日本地球惑星科学連合2023年大会

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セッション記号 H (地球人間圏科学) » H-TT 計測技術・研究手法

[H-TT13] 高精細地形表層情報と人新世におけるコネクティビティ

2023年5月24日(水) 10:45 〜 12:00 201A (幕張メッセ国際会議場)

コンビーナ:早川 裕弌(北海道大学地球環境科学研究院)、Gomez Christopher(神戸大学 海事科学部 海域火山リスク科学研究室)、笠井 美青(北海道大学大学院農学研究院)、小倉 拓郎(兵庫教育大学学校教育研究科)、座長:早川 裕弌(北海道大学地球環境科学研究院)、Gomez Christopher(神戸大学 海事科学部 海域火山リスク科学研究室)、小倉 拓郎(兵庫教育大学学校教育研究科)、笠井 美青(北海道大学大学院農学研究院)



10:45 〜 11:00

[HTT13-01] Measurement of microtopographical features using the low-cost mobile laser scanner in Nippara Limestone Cave, eastern Japan

*小倉 拓郎1、坂本 優紀2、安藤 奏音3 (1.兵庫教育大学学校教育研究科、2.東京都立大学都市環境学部、3.中央大学理工学部)

キーワード:低価格モバイルレーザ測量、点群解析、溶食ノッチ、日原鍾乳洞

Understanding the landform development and corrosion process of limestone caves requires the measurement of the microtopography inside them. Qualitative descriptions would traditionally have been based on photographs and sketches. In recent years, photogrammetry and laser scanning have been widely spread and utilized for obtaining high-definition topographic data. Laser scanners are particularly becoming easily available for their lowering price. SLAM technology has enabled automatically combined point clouds, simplifying the creation of 3D topographic maps. Therefore, this study attempted 3D surveying the cave interior using a low-cost laser scanner at Nippara Limestone Cave in Tokyo, eastern Japan. The cave has a total length of 1,270 m and a height difference of 134 m and is open to tourists. The planform of the cave is constrained by faults, which developed with the branch points facing almost directly at right angles to each other. The measurement result showed the cave has various microtopographic features, including speleothems and corrosion notches. The three-dimensional topography of the cave was measured with a low-cost laser scanner, Avia (Livox, Inc.), and a laptop PC with SLAM installed. A total of 24 measurements obtained the overall shape of the cave. Cross-sections can be drawn at any location using CloudCompare, a free point cloud analysis software. The measurement result indicated corrosion notches of the hollow smaller than the ones noted in the previous study (Fig. 1). The processes of lateral erosion caused by groundwater convection and water flow are expected to be clarified by high-precision measurements of corrosion notch depths.