the north and southwest parts of Japan.
Those values ranged from 0permil to 40permil in the north part and from 0permil to 30permil in the southwest part of Japan.
Especially in the north part of Japan, monthly d-excess values were extremely high in the winter month (December to February).
The high d-excess values are caused by the strong evaporation from the Japan Sea in the winter months.
Keywords: stable isotope, precipitation, d-excess, all over Japan, Isotope Mapping Working Group

1/1

AHW24-04

Room:301A

Time:May 25 10:15-10:30

Comparison of stable precipitation isotopes between regional isotope simulation and intensive observation around JapanTANOUE, Masahiro1∗ ; ICHIYANAGI, Kimpei2
1

School of Engineering, The University of Tokyo, 2 Graduate School of Science and Technology, Kumamoto University

Stable isotopes in precipitation have been used as tracer of hydrological cycle. However, there are few or no observation
studies throughout Japan at the same time. Here, we organized Isotope Mapping Working Group (IMWG), and conducted theintensive observations for the period from January to December in 2013 at 124 sites. These observational data with high spatial
resolution are vulnerable on a global scale. In this study, the observational data was compared with isotopic compositions derived from isotope regional circulation model. By comparing spatial distribution of isotopic compositions of precipitation, it wasseen that the model captured not only the latitude effect (values decrease with increasing latitude), but also the intensity of theeffect around Japan, except for June to September. The spatial distributions from June to September were uniform around Japan.
Then, in order to compare seasonal variation of isotopic compositions of precipitation between simulation and observation, we
calculated regional averaged seasonal variations according to regional partition of Japan Meteorological Agency. As a result,the model captured observed seasonal variation, such as high values from March to July in the northern part of Japan. However,model overestimated isotopic compositions in January in the western part and the eastern part of Japan. The overestimation was
due to an intensity of the low pressure system in the south coast of Japan around 14 January 2013, because the simulated isotopic
compositions by the low pressure system were higher compared with observed that. We will introduce the result of comparisons.
Keywords: stable isotopes in precipitation, isotope regional circulation model

1/1

AHW24-05

Room:301A

Time:May 25 10:30-10:45

A two-year record of stable isotope characteristics of monthly rainfall at the Douala andYaounde urban cities, Cameroon
WIRMVEM, Mengnjo jude1∗ ; OHBA, Takeshi1 ; BAFON, Tasin godlove2 ; KAMTCHUENG, Brice tchakam3 ;TAYLOR, Eldred tunde4 ; ASAAH, Asobo nkengmatia elvis5 ; WOTANY, Engome regina6 ; OOKI, Seigo1 ;FANTONG, Wilson yetoh7 ; AYONGHE, Samuel ndonwi6
1

