尼泊尔中部达曼园艺农场浅层土坡失稳分析

S. Manandhar
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引用次数: 2

摘要

对尼泊尔中部马哈巴拉特地区达曼园艺农场周围的斜坡进行了边坡稳定性分析。达曼位于摩诃婆罗带,基底岩为侵入花岗岩。这些花岗岩高度风化到完全,从暴露的表面分解到几米深。园艺农场坐落在这些腐烂的岩石上,山坡上有一些堆积。1993年7月19日至21日的暴雨摧毁了园艺农场,造成许多山体滑坡和沟壑侵蚀。基于极限平衡分析理论和计算指标,结合土体的强度特性,对3个失稳边坡进行了分析。分析表明,滑梯只有在完全饱和的条件下才不稳定。doi: 10.3126/ bg .v10i0.1422尼泊尔加德满都特里布万大学地质系通报,2007年第10卷,第71-78页
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Shallow soil slope instability analysis at horticultural farm, Daman, Central Nepal
Slope stability analyses were carried out for slopes around the horticultural farm at Daman, Central Mahabharat Region of Nepal. Daman lies in the Mahabharat zone with intruded granite as the basement rock. These granites are highly to completely weathered and decomposed to few metres depth from the exposed surfaces. The horticultural farm is situated over these decomposed rocks with some colluvium along the hill slopes. The rainstorm of 19-21 July 1993 devasted the horticultural farm with numerous landslides and gully erosions. Based on the limit equilibrium analysis theory and computed index as well as strength properties of the soil, analyses of three of the failed slopes were carried out. The analyses revealed that slides were unstable only during fully saturated conditions. doi: 10.3126/bdg.v10i0.1422 Bulletin of the Department of Geology, Tribhuvan University, Kathmandu, Nepal, Vol. 10, 2007, pp. 71-78
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