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自然科学系 農学部 #紀要論文

地すべり斜面の地下水の2次元的な観測・解析による斜面安定解析

AI解説:
地すべり地の地下水観測において、従来から全長ストレーナ式観測孔が用いられることが多いが、この方法では地下水流が静水圧分布になると仮定しているため、斜面の安定度や地下水排除工による水抜きの効果を正確に評価できない可能性がある。本研究では、深度別に地下水頭を測定し、地下水流を2次元的に捉えることで、2次元浸透流解析を行い、斜面安定解析を従来の方法と比較することを目的としている。
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著者名:
稲葉 一成
掲載誌名:
秋田県立農業短期大学研究報告
巻:
23
ページ:
1 - 23
発行日:
1997-08
著者による要約:
This paper deals with the stability analyses of landslide slopes by the two-dimensional observations and analyses of groundwater pressure. In the landslide slopes having an inclined groundwater flow or having the multi-stratums with the different coefficients of permeability, the groundwater pressure can not be obtained from the static pressure calculated from the groundwater level since the vertical distribution of the groundwater pressure is not static. In this case, the observations and analyses of groundwater pressure should be considered to be a two-dimensional flow systems in a vertical section. And the distribution of pore water pressure along the slip surface used for the stability analyses should be determined from the water pressure using the finite element solution of groundwater flow. In Higashi-mushigame landslide and Matunoyama-koshi landslide, the groundwater pressures were measured by using the observation boreholes having a screened section not along all its length but only at the desired depth. The numerical models having the multi-stratums with the different coefficients of permeability were by trial and error identified by the finite element method so that the numerical results may agree with these field measurements. The stability analyses of landslide slopes using these distributions of pore water pressure along the slip surface provide the reasonable factors of safety.
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