UAVによる空撮とSfM-MVS解析による地表地震断層の地形モデル作成とその精度

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タイトル別名
  • Evaluation of High-resolution Digital Surface Models of Surface Rupture Associated with the 2014 Kamishiro Fault Earthquake, Central Japan, Using Unmanned Aerial Vehicle Photography and SfM-MVS Analysis
  • UAVによる空撮とSfM-MVS解析による地表地震断層の地形モデル作成とその精度 : 2014年11月長野県北部の地震を例に
  • UAV ニ ヨル クウサツ ト SfM-MVS カイセキ ニ ヨル チヒョウ ジシン ダンソウ ノ チケイ モデル サクセイ ト ソノ セイド : 2014ネン 11ガツ ナガノケン ホクブ ノ ジシン オ レイ ニ
  • —2014年11月長野県北部の地震を例に—

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Surface ruptures associated with the 2014 Kamishiro fault earthquake (Mj 6.7), appeared along the Itoigawa-Shizuoka Tectonic line active fault system in the northern part of Nagano Prefecture, central Japan. We photographed it with digital cameras mounted on an unmanned aerial vehicle (UAV). Digital surface models (DSMs) were generated from the acquired photographs by applying SfM-MVS technology. The UAVs used in this study were the F450 and Phantom 2 manufactured by DJI Inc., and the cameras were the GR model manufactured by RICOH Inc. and were attached to each UAV for aerial photography. The ground control points required for generating DSMs using SfM-MVS analysis were measured using an RTK-GNSS (Leica GPS900), and the topographic profiles used for the accuracy assessment of the DSMs were measured in situ using a total station (Leica TCR705) and digital auto level (SOKKIA SDL50).<BR>As a result, we were able to create DSMs and ortho-photographs at the resolution of a few centimeters. The accuracy was assessed by comparing the topographic profiles measured by the total station and leveling with those generated by the DSMs. Validation against the nine topographic profiles revealed that the DSM had a relative height error of 4.0cm with an average standard deviation.<BR>Taking photographs from a UAV is one of the quickest and most cost-effective methods to record detailed surface topography. Generating a DSM of surface ruptures using UAV photography with SfM-MVS is particularly advantageous because ruptures will change their features quickly, and surface topographic variations of 10 cm or less cannot be recognized in field observations.

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