大气降水对崩滑流地质灾害的影响  

Influence of Atmospheric Precipitation on Slump Flow Geologic Hazards

作　　者：陈冲 王洪永 Chen Chong;Wang Hongyong(Geo-information Engineering Team of Jiangxi Geology Bureau,Nanchang,Jiangxi 330001;Geological Environment Monitoring Institute of Jiangxi Geological Survey and Exploration Institute,Nanchang,Jiangxi 330001)

机构地区：[1]江西省地质局地理信息工程大队,江西南昌330001 [2]江西省地质调查勘查院地质环境监测所,江西南昌330001

出　　处：《江西煤炭科技》2023年第3期115-117,124,共4页Jiangxi Coal Science & Technology

摘　　要：崩滑流地质灾害的发生是地形地貌、地质构造、岩土体结构类型、大气降水、地震、人类工程活动等诸多因素共同作用的结果,其中大气降水是崩滑流地质灾害的主要诱发因素。文章从上高县年降雨量、月均降水量、降水集中区、降雨强度等方面,探讨大气降水对崩滑流地质灾害的影响。The occurrence of slump flow geologic hazards is the result of the combined action of many factors such as topography,geological structure,rock and soil structure type,atmospheric precipitation,earthquakes,and human engineering activities,among which atmospheric precipitation is the main inducing factor.The paper discusses the influence of atmospheric precipitation on the slump flow geologic hazards from the aspects of annual rainfall,monthly average rainfall,rainfall concentration area,rainfall intensity,etc.in Shanggao County.

关 键 词：崩滑流地质灾害 大气降水 年降雨量 降雨强度 

分 类 号：P642.2[天文地球—工程地质学]