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岩石内应力的基本特征及研究进展

陈卫昌 王思敬 傅焕然

工程地质学报2018,Vol.26Issue(1):62-72,11.
工程地质学报2018,Vol.26Issue(1):62-72,11.DOI:10.13544/j.cnki.jeg.2018.01.007

岩石内应力的基本特征及研究进展

STUDY ADVANCE ON BASIC CHARACTERISTICS AND FORMATION CAUSES OF ROCK INNER STRESS

陈卫昌 1王思敬 2傅焕然1

作者信息

  • 1. 中国科学院地质与地球物理研究所 北京 100029
  • 2. 中国科学院大学 北京 100049
  • 折叠

摘要

Abstract

The history and current research status of the internal stress in the residual stress of rock are reviewed and important meanings of research on the internal stress are pointed out in this paper.The basic characteristics of internal stress in rock are analyzed and the formation cause and mechanism are concluded and discussed.Based on analysis,we conclude that the elastic and plastic characteristics and inhomogeneous plastic deformation are necessary condition for locking internal stress of rock,and external loads.Physical and chemical effects and thermodynamic functions are the direct power to store internal stresses.Determining principle and measurement techniques of internal stress in rock are analyzed and summarized respectively.We believe that the plastic deformation is the fundamental cause for releasing of internal stress.Besides,internal stress in rock may affect mechanical behavior,to which attention should be pay.

关键词

岩石内应力/形成机理/释放特征

Key words

Rock inner stress/Formation mechanism/Release characterisitics

分类

天文与地球科学

引用本文复制引用

陈卫昌,王思敬,傅焕然..岩石内应力的基本特征及研究进展[J].工程地质学报,2018,26(1):62-72,11.

基金项目

科技支撑计划课题(2014BAK16B02),地质灾害防治与地质环境保护国家重点实验室开放基金(SKLGP2016K001)资助. (2014BAK16B02)

工程地质学报

OA北大核心CSCDCSTPCD

1004-9665

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