Department of Chemistry, School of Science, Tokai University, 2 Compagnie Miniere Du Cameroun, 3 Graduate School of
Science and Engineering for Education, University of Toyama, 4 IEMQC, Njala University, 5 Department of Earth & Planetary
Sciences, Tokyo Institute of Technology, 6 Department of Environmental Science, Faculty Science, University of Buea, 7 Instituteof Mining and Geological Research, Cameroon
The stable isotopes of oxygen (18 O) and hydrogen (2 H) in precipitation are useful tools in environmental studies includinghydrological and climatological investigations. Like in most of tropical Africa, stable isotope data of rainfall is regrettably limitedin Cameroon. As a contribution to desired data, 43 monthly rainfall samples have been collected from January 2013 to December
2014 in the urban cities of Douala and Yaounde (in the tropical evergreen forest of Cameroon). The objectives were to produce
local meteoric water lines (LMWLs), define the spatial and temporal variations of the stable isotopes and controlling factors.
The conventional delta (δ) 18 O-δ 2 H diagram for the two-year data gave the regression lines: δ 2 H= 7.92δ 18 O + 12.99 (R2 =0.97)
and δ 2 H = 8.35δ 18 O +15.29 (R2 = 0.99) for Douala and Yaounde, respectively. These lines represent the LMWLs for the twocities. The similarity of slopes to the Global Meteoric Water Line (GMWL) of 8 indicates that rain formation processes in bothareas occurred under conditions close to isotopic equilibrium with insignificant evaporation effect during precipitation. Douala
precipitation showed a wide range of δ 18 O from -5.22 to -0.75 ‰, mean of -2.71 ‰ (2013); and -5.26 to -1.28 ‰, average of-3.09 ‰ (2014). A similar range was observed in Yaounde for δ 18 O from -5.20 to 1.81 ‰, mean of -2.49 ‰ (2013); and -5.86
to -0.66 ‰, average of -3.37 ‰ (2014). The large range suggests varied controls on precipitation in both localities. Despite thecloseness of the Douala sampling point to the Atlantic Ocean (35 km), the weighted mean d-excess value of 13.12 ‰ was higher
relative to 10 ‰ of the Atlantic moisture. Further inland in Yaounde (191 km), a relatively higher weighted mean d-excess value(14.55 ‰) was also observed. The high d-excess values in both cities reflect an addition of recycled continental moisture to
precipitation. The additional moisture is likely from the evergreen rainforest and a network of rivers in the areas. Weighted mean
δ 18 O and δ 2 H values for the sampling period were -3.27 ‰ and -13.01 ‰, and -3.07 ‰ and -10.04 ‰ in Douala and Yaounde,respectively. The slight increase in weighted mean δ values from Douala to inland Yaounde reflects a lack of continental effectprobably due to the additional supply of inland recycled moisture to rain. Monthly weighted mean δ values showed a definite
seasonal variability in both areas. Isotopically enriched and depleted values were observed during the pre- and post-monsoon low
rainfall and heavy monsoon rains, respectively, in agreement with the amount effect of tropical low latitude rains. This effect isprobably controlled by northward and southward oscillation of the Intertropical Convergent Zone and associated air masses. The
δ 18 O and δ 2 H of rainfall in the tropical cities of Douala and Yaounde show a similar temporal variability that is mainly controlled
by the addition of inland recycled moisture and amount effect. The generated isotope data and LMWLs can be used as tools forgroundwater recharge and atmospheric moisture circulation studies in the region.
Keywords: Stable isotope variation, Local meteoric water line, Amount effect, Moisture recycling, Douala-Yaounde, Cameroon

1/1

AHW24-06

Room:301A

Time:May 25 11:00-11:15

Saline groundwaters in and around the Osaka Basin and those origins
MASUDA, Harue1∗ ; SHINTANI, Tsuyoshi1 ; MITAMURA, Muneki1 ; MARUI, Atsuhisa2 ; MORIKAWA, Noritoshi2 ;NAKANO, Takanori3
1

Graduate School of Science, Osaka City University, 2 AIST, 3 Research Institute for Humanity and Nature

Many saline waters including high amounts of Fe and occasionally CO2 and bicarbonate ions are issuing in the mountainous
areas surrounding Osaka Basin. Among those waters, Arima hotspring is the most famous and the hot saline water has beencalled Arima-type brine, which is characterized by heavy oxygen isotope shift and high 3He/4He ratio similar to the mantle
derived component (e. g., Nagao et al. 1981). High CO2 and 3 He/4 He saline waters similar to the Arima-type brine have been
known at Ishibotoke at southern mountainous area of Osaka (e. g., Matsumoto et al., 2003). Saline groundwaters were found in
the Quaternary sediments and underlying basement rocks of Osaka Basin. Those waters occasionally contained high 3 He/4 He
ratios and were suggested the similarity to the Arima-type brine (Morikawa et al., 2008). In this study, saline waters containing>500 mg/L chloride ions and >400 mg/L HCO3 − ions were three-dimensionally mapped assuming the well depth was the
sampling depth of groundwater to see the relationship between the occurrence of saline waters and geological structure. Then,the origins of saline waters were estimated from the relationships among hydrogen and oxygen isotope ratios and chloride ion
concentrations.
The saline waters distribute characteristically along the boundary between sedimentary basin and surrounding mountains andthe bottom of the basin including the lowermost sedimentary formation and basement rocks. The former is usually along active
faults; Arima-Takatsuki Tectonic Line at the north and Ikoma faults system at the east and south. These faults would work as
recharging paths of deep groundwater and seawater might inflow using these faults. The latter does not have clear relationship to
the tectonic structure.
Hydrogen and oxygen isotope ratios of saline waters are plotted on a mixing line of seawater and local meteoric water. If
seawater is one of the end members, relationships of chloride concentration and those isotope ratios also give mixing lines.
Although these relationships of saline waters at <100 m depths show the mixing lines, the those of deeper ones do not give
simple mixing lines; chloride concentration and oxygen isotope ratio of saline waters at 100-500 m depths are on the mixing
line while hydrogen isotope ratios are smaller than those affected by seawater, and the saline waters >500 m depth have smaller
isotope ratios than those contributed by seawater. Compared with the Arima-type brine, oxygen shift is not large for these saline
waters, however, such an isotope characteristics would be on the formation process of Arima-type brine.

