HTT08-01

会場:101B

時間:5 月 26 日 09:00-09:15

根尾谷断層水鳥断層崖における UAV を用いた DSM の RTK-GPS 測量による精度評
価Accuracy evaluation of UAV-measured DSM by RTK-GPS on Midori fault scarp of Neodani active fault, Gifu Prefecture, Japan佐藤 浩 1∗ ; 内山 庄一郎 2
SATO, Hiroshi, P.1∗ ; UCHIYAMA, Shoichiro2
1
1

日本大学文理学部, 2 防災科学技術研究所
College of Humanities and Sciences, Nihon Univ., 2 National Research Institute for Earth Science and Disaster Prevention

樽見鉄道水鳥駅周辺の根尾谷断層による水鳥断層崖を対象に，リアルタイムキネマティック GPS によって平面位置が悪く見積もって 8 mm の精度をもつ基準点を６点設置し，その標高値を正解として，UAV の撮像画像から生成した DSMの標高の計測精度を評価した．その結果，崖上の３点でそれぞれ 3 cm，− 8〜− 9 cm，− 5〜− 7 cm の較差となった．
また，崖下の３点でそれぞれ 40 cm 前後，− 3〜− 4 cm，− 0.6〜− 2 cm となった．崖下の１点を除けば，DSM は概ね10 cm 未満の精度のあることが分かった．

謝辞
仮想基準点方式による RTK-GPS の測量結果は玉野総合コンサルタントから提供いただいた．

参考文献
内山ほか, 2014, 小型 UAV と SfM ソフトウェアを用いた断層変位地形把握の試み−根尾谷断層水鳥断層崖を例に−, 活断層研究, 40, 35-41.
キーワード: 断層, UAV, GPS, リアルタイムキネマティック, DSM, 仮想基準点
Keywords: fault, UAV, GPS, RTK, DSM, VRC

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HTT08-02

会場:101B

時間:5 月 26 日 09:15-09:30

Structure from Motion および様々なカメラを用いた精度比較
Comparison of accuracy using various cameras and Structure from Motion
小林 勇介 1∗ ; 石川 正樹 2 ; 渡辺 悌二 3KOBAYASHI, Yuusuke1∗ ; ISHIKAWA, Masaki2 ; WATANABE, Teiji311

北海道大学環境科学院環境起学専攻, 2 北海道大学環境科学院環境起学専攻, 3 北海道大学
Graduate School of Environment Hokkaido Univ., 2 Graduate School of Environment Hokkaido Univ., 3 Hokkaido University

Recently, the significance of Unmanned Aerial Vehicle (UAV) and Structure from Motion (SfM) has been increasing in geoscience field to understand geomorphological phenomena. These two new technologies can be used inexpensively, easily, rapidly
and automatically in comparison to a traditional photogrammetry method, so that geomorphological changes that are caused byvarious agencies can be estimated at close interval. For these reasons, geomorphological information (e.g. DEM and Orthophotograph) can be made flexibly to suit researcher preferences. Most mountain national parks in Japan have been suffered fromserious trail erosion for long time. Especially, some mountain trails in Daisetsuzan National Park in Hokkaido, northern Japan,
have been eroded in a few meters in depth. This serious soil erosion bothers national park managers, mountain hikers and alsoalpine vegetation. It is important for park managers to accurately and easily understand that eroded soil volume and geomorphological changes. For the purpose of the management, this study demonstrated two new technologies and evaluated qualityof DEMs and orthophotographs. This study aims: (1) to demonstrate two new technologies under various conditions, and (2) tounderstand differences of accuracy in some cameras and some software to make three-dimensional data.
This study used two methods to take photographs: (1) UAV (DJI Phantom2 +Vision) at 5 m, 10 m and 20 m flying height; and2) a monopod at distance of 1.5 m and 3 m from the ground surface at 24 viewpoints. In order to compare difference of accuracy of cameras, Ricoh GR, Ricoh CapioR7 and DJI camera were used with UAV; and Ricoh GR, Canon power shot SX150IS,
NikonD90, Panasonic LUMIX DMC TZ-60, Ricoh CapioR7, SONY Cyber-shot DSC-TX5, Ricoh GR, and Panasonic LUMIXDMC-GX1 camera were used with monopod. Sixty pictures were taken by the cameras on UAV, and 24 pictures were taken by
the cameras on the monopod. Moreover the following software was used for making DEMs and orthophotographs: Visual SfM(free), Photo Scan Pro (commercial) and 123Dcatch (free). In place of the actual micro-topography, artificial sheet and blocks
were placed on a flat ground for targets when taking photographs to evaluate absolute positional accuracy.
The analysis of the photographs taken with UAV by Photo Scan Pro shows that the average absolute positional error score wasalmost the same in Ricoh GR (0.001 cm) and Ricoh CapioR7 (0.042 cm) at the 5-m flying height. But, at the 10-m flying height
the average absolute positional error score was as large as 1.371 cm in Ricoh CapioR7. On the other hand, the score for Ricoh
GR was 0.039 cm. At the 20-m flying height, the score for Ricoh GR was 0.066 cm. In this flying height, Ricoh CapioR7 was notsuitable due to bad resolution. DJI camera was not suitable in all cases. When using a monopod, the average absolute positional
error score was less than 1 mm in all cameras from distance of 1.5 m (Ricoh GR: 0.89 mm, Canon Power Shot SX150IS: 0.71mm, Nikon D90: 0.68 mm, Panasonic LUMIX DMC TZ-60: 0.68 mm, SONY Cyber-Shot DSC-TX5: 0.65 mm, Ricoh CapioR7:
Not suitable). The results show that UAV-SfM is a useful method for national park managers and even mountain hikers to obtainhigh-resolution models by using inexpensive cameras to record trail conditions.
Keywords: Structure from Motion, UAV

