茂县是西南深切河谷地区地质灾害的重灾县之一,亦是对区域地质灾害进行特征分析及易发性评价的良好试验基地。在茂县斜坡地质灾害详查及遥感数据解译的基础上,选取高程、地形起伏度、坡形、坡度、地层岩性、水系因子及地质构造7个因素作为评价指标,采用层次分析法对研究区斜坡地质灾害易发性进行评价与区划。结果表明:地质灾害高易发区占地面积约46.1 km2,占10.02%,主要分布于研究区的岷江干流沿岸及其部分支流沿岸等;中易发区面积约149.59 km2,占32.52%;低易发区面积约205.25 km2,占44.62%;非易发区面积约59.06 km2,占12.84%。评价结果与野外调查基本吻合,可为茂县斜坡地质灾害防治及土体规划利用提供依据。
Abstract
Maoxian county is located in the deep valley region of southwest China with severe slope geological hazards, hence is a good experimental base for characteristic research and susceptibility evaluation of geological disasters. In this research, Analytical Hierarchy Process (AHP) was adopted for the evaluation and zoning of geological disaster susceptibility in the study area based on geo-hazard investigation and remote sensing data interpretation. Seven indices inclusive of height, land relieve, slope shape, gradient, lithology, water, and geological structure were selected as evaluation indicators. Result show that the area of high susceptibility covers 46.1 km2, accounting for 10.02% and distributing mainly along mainstream Minjiang River and some tributaries; the area of medium susceptibility covers 149.59 km2, accounting for 32.52%; and area of low susceptibility is 205.25 km2, taking up 44.62%; and the stable area covers 59.06 km2, comprising 12. 84%.The results are consistent with field investigation results in general, and thus could be taken as basis for land use planning and slope geo-hazard prevention and reduction in Maoxian county.
关键词
斜坡地质灾害 /
易发性评价 /
四川茂县 /
地理信息系统 /
层次分析法
Key words
slope geo-hazard /
susceptibility evaluation /
Maoxian county /
GIS /
AHP
{{custom_sec.title}}
{{custom_sec.title}}
{{custom_sec.content}}
参考文献
[1] 柴宗新. 山地灾害概念之我见[J]. 山地学报, 1999, 17(1):91-94.
[2] 孟庆华, 孙炜锋, 王 涛. 陕西凤县地质灾害易发性评价研究[J]. 工程地质学报, 2011, 19(3):388-396.
[3] 王 哲, 易发成. 基于层次分析法的绵阳市地质灾害易发性评价[J]. 自然灾害学报, 2009, 18(1):14-23.
[4] 唐 川, 许 强. 强震区城市地质灾害风险管理的研究内容与方法探讨[J]. 工程地质学报, 2009, 17(1):56-61.
[5] 赵 成, 张永军, 赵玉红. 层次分析法在甘肃省地质灾害易发性评价中的应用[J]. 冰川冻土, 2009, 31(1):186-192.
[6] CASCINI L, BONNARD C. Landslide Hazard and Risk Zoning for Urban Planning and Development[J]. Landslide Risk Management, 2005,(7):199-235.
[7] CARRARA A, GUZZETTI F. Use of GIS Technology in the Prediction and Monitoring of Landslide Hazard[J] . Natural Hazards, 1999,20(2):117-135.
[8] 唐 川, 朱 静. 澜沧江中下游滑坡泥石流分布规律与危险区划[J]. 地理学报, 1999,54(6):84-92.
[9] 金艳珠, 谈树成, 虎雄岗,等. 基于层次分析法与GIS相结合的岩溶塌陷地质灾害易发性分区评估——以云南省师宗县为例[J]. 热带地理, 2012, 32(2):173-178.
[10] 谷天峰, 王家鼎. 地理信息系统在黄土工程地质中的应用[M].北京:地震出版社, 2013.
[11] 铁永波, 唐 川. 层次分析法在单沟泥石流危险度评价中的应用[J]. 中国地质灾害与防治学报, 2006, 17(4):79-84.
基金
中国地质调查局项目(12120113010500)