Keywords: Deep groundwater, Arima-type brine, active faults, hydrogen and oxygen isotope ratios

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AHW24-07

Room:301A

Time:May 25 11:15-11:30

On deep-seated salty groundwater mixed into shallow groundwater flow system in Sagae
district, Yamagata, JapanYASUHARA, Masaya1∗ ; MORIKAWA, Noritoshi1 ; INAMURA, Akihiko1 ; TAKAHASHI, Hiroshi11Geological Survey of Japan, AISTOn deep-seated salty groundwater mixed into shallow groundwater flow system in Sagae district, Yamagata, Japan

Keywords: deep-seated groundwater, salty water, shallow groundwater flow sytem, mixing ratio, isotopes

1/1

AHW24-08

Room:301A

Time:May 25 11:30-11:45

Chemical properties of deep groundwater at coastal area
MACHIDA, Isao1∗ ; ONO, Masahiko1 ; KOSHIGAI, Satoru1 ; IKAWA, Reo1 ; MARUI, Atsunao1
1

Geological Survey of Japan, AIST

Two drilling surveys up to a depth of 150m have been carried out close to shoreline at Suruga bay, Shizuoka Prefecture. The
properties of groundwater flow can be discussed by the chemical and isotopical data from geological core.
Keywords: Borling survey, Pore water, Coastal Area, Boundary of saline and fresh water, Isotopes, Water quality

1/1

AHW24-09

Room:301A

Time:May 25 11:45-12:00

Vertical profiles of stable isotopic composition of groundwater in Abukuma granite: comparison with radiocarbon dates
TAKAHASHI, Hiroshi1∗ ; TAKAHASHI, Masaaki1 ; TSUKAMOTO, Hitoshi1 ; YASUHARA, Masaya1 ;KAZAHAYA, Kohei1 ; INAMURA, Akihiko1
1Geological Survey of Japan, AIST

Groundwater in hard rock aquifer mainly circulates along fractures and fissures, and the flow is mainly governed by the physical properties of the rock heterogeneities such as opening, spacing and connectivity. The present study reported stable isotopic
compositions of groundwater in granite fractures. The study site is situated at the northern part of the Abukuma Mountains inFukushima Prefecture, northeastern Japan. To collect groundwater in granite fractures, three drillings were performed. Groundwater sample in the present study were taken from fractures in the weathered-fissured zone and fracture zone of granite. The
radiocarbon dates of groundwater ranged from modern to ˜16 ka. The vertical profiles of radiocarbon dates indicate a relatively
constant age of 10-16 ka for groundwater deeper than 100 m.
Stable isotopic composition suggests that all groundwater originated from meteoric water. The shallow around-groundwaters
indicated wide isotopic range, since the monsoon climate will produce the seasonal isotopic variations of precipitation. The
range of stable isotopic compositions of stream waters around Mt. Utsushiga-take showed slightly lower than that of aroundgroundwater. This suggested that around-groundwater is unlikely originated from recharge area in Mt. Utsushiga-take, although
the local groundwater flow was not clarified. Groundwater flow from the mountain to the drilling sites might be blocked off,
owing to the faults and tectonic line between Mt. Utsushiga-take and the drilling sites.
The isotopic values of borehole-groundwater beneath the depth of 100 m showed significantly lower values than those ofaround-groundwaters: the isotopic depletions are 5-10 ‰ in hydrogen isotopic ratio and 1.5-2.0 ‰ in oxygen isotopic ratio.
These indicate that they were recharged under colder climate conditions and/or at higher altitudes. The stable isotopic compositions of stream water of the Mt. Utsushiga-take did not represent the same ranges with those of borehole-groundwater.
Radiocarbon dates of groundwater beneath the depths of 100 m ranged 10-16 ka, corresponding to be the last glacial period,
Oldest, Older and Younger Dryas periods. The colder climate enhances the isotopic fractionation during the air mass transportation and rainfall. Some studies reported the low values of isotopic compositions of groundwater due to recharge under the clod
climate such as last glacial period.
This study is regulatory support research funded by the Nuclear and Industrial Safety Agency, Ministry of Economy, Tradeand Industry, Japan.