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HTT08-03

会場:101B

時間:5 月 26 日 09:30-09:45

Tsunami-induced bedrock erosion and sediment deposition on uplifted coastal bench:Cape Todogasaki, eastern Japan
Tsunami-induced bedrock erosion and sediment deposition on uplifted coastal bench:
Cape Todogasaki, eastern Japan早川 裕弌 1∗ ; 小花和 宏之 2 ; Wassmer Patrick3 ; 齋藤 仁 4 ; 小口 高 1
HAYAKAWA, Yuichi S.1∗ ; OBANAWA, Hiroyuki2 ; WASSMER, Patrick3 ; SAITO, Hitoshi4 ; OGUCHI, Takashi1
11Univ. Tokyo, 2 Chiba Univ., 3 Univ. Strasbourg, 4 Kanto Gakuin Univ.
Univ. Tokyo, 2 Chiba Univ., 3 Univ. Strasbourg, 4 Kanto Gakuin Univ.

An uplifted coastal bench at an elevation of ca. 20 m a.s.l. is located around Cape Todogasaki of the ria-type rocky coastin Sanriku, northeastern Japan. Tsunami waves induced by the 2011 Tohoku Earthquake were high enough to spread over the20-m high terrace. To clarify the effects of tsunamis on the terrace surface micromorphology, we performed field measurementsof structure-from-motion multi-view stereo (SfM-MVS) photogrammetry using an unmanned aerial system (UAS), composed ofa digital camera mounted on a small unmanned aerial vehicle (sUAV), and terrestrial laser scanning (TLS). Global navigation
satellite system (GNSS) rover was used to obtain geographical coordinates (centimeter accuracies) of ground control points forthe georeferencing of the UAS and TLS data. Using digital elevation models (DEMs) with a 20-cm resolution generated from thepoint clouds of UAS and TLS, micromorphology of the terrace surface was analyzed. Despite limited basin area draining into theterrace, erosional features in the bedrock were identified. These features appear to be formed by the tsunami flow. Furthermore,
sedimentological characteristics of small thin clasts and large (>2 m) boulders located on the terrace were examined in the field,
revealing that the sediments are likely disloaded from in-situ bedrock at the terrace edge. Evidences of landward flow were also
found from the sediment structure. We conclude that the uplifted terrace surface underwent erosion by not only the 2011 tsunami
but also repeated significant tsunamis in the past, some of which could have been much larger than that in 2011.
キーワード: tsunami, UAS, TLS, erosion, sediments
Keywords: tsunami, UAS, TLS, erosion, sediments

