为对大范围区域斜坡的稳定性进行有效、定量的评价,提出一个耦合二维力学分析模型的区域斜坡稳定性评价方法。选择宝鸡市金台区的一段黄土沟谷作为研究区,对文章提出的方法进行验证。首先,利用GIS实现斜坡单元的划分;然后,利用钻探及调查得到的地层数据形成区域的多层Grid模型;在此基础上,开发程序,完成计算剖面生成、滑面搜索、稳定性评价等工作;最后,根据各单元的稳定性系数,生成区域斜坡稳定性分区图。这种方法以二维极限平衡方法为基础,即可得到研究区域的二维安全系数分布图,又可求得最危险滑动面的位置和规模。
Landslide is one of the most damaging natural hazards in China, thus landslide susceptibility map- ping plays an important role in disaster prevention. Probability-based analysis is the most popular method to evaluate a wide range of natural slope instability risk. But the applications of it are limiting factor for lack of landslides data. In order to evaluate a wide range of natural slope instability risk effectively and quantitatively, this article presents a new method which evaluate regional slope instability risk, combining with two-dimen- sional mechanical analysis model and Geographic Information System (GIS) method. Firstly, a region is divid- ed into a group of slope zones according to the terrain condition by using watershed hydrology analysis meth- od in GIS. The location of main section line of each slope zone is set according to its average slope inclination and angle. A series of possible sliding surfaces are formed and the minimum safety factor of every slope zone is calculated based on two-dimensional mechanical analysis model. On the basis of calculation results, slope risk zoning map is drawn. A loess gully region in Jintai District of Baoji City, Shaanxi Province, China, is se- lected as the study area. The proposed method is verified. First of all, the topographic map is changed into a digital elevation model, with the planar range is 3 kmx4 km and grid size is 10 m. According to the process mentioned above, the area is divided into 76 zones using hydrology tools. Secondly, the grid layers of strata in- terfaces are interpolated with the data of stratums, which is obtained from drilling and investigation. And then, geologic model of this area is set up using multi grid layers method. Thirdly, a regional stability evaluation pro- gram is developed according to the stability factor of each unit. It can read files in GIS formats, extract sec- tions automatically, access stability, and convert the results into GIS data. Finally, with this program, calcula- tion profile of every zone is generat