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AHW24-10

Room:301A

Time:May 25 12:00-12:15

Isotopic characteristics of acid springs in Shunomata river basin in Mt. Chokai volcano
HAYASHI, Takeshi1∗ ; YASUHARA, Masaya2 ; MORIKAWA, Noritoshi2 ; TAKAHASHI, Hiroshi2 ;ASAI, Kazuyoshi3 ; KUSANO, Yukiko4
1

Akita Univ. Faculty of Education and Human Studies, 2 GSJ, AIST, 3 Geo-science Laboratory, 4 Graduate School of Frontier
Sciences, The University of Tokyo
There are some rivers that have low pH and deposition of Iron oxides on the east side of Mt. Chokai volcano. Shunomata
river basin has some limonite ore deposits on the river bed of tributaries (EL: approximately 900m). These ore deposits are
considered to have made by acid springs that are characterized by low pH (about 3 to 5) and relatively high temperature (about
20 to 25 degree Celsius). Also, previous studies pointed out that pH of the acid springs have decreased after a volcanic activityof Mt. Chokai in 1974. However, there are quite few studies on the origin and groundwater quality evolution process of the acidsprings. Therefore, this study aims to clarify these points. We will show the results of measurements of major dissolved ions andenvironmental isotopes.
Temperature and pH of the acid springs showed 15.5 to 19.5 degree Celsius and 2.8 to 3.0, respectively. As for major dissolved
ions, groundwater quality was characterized by high concentrations of SO42- and Cl (117 to 181 mg/L and 66 to 106 mg/L).
Comparing these results with that of ”Detsubo” spring that is located on the north side of Mt. Chokai volcano and is famous
for low temperature (about 7 degree Celsius) and low pH (about 4.5), groundwater quality was largely different. Stable isotopic
ratios of oxygen and hydrogen were about -11.5 per-mil and -68 to -69 per-mil, respectively. Elevation of recharge area of theacid springs was estimated more than 1,600 masl.
The results of this study suggest that there are some groundwater quality evolution systems of acid springs in Mt. Chokai
volcano.
Keywords: acid springs, environmental isotopes, limonite ore deposits, Mt. Chokai Volcano

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AHW24-11

Room:301A

Time:May 25 12:15-12:30

Groundwater age determination by using 85 Kr and its verification by other hydrogeochemical tracers
KAGABU, Makoto1∗ ; MATSUNAGA, Midori1 ; ISHII, Tomohisa1 ; MOMOSHIMA, Noriyuki2 ; SHIMADA, Jun1
1

Graduate School of Science and Technology, Kumamoto University, 2 Radioisotope Center, Kyushu University

Krypton 85 (85 Kr) is a man-made trace gas from reprocessing plant origin whose atmospheric concentrations have been increasing over the past few decades. As it is soluble in water, it can be used as groundwater age indicators over timescales ranging
from a few years to a few decades. In this study, 85 Kr specific activities in groundwater were measured with an on-site dissolved
Kr gas extraction system using an external flow through type hollow fiber membrane modified after Ohta et al. (2009).
85
Kr specific activities in groundwater were confirmed at 3 sites in Miyakonojo basin, south-western Japan, considering regional groundwater flow system. Estimated groundwater age were 2 years, 11 years and 60 years in the recharge, intermediateand stagnant discharge areas along the groundwater flow line, respectively. In order to verify these 85 Kr ages, we also measured
other age tracer gases such as Sulfur hexafluoride (SF6 ) and Chlorofluorocarbons (CFCs) at the same sampling wells of 85 Kr
measurement. The result of the SF6 age dating in the three locations were well harmonized with the 85 Kr dating results; theSF6 age were 1 year, 23 years and over 60 years. However, CFCs could not show reasonable groundwater age due to the local
contamination by the urban and industrial origin CFCs.
The seasonal fluctuation of the stable isotopes (δ 18 O and δD) in groundwater were also measured to evaluate the comprehensive groundwater age tendency. Relatively high seasonal fluctuation of the stable isotopes were measured only in the shallow
unconfined well site at the recharge area, which reflect the seasonal isotopic fluctuation in the precipitation. This is anotherevidence of the relatively young groundwater characteristics to support the 85 Kr and SF6 age in the recharge area.
Keywords: Krypton-85, Groundwater age, Groundwater flow system, Sulfur hexafluoride, Groundwater age tracer, Miyakonojo
basin

