基于遥感和GIS技术的北川县地震次生地质灾害分布特征

黄庭; 张志; 谷延群; 周曼蒂; 强建华

doi:10.11834/jrs.20090122

四川汶川地震遥感监测评价专栏 | 浏览量 : 0 下载量: 1366 CSCD: 17 更多指标

PDF
导出
分享
收藏
专辑

基于遥感和GIS技术的北川县地震次生地质灾害分布特征
Distributed characteristics research of earthquake-induced secondary geological disasters in BeiChuan County:Based on GIS and remote sensing
2009年13卷第1期页码：177-182
纸质出版日期： 2009 ，
DOI： 10.11834/jrs.20090122

扫描看全文

[1]黄庭,张志,谷延群,周曼蒂,强建华.基于遥感和GIS技术的北川县地震次生地质灾害分布特征[J].遥感学报,2009,13(01):177-182.

Distributed characteristics research of earthquake-induced secondary geological disasters in BeiChuan County:Based on GIS and remote sensing[J]. Journal of Remote Sensing, 2009,13(1):177-182.
[1]黄庭,张志,谷延群,周曼蒂,强建华.基于遥感和GIS技术的北川县地震次生地质灾害分布特征[J].遥感学报,2009,13(01):177-182. DOI： 10.11834/jrs.20090122.

Distributed characteristics research of earthquake-induced secondary geological disasters in BeiChuan County:Based on GIS and remote sensing[J]. Journal of Remote Sensing, 2009,13(1):177-182. DOI： 10.11834/jrs.20090122.

摘要

以北川县为研究区域

利用多源、多时相卫星数据判读地震次生地质灾害

并在ARCGIS软件的支持下

对地震次生地质灾害的空间分布规律及其影响因素做相关性研究。结果发现

地层岩性、构造、水系、地形地貌等是地震次生地质灾害分布的主要影像因素。不同空间区域上各主要控制因素对次生地质灾害发育的控制力不一样。北川县的地震次生地质灾害沿北川—映秀断裂带密集分布

受岩石地层结构组分的影响

在志留纪地层中集中发育

受地形地貌的影响

在地形坡度30°—70°区域内集中发育。这些分布规律的发现

可以及时为北川县防灾规划和灾后重建提供科学依据。

Abstract

In this paper

we study the spatial distribution rules of earthquake-induced secondary geological disasters and the relationships between the disasters and their impact factors

based on multi-source multi-temporal satellite data

which was support in ARCGIS software platforms.The results show that stratum lithology

geology structure

water system and topography are major controlling factors in disasters;mean while

different regions have different controlling factors

The distribution of BEICHUAN disasters is along the BeiChuan-YingXiu fault zone as banded;a mass of disasters develops in Silurian strata because of structural components;a mass of disasters affected by the topography developed in the terrain with slope of 30°—70°.The distribution regularity of disasters can provide scientific foundation for prevention earthquake plans and reconstruction after earthquake.