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基于SINMAP模型的区域滑坡危险性定量评估及模型验证 被引量:16

A SINMAP-Based Quantitative Assessment and Model Verification of Regional Landslide Hazard
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摘要 利用稳定态水文学理论与无限斜坡稳定性模型,构建分布式斜坡稳定性定量评估模型SINMAP,以坡体滑塌十分发育的陕西省略阳县为试验区,利用Grid DEM提取坡度、流向、地形湿度指数和有效汇水面积等流域地形水文数据,将GIS专题图、遥感数据等作为模型输入数据,获得地表斜坡稳定性分级专题图,实现滑坡危险性定量评估;将模型模拟结果与目前国内最具有权威性的中国县(市)地质灾害调查结果进行对比分析,发现两者在稳定性分级标准划分、滑坡点定性评价、滑坡危险性分区等方面都具有很好的相似性和可比性,说明模型的模拟结果能够客观反映研究区地表滑坡危险性,对可能出现的滑坡具有一定的预测精度。因此,该模型的研究有望为定量分析区域滑坡与环境因子的关系、区域滑坡预测等工作奠定基础。 The regional landslide hazard is evaluated by the factors that affect the stability of the landslope,therefore,the regional landslide hazard evaluation is the landslope stability evaluation.In this paper,Lueyang County,Shaanxi Province is selected as the study area,where the landslide develops typically.By using the quantitative distributed model SINMAP that studies the hillslope stability and 3S(GIS,RS,GPS) technique,the comparison of analogue modeling findings with the most authoritative results of landslide hazard investigation of Chinese cities and counties finds that there are a lot of similarities on the qualitative landslide evaluation,the division of landslide hazard zonation and the criterion of division.It shows that the results of analogue modeling are reliable,and the landslide hazard of the study area are objective,and can give a relative accurate prediction of the potential landslide.Therefore,SINMAP provides a solid foundation for the quantitative analysis of the relationship between study area landslide and the environmental factors and the prediction of the regional landslide.
作者 武利
出处 《地理与地理信息科学》 CSCD 北大核心 2012年第2期35-39,F0003,共6页 Geography and Geo-Information Science
基金 科技部国家重点基础研究发展规划项目(2006CB400502) 中国科学院知识创新工程项目(KZCX1-06) 国家气象局行业专项(GYHY200706001)
关键词 滑坡危险性 斜坡稳定性 SINMAP 稳定性指数 略阳县 landslide hazard slope stability SINMAP surface stability index Lueyang County
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  • 1国土资源部.全国地质灾害通报[EB/OL].http://www.cigem.gov.cn,2011-09-30.
  • 2MONTGOMERY D R,DIETRICH W E.A physically basedmodel for the topographic control on shallow landsliding[J].Water Resources Research,1994,30(4):1153-1171.
  • 3WU W,SIDLE R C.A distributed slope stability model for steepforested watersheds[J].Water Resources Research,1995,31(8):2097-2110.
  • 4PACK R T,TARBOTON D G,GOODWIN C N.The SINMAPapproach to terrain stability mapping[A].MOORE D,HUNGRO.Proceedings of 8th Congress of the International Associationof Engineering Geology[C].Rotterdam,Netherlands:A Balke-ma Publisher,1998.1157-1165.
  • 5BEVEN K J,KIRKBY M J.A physically based variable contribu-ting model of basin hydrology[J].Hydrological Sciences Bulle-tin,1979,24(1):43-69.
  • 6BEVEN K J.Topmodel[A].SINGH V P.Chapter 18in Com-puter Models of Watershed Hydrology[C].Littleton:Water Re-sources Publications,1995.
  • 7O′CALLAGHAN J F,MARK D M.The extraction of drainagenetworks from digital elevation data[J].Computer VisionGraphics and Image Processing,1984,28:328-344.
  • 8TARBOTON D G.A new method for the determination of flow di-rections and contributing areas in grid digital elevation models[J].Water Resources Research,1997,33(2):309-319.
  • 9唐川,JorgGrunert.滑坡灾害评价原理和方法研究[J].地理学报,1998,53(B12):149-157. 被引量:39
  • 10COSBY B J.A statistical exploration of the relationships ofsoil moisture characteristics to the physical properties of ofsoil[J].Water Resources Research,1984,20:682.

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