1/1

AHW24-P01

Room:Convention Hall

Time:May 25 18:15-19:30

Stable isotopic ratio of atmospheric vapor in Hiratsuka, Japan
TAKAGI, Kenta1∗ ; INOUE, Takayuki2 ; OOKI, Seigo2 ; OHBA, Takeshi2
1

Course of Chemistry, Graduate School of Science, Tokai University, 2 Course of Chemistry, School of Science, Tokai University

The origin of water vapor in atmosphere could be variable, for example, the water vapor at a specific point is transported froma distance or the vapor is generated from surface water near the specific point. If there is equilibrium between precipitation
and atmospheric vapor, the hydrogen and oxygen isotope ratios (δD and δ 18 O) of atmospheric vapor are plotted theoreticallyin meteoric water line. Recently, δD and δ 18 O of atmospheric vapor is used as a tracer for atmospheric water cycle, because
the water vapor is much ubiquitous than precipitation (Tsunakawa and Yamanaka, 2005). However, Japan has various water
resources. From this aspect, δD and δ 18 O of atmospheric vapor could be disturbed by several factors such as seasonal variationand difference vapor source of supply (Hiyama et al, 2008). In this study, we investigated the seasonal isotopic variation of
atmospheric vapor and precipitation. Then, we also examined surface water on ground and transpiration from leaves of plants,
as the candidates of atmospheric vapor sources.
Precipitation and atmospheric vapor were collected on the roof of a No.17 building at Shonan campus, Tokai University fromMay 2013 to Dec. 2014. Precipitation samples were collected based on the method described by Negrel et al. (2011) andYoshimura (2002). The duration of collection varied from hours to days. Precipitation samples were percolated through 0.2 µm
filter, and kept into a 100 ml low-density polyethylene bottle. Atmospheric vapor samples were collected by the cryogenic trap
cooled with ethanol-dry ice mixture (Tsunakawa and Yamanaka, 2005). The total number of precipitation and atmospheric vapor
samples were 142 and 90, respectively. The atmospheric vapor may be supplied by surface water on ground and transpirationfrom leaves of plants, therefore surface water samples were collected on 4 points (pond or river) near a No.17 building from Apr.
to Dec. 2014. Transpiration samples were collected at 6 points near a No.17 building from Aug. to Dec. 2014 by polyethylene
bag which covers leaves and twig over 1-4 days. Surface water and transpiration samples were percolated through 0.2 µm filter,and kept into a low-density polyethylene bottle. The total number of surface water samples was 6 in each points and the total
number of transpiration samples were 16. δD and δ 18 O of samples were measured by a Cavity Ring-Down Spectrometer analyzer(model L2120-i from PICARRO). Some data of rain water, which were sampled several times in a day, were processed to be theweighted average value.
Precipitation showed wide variations in δD and δ 18 O from -124.7 to +9.1 ‰ and -16.6 to -0.6 ‰, respectively. Atmosphericvapor also showed wide variations from -223.5 to -82.2 ‰ and -31.2 to -11.6 ‰, respectively. The δD-δ 18 O relationship ofprecipitation and atmospheric vapor were regressed by δD=8.5δ 18 O+17.4 (R2 =0.95) and δD=6.6δ 18 O-2.6 (R2 =0.92), respectively. The d-excess values (d=δD-8δ 18 O) of precipitation has a variation from -0.7 to 31.4 ‰. The d-excess of atmosphericvapor shows a definite seasonal trend within the range between 5.6 and 35.7 ‰. The isotopic compositions of atmospheric vapor
almost agreed to the calculated value from precipitation assuming isotopic equilibrium with the exception in May 2014, wherea significant difference between the observed and the calculated isotopic ratios. Such a composition seemed to be generated by
the completely evaporated vapor originating in precipitation (= bulk vapor). In Jun. 2014, the d-excess of atmospheric vapor was
deviated from the seasonal variation. Such a deviation can be caused by the addition of evaporated vapor from local surface water.
The δD-δ 18 O plots of all sample suggested that atmospheric vapor was mainly composed by three kinds of vapor, namely, thevapor equilibrated with precipitation, the bulk vapor and the vapor evaporated from the local surface water near the observation
point.
Keywords: Precipitation, Atmospheric vapor, Stable isotope

