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岩溶塌陷发育机理模式研究

姜伏伟

中国岩溶2017,Vol.36Issue(6):759-763,5.
中国岩溶2017,Vol.36Issue(6):759-763,5.DOI:10.11932/karst2017y37

岩溶塌陷发育机理模式研究

Study on the developing model of karst collapse

姜伏伟1

作者信息

  • 1. 贵州理工学院,贵州 贵阳550003;中国地质科学院岩溶地质研究所,广西桂林541004
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摘要

Abstract

Karst collapse is a common geological disaster in karst area of China.Currently,the mechanisms of karst collapse development are mainly based on mechanical analysis.In this paper,the mechanisms of karst collapse development is studied based on the developing process of karst collapse.Two conclusions are obtained as follows,(1)According to the aquifer conditions,soils are divided into three types,the unsaturat-ed soil in the aeration zone,the saturated soil in the unconfined aquifer and the pressure-bearing soil in the confined aquifer;(2)On the basis of the interaction between groundwater and soils,three models of karst collapse are established as the disintegration model in the aeration zone,the seepage erosion model in the un-confined aquifer,and the hydraulic fissure model in the confine aquifer.

关键词

岩溶塌陷/崩解作用模式/潜蚀作用模式/水力裂隙作用模式

Key words

karst collapse/the disintegration model/the seepage erosion model/the hydraulic fissure model

分类

天文与地球科学

引用本文复制引用

姜伏伟..岩溶塌陷发育机理模式研究[J].中国岩溶,2017,36(6):759-763,5.

基金项目

贵州省科技厅科技支撑计划社发公关领域项目(黔科合[2016]支撑2846) (黔科合[2016]支撑2846)

贵州省教育厅青年科技人才成长项目(黔教合KY字[2016]226) (黔教合KY字[2016]226)

中国地质调查项目(DD20160254) (DD20160254)

中国岩溶

OA北大核心CSCDCSTPCD

1001-4810

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