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Regional slope stability zonation based on the factor overlapping method

机译:基于因子重叠方法的区域边坡稳定性区划

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Regional slope stability is to study the possibility of slope deformation and instability from theview of regional scale. The paper took the Maerqu watershed from Makehe to Moba County in the upper reachesof Dadu River as the study area. Gradient,fault,slope type,elevation difference,earthquake intensity,lithology,rainfall and land use were chosen as the main factors to affect slope stability. These 8 factors were classified,quantified and scored firstly. Then the original maps of the 8 factors were overlapped by using the factoroverlapping method. Consequently,the regional slope stability of the study area was divided into three types ofregions: the stable region,the middle-stable region and the unstable region. The area of the unstable region is810 km2 which occupies 51.9% of the total study area. It is indicated that the possibility of slope deformationand instability of the study area is high.
机译:区域边坡稳定性是研究区域规模视图坡度变形和不稳定性的可能性。本文将Maerqu流域从大都河上到达的Movehe到Moba County作为研究区。选择梯度,故障,斜坡类型,高度差异,地震强度,岩性,降雨和土地使用作为影响坡度稳定性的主要因素。这8个因素是首先分类,量化和得分。然后,使用因子寄存方法重叠8个因子的原始地图。因此,研究区域的区域边坡稳定性分为三种类型的细节:稳定区域,中稳地和不稳定区域。不稳定地区的区域为810 km2,占总学习区域的51.9%。结果表明,研究区域的坡度变形的可能性高。

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