1/1

AHW24-P02

Room:Convention Hall

Time:May 25 18:15-19:30

Characteristics of water quality in groundwater near the coastal area at northern part of
Fukushima Prefecture
YABUSAKI, Shiho1∗
1

Faculty of Symbiotic Systems Science, Fukushima University

The coastal area at northern part of Fukushima Prefecture suffered big damage by a tsunami generated in 11 March, 2011. The
groundwater around these areas was affected by the tsunami. These areas were greatly affected by the accident of the nuclear
power plant, and the radioactive contamination of a plant, soil and farm products became serious problem. It is important to makeclear the groundwater flow in these areas because of considering the solution to the serious problem. The objective in this study
is to uncover the groundwater flow system and residence time of spring water and groundwater in the coastal area at northernpart of Fukushima Prefecture.
As a result of field survey, EC values of spring water and groundwater were under 30 mS/m in most sites. Almost site shows
lower than 7 of pH values, however, in several sites show higher than 7.5 of pH. The water temperature is from 13 to 18 degree
Celsius in almost site, but some site shows the lower than 12 degree Celsius. So, it is considered that the groundwater andspring water which show lower than 12 degree Celsius were recharged in the relative high altitude area. Water quality of shallow
groundwater is Ca-HCO3 type, but that of spring water and deep groundwater is Na-HCO3 type. Since the SiO2 concentrationof these spring water and deep groundwater is relatively high, it is expected that the residence time of these water are relatively
long.
The δ 18 O values show from -10 to -6 ‰ and δD values show from -65 to -35 ‰. The altitude effect in this area is -0.16 ‰/100
m of δ 18 O and -0.6 ‰/100 m of δD.
In future, we will analyze the 3 H, CFCs and SF6 , and will consider the residence time and groundwater flow system.
Keywords: Minamisoma City, Soma City, Namie City, water quality, stable isotopes, recharge area

1/1

AHW24-P03

Room:Convention Hall

Time:May 25 18:15-19:30

Effects of mountainous water recharge to groundwater quality of alluvial fan
NAKAMURA, Takashi1∗ ; NISHIDA, Kei1 ; KAZAMA, Futaba1
1

ICRE, University of Yamanashi

In this study, the hydrogen and oxygen stable isotopes (dD and d18O) and chemical compositions of environmental water were
employed to identify the effects of mountainous water recharge for groundwater quality on alluvial fan.
The study area is Midaigawa alluvial fan, located in western Kofu basin on central Japan, which is formed by Raised-bed River
discharged from the mountain watershed.
The groundwater samples were collected from 25 deep wells (100˜300m) in June-2010, Novenber-2011 and Novenber-2012.
Those wells were located on Midaigawa alluvial fan and adjacent mountain. Four End-member mixing analysis using isotope
value and chemical compositions revealed spatial variation in the contribution ratios for various groundwater sources. This
presentation focused on groundwater recharge from mountain area to alluvial fan. It also found the relationship between contributions of mountainous water on groundwater and chemical composition.
Acknowledgment
This study was supported by the Kurita water and environment Foundation (No.14B063).
Keywords: Groundwater recharge, Alluvial fan, Isotopes, End-member mixing analysis, Mountainous water resource

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AHW24-P04

Room:Convention Hall

Time:May 25 18:15-19:30

Change of rainfall runoff processes with the erosion of the volcano body: a case study of
Mt. Ontake
ASAI, Kazuyoshi1∗ ; TSUJIMURA, Maki2
1

Geo-science laboratory, 2 University of Tsukuba

To clalify the change of rainfall-runoff processes with the erosion, long-term monitoring of stream-runoff and EC were conducted on two basins in Mt. Ontake.
Keywords: rainfall-runoff, Mt. Ontake, erosion, hydrograph separation, direct runoff, recharge rate

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AHW24-P05

Room:Convention Hall

Time:May 25 18:15-19:30

Helium isotopes in groundwaters from the middle and lower reaches of the Tone River,Japan.
MORIKAWA, Noritoshi1∗ ; YASUHARA, Masaya1 ; NAKAMA, Atsuko1 ; INAMURA, Akihiko1 ;TAKAHASHI, Masaaki1
1

