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Bibliographic Record
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- Material Type
- 文書・図像類
- Author/Editor
- 地頭薗, 隆
- Author Heading
- 地頭薗, 隆 ジトウソノ, タカシ
- Publication, Distribution, etc.
- Text Language Code
- jpn
- Target Audience
- 一般
- Note (General)
- 2011-2013年度科学研究費助成事業（基盤研究（B））研究成果報告書 課題番号：23380086 研究代表者：地蔵薗隆（鹿児島大学・農学部・教授）近年、日本各地で深層崩壊が多発している。九州では様々な地質条件下で深層崩壊が発生している。深層崩壊は、大雨による岩盤地下水位の上昇、深層風化した岩盤、地下水を貯留しやすい水文地形的な地下構造に原因して引き起こされている。地形・地質・水文調査に基づいて深層崩壊発生場の予測法を検討した。本研究では、特に山地系流水を活用した深層崩壊発生場の予測法を開発した。そのために渓流縦断方向の渓流水の電気伝導度を測定し、この電気伝導度の分布図から深層崩壊発生場を予測した。ecently, there have been many deep-seated landslides in Japan. The deep-seated landslides have occurred under various geology conditions in Kyushu. The deep-seated landslides were a resuit of rising groundwater levels caused by heavy rainfall, deeply weathered rocks, and hydrogeomorphological formation of underground areas that are prone to the storage of groundwater. Some methods for site prediction of potential deep-seated landslides were examined based on geomorphic, geological and hydrological surveys. This study aimed to develop a method for predicting the sites of potential deep-seated landslides by using mountain stream water. To this end, I measured the electric conductivity of mountain stream water in the upstream direction. The distribution map of the measured electric conductivity helped to predict the sites of potential deep-seated landslides.
- Format (IMT)
- application/pdf