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HTT08-04

会場:101B

時間:5 月 26 日 09:45-10:00

沿岸海底地形学および関係諸科学のための高解像度マルチビーム測深調査
High-resolution multibeam bathymetric survey for coastal seafloor geomorphology andrelated sciences
菅 浩伸 1∗ ; 長尾 正之 2 ; 渡久地 健 3 ; 堀 信行 4 ; 浦田 健作 5 ; 藤田 和彦 3 ; 横山 祐典 6 ; 中島 洋典 7 ;長谷川 均 8 ; 中井 達郎 8 ; 後藤 和久 9 ; 片桐 千亜紀 10 ; 小野 林太郎 11 ; Sinniger Frederic12 ;Prasetia Rian3 ; 波利井 佐紀 3 ; 井口 亮 13 ; 鈴木 淳 2
KAN, Hironobu1∗ ; NAGAO, Masayuki2 ; TOGUCHI, Ken3 ; HORI, Nobuyuki4 ; URATA, Kensaku5 ;FUJITA, Kazuhiko3 ; YOKOYAMA, Yusuke6 ; NAKASHIMA, Yosuke7 ; HASEGAWA, Hitoshi8 ; NAKAI, Tatsuro8 ;GOTO, Kazuhisa9 ; KATAGIRI, Chiaki10 ; ONO, Rintaro11 ; SINNIGER, Frederic12 ; PRASETIA, Rian3 ;HARII, Saki3 ; IGUCHI, Akira13 ; SUZUKI, Atsushi2
1

九州大学地球社会統合科学府, 2 産総研地質情報, 3 琉球大学, 4 奈良大学, 5 大阪経済法科大学, 6 東京大学大気海洋研究所, 7 有明高専, 8 国士舘大学, 9 東北大学災害科学国際研究所, 10 沖縄県立博物館美術館, 11 東海大学, 12 海洋研究開発機
構, 13 沖縄高専
1Graduate School of Integrated Sciences for Global Society, Kyushu University, 2 Institute of Geology and Geoinformation,
AIST, 3 University of the Ryukyus, 4 Nara University, 5 Osaka University of Economics and Law, 6 AORI, University of Tokyo,
7Ariake National College of Technology, 8 Kokushikan University, 9 IRIDeS, Tohoku University, 10 Okinawa Prefectural Museum
and Art Museum, 11 Tokai University, 12 JAMSTEC, 13 Okinawa National College of Technology

The geomorphology of shallow coastal regions has been modulated by repeated subaerial and submarine processes during
glacio-eustatic sea-level change. However, in contrast to the vast knowledge that has been accumulated regarding terrestrial landforms, few previous studies have dealt with shallow seafloor landforms, which represent former terrestrial landscapes modified
by present marine processes, from a geomorphological perspective.
A broadband multibeam echosounder (Sonic 2022, R2 Sonic, LLC) and its accessory system were introduced to H. Kan’slaboratory in 2010 using JSPS Grant-in-Aid for Scientific Research A. We have carried out our bathymetric survey in Kume,Ishigaki, Kikai Islands and the southeastern and northwestern coasts of Okinawa Island in the Ryukyus, southwestern Japan
since 2010.
The Sonic 2022 has a variable ultrasonic frequency of 200 to 400 kHz, 256 ultrasonic beams and selectable swath coverageof 10 to 160 degrees. The typical ultrasonic beam widths parallel and orthogonal to the direction of travel are within one degree of each other when an ultrasonic frequency of 400 kHz is selected. We used a VS111 GPS compass system with A20 andA30 antennas (Hemisphere Inc.) combined with a dynamic motion sensor (DMS-10, Teledyne TSS Ltd.), a sea surface soundvelocity sensor (miniSVS, Valeport Ltd.), a sound velocity profiler (MicroSVP, AML Oceanographic Ltd.). Overlap of at least
˜20% (typically ˜50%) was implemented throughout the bathymetric survey to ensure 100% coverage of the surveyed area. Theminimum and maximum depth was 1m and 400m, respectively. The HYPACK2010 software was used for both hydrographic
survey and data processing. IVS3D Fledermaus was used for three-dimensional visualization.
We conducted geomorphological studies of the coastal seafloor in the coral reef areas of the Ryukyu Islands based on our highresolution bathymetric map with a grid size of 1 m combined with SCUBA diving observations. For example, the submerged
tropical karst features were discovered in Nagura Bay, Ishigaki Island (Kan et al. 2015). This is the first description of submerged
humid tropical karst using multibeam bathymetry. Along with the geomorphological studies, we have also started biological andarcheological studies in our bathymetric areas to promote interdisciplinary researches which link natural and human sciences.
Keywords: multibeam ecosounder, coastal seafloor geomorphology, biology, archaeology, coral reefs, Ryukyu Islands

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