Geological Survey of Japan, AIST

There exist three regions in the Kanto plain, central Japan, whose groundwater is characterized by a high Cl− concentration:(1) floodplains and deluvial uplands along the lower reaches of the Tone rivers (Ibaraki and Chiba Prefectures), (2) south-east
parts of the Gunma Prefecture along the middle reaches of the Tone rivers, (3) central parts of the Kanto plain, south east of the
Area (2).
The high-chloride groundwaters from the central parts of the Kanto plain are characterized by the following features; (a)helium isotopic ratios (3 He/4 He) are relatively homogeneous with an end member of 0.8-1.1 x 10−6 , (b) helium-4 concentration
show positive correlation with chloride concentration (Morikawa et al., 2006). Morikawa et al (2014a) investigated the noble
gases in the deeper groundwaters (hot springs) in the central parts of the Kanto plain and the high-chloride groundwaters fromsouth-east parts of the Gunma Prefecture to elucidate the origin of water and chrolide component. Low 3 He/4 He ratios in the
hot springs indicate that there is almost no interconnectivity between the high chloride groundwater and hot spring water aroundthese regions. In contrast, both 3 He/4 He ratio and correlative 4 He and Cl− concentration in the high-chrolide groundwatersfrom south-east parts of the Gunma Prefecture are similar to those in the groundwaters in the central part of the Kanto Plain.
They suggest that these groundwaters and their constituents are closely related to each other in their origin. Although there isno hydrogeological connectivity, groundwaters from some part of the lower reaches of the Tone river also show similar helium
isotopic ratios (3 He/4 He) and positive 4 He-Cl correlation (Morikawa et al., 2014b).
In this study, we further conducted complementary investigation for the groundwaters between the region of middle reach andlower one of the Tone River. Low Cl− with low 4 He groundwaters exist in this region. Combined with previous and present
results, the groundwaters along the Tone River implies a mixture of young meteoric water and high chloride saline water bearing
with high 4 He which seems to be stagnant nature.
References: Morikawa et al. (2006) JPGU 2006, H121-004, Morikawa et al. (2014a) JPGU 2014, AHW25-12, Morikawa etal. (2014b) JAHS 2014, P18.

Keywords: Helium, Groundwater, Tone River, Kanto Plain, Chloride Ion, Noble Gas

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AHW24-P06

Room:Convention Hall

Time:May 25 18:15-19:30

Visualization of the deep-seated fluid ascending along the fault
NISHIYAMA, Nariaki1∗ ; TANAKA, Kazuhiro1 ; SUZUKI, Koichi2
1

Yamaguchi University, 2 Central Research Institute of Electric Power Industry

1. Introduction
It is known that deep-seated fluid is highly saline water and includes gas. In addition, it is thought that fluid rises from thedeep part under the ground. Therefore it is thought that the deep-seated fluid has a big influence on environment of deep partgroundwater.
It is known that the groundwater mix deep-seated fluid derived from the slab, based on the result of geochemical analysis
at the inland from Northeast Yamaguchi to Southwest Shimane (Murakami and Tanaka, 2009). The most of these fluids spout
out at the surface of the ground. However, the fluid erupted from only the flowing borehole in Tokusa basin, Yamaguchi. We
cannot identify the deep-seated fluid if we don’t play drilling operation. Therefore, we cannot identify the fluid if we play field
investigation. And, distribution and flow of the deep-seated fluid is not known in underground.
I used the CSAMT method in this study in Tokusa Basin and tried visualization of the distribution of the deep-seated fluid
underlying underground.
2. Geological setting
The bedrock consisted of Late Cretaceous welded tuff and rhyolitic lava of Abu group in Tokusa Basin. Sediments of the
Quaternary period cover the bedrock in the basin. Based on the result of gravity survey, thickness of the sediments are up to
about 200 m. The point of the fluid spout out from the borehole is three places in total and is distributed along Tokusa-Jifuku
fault dislocation estimated by NE-SW direction.
3. Results
Groundwater from the borehole : Electric conductivity of the groundwater is higher than general groundwater (211 mS/m,
426mS/m and 1,310 mS/m). Water quality type are NaCl type or NaHCO3 type. Though the groundwater is an inland, it ishighly saline water.
The surface groundwater : Electric conductivity of the groundwater varied considerably ranging from 5.80 to 22.8 mS/m.
The water quality type of most surface groundwater is CaSO4 type. However, the groundwater of the north side of the fault tends
to be slightly higher Na+ and Cl- than the groundwater of the south side of the fault. Based on the result of groundwater level
survey, the surface groundwater flows to the river of the northwest direction across the fault from the southeastern direction.
Distribution of resistivity : Fig-1B shows the resistivity profile line X-X’. As a result, H1 was a high resistivity zone morethan 1,000 ?m and caught distribution of the bedrock. And, L1 and L2 were low resistivity zone less than 100 ?m and 30 ?m.
These low resistivity zone is the area where the deep-seated fluid gets mixed with.
4. Discussion
The area of L1 where low resistivity is distributed in Fig.1B is known that distribution Tokusa-Jifuku fault and the highly
saline groundwater is identified in the direct top. As a result, L1 that low resistivity zone catches the rise of the deep-seated fluid
along the fault. It is thought that the deep-seated fluid ascending along the fault penetrates in sediment, because low resistivity
zone L2 distributes the north side of the fault and the shallow groundwater of the NaCl type distributes. Namely, the deep-seatedfluid ascending Tokusa-Jifuku fault (L1) mixes the shallow groundwater in sediments, but the flow is regulated by the shallow
groundwater system which flows from the south of the Tokusa Basin to the north (L2). The plural ratio resistivity distribution
across Tokusa-Jifuku fault shows similar tendency to Fig.1B. Therefore, the deep-seated fluid distributes not only the place where
the fluid spouts out from the borehole but also in the range of at least 1.5km along the fault in the underground of the Tokusa
Basin.
When the fluid spouts out from the borehole in the place where the sediments distributes, it is necessary to considerate that thefluid may be widely distributed along fracture zone such as faults in the underground.

