書誌事項
- タイトル別名
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- TOPOGRAPHY, TOPSOIL STRUCTURE AND PHYSICAL SOIL PROPERTIES ON THE FORESTED HILLSLOPE-THE RESIDUAL SOIL OF GRANITE IN ASUKA VILLAGE, JAPAN-
- シンリン デ オオワレタ シャメン ノ チケイ ドソウ コウゾウ オヨビ ツチ
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抄録
The authers found several presumptive evidence concerning subsurface soil movement and mass movement of topsoil on the forested hillslope, by practices of topographic survey, trench, simplified corn penetration test, physical analysis of soil and X-ray diffraction.The thickness of topsoil increased and then decreased along the slope. It should mean that soil is moving along the slope. At the upper part of topsoil, soil pipes were found. Some of them contribute to soil particle transfer.At the lower half of the upper slope, slip failure was found. And at the middle slope, loose soil was observed. Topsoil is thought to be failing at about 60cm. In depth. Clay content in the soil varied according to the locations on the slope and in the soil profile.Fine material are considered to be moving with subsurface water.
収録刊行物
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- 京都大学防災研究所年報. B
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京都大学防災研究所年報. B 37 (B-1), 127-139, 1994-04-01
京都大学防災研究所
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詳細情報 詳細情報について
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- CRID
- 1050845760512161792
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- NII論文ID
- 120001178838
- 10006385562
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- NII書誌ID
- AN00027784
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- ISSN
- 0386412X
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- HANDLE
- 2433/72517
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- NDL書誌ID
- 3592381
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- 本文言語コード
- ja
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- 資料種別
- departmental bulletin paper
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- データソース種別
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- IRDB
- NDL
- CiNii Articles