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初论环境地质中裂隙岩体渗流 -应力-温度耦合作用研究

杨立中 黄涛

水文地质工程地质2000,Vol.27Issue(2):33-35,3.
水文地质工程地质2000,Vol.27Issue(2):33-35,3.

初论环境地质中裂隙岩体渗流 -应力-温度耦合作用研究

The primary study of coupling among seepage-stress-temperature  in fractured rock mass in environmental geology

杨立中 1黄涛1

作者信息

  • 1. 西南交通大学,四川成都 610031
  • 折叠

摘要

Abstract

Fractured rock mass is located in a complex geological environment where groundwater seepage field, stress field and temperature field exist simultaneously. With mutual action among the above fields, the estimation accuracy of deep-buried groundwater resource would be affected on one hand; and on the other hand, the geological hazards such as rock mass' stability loss, rock burst, water gushing and geothermal calamity would be induced in practice. In order to predict the deep-buried groundwater resource and prevent the above disasters in engineering, this article presents a research format about the coupling among seepage, stress and temperature in fractured rock mass, which has developed a new study method for hazards' precaution and rational utilization of groundwater resource in environmental geology.

关键词

裂隙岩体/渗流/应力/温度/耦合作用

Key words

fractured rock mass/seepage/stress/temperature/coupling

分类

天文与地球科学

引用本文复制引用

杨立中,黄涛..初论环境地质中裂隙岩体渗流 -应力-温度耦合作用研究[J].水文地质工程地质,2000,27(2):33-35,3.

基金项目

国家自然科学基金资助项目(49872082) (49872082)

水文地质工程地质

OACSCD

1000-3665

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