Keywords: Deep-seated fluid, CSAMT method, Tokusa-Jifuku fault

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AHW24-P06

Room:Convention Hall

Time:May 25 18:15-19:30

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AHW24-P07

Room:Convention Hall

Time:May 25 18:15-19:30

Secular change of stable carbon isotopic ratio in groundwater samples during their storage
in laboratory
TAKAHASHI, Hiroshi1∗ ; HANDA, Hiroko1 ; MINAMI, Masayo2 ; ARAMAKI, Takafumi3 ; NAKAMURA, Toshio2
1

Geological Survey of Japan, AIST, 2 Center for Chronological Research, Nagoya University, 3 National Institute for Environmental Studies
Carbon isotope is a useful tracer in order to identify carbon sources and behavior in the fields of biogenic and geochemical
processes. However, the isotopic change during the storage in sample bottles until the measurement sometimes occurs owing
to carbon exchange between DIC and atmospheric CO2 , biogenic activity and/or carbonate mineral reactions (deposition anddissolution). The present study examined the secular change of carbon isotopic compositions, 13 C/12 C and 14 C/12 C, of DIC inwater samples.
The water samples examined are surface seawater (RICE-W01), hot spring water (RICE-W03: high salinity and high DIC,
W04: high salinity and low DIC), shallow groundwater (RICW-W05: low salinity and low DIC), deep groundwater (RICE-W06:
low salinity and low DIC), and RO water prepared by dissolving chemical regent (RICE-W07: low DIC, W08: high DIC). The
carbon isotopic measurements were carried out on the samples which storage periods ware 860 days for W01, 560 days for
W03-W06, and 480 days for W07 and W08.
Secular changes of δ 13 C ranged from -5.4 ‰ to -0.2 ‰. The large isotopic change might be caused by decomposition ofbiogenic carbon in water samples, since the Keeling Plot showed the biogenic features of δ 13 C of added carbon. The storage examination suggested that some water samples did not change the δ 13 C values widely for years. The biogenic activity is prevented
by regent addition to water samples. Commonly HgCl2 or NaN3 is used, but it is hard to use them for groundwater samples
because sampling filed is not situated in the chemical controlled site. The present study confirmed that isotopic change reduced
by NaOH instead of poisonous materials.
The materials of storage bottles are also influenced the secular isotopic change. The present study compared the δ 13 C valueand 14 C concentration among the glass, PAN plastic and PP plastic bottles. The δ 13 C value was relatively constant for all bottles,
while the 14 C concentration was clearly different. The contamination of modern carbon was detected for PP plastic bottle.
This work was supported by the Japan Society for the Promotion of Science, Grant-in-Aid for Scientific Research C (No.
26340017): Radiocarbon Intercomparison on Chemical Experiments, Water series (RICE-W).

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