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岩体应力的现场研究
引用本文:李光煜,白世伟.岩体应力的现场研究[J].岩土力学,1979,1(1):76-90.
作者姓名:李光煜  白世伟
作者单位:中国科学院武汉岩体土力学研究所
摘    要:岩体力学不同于力学的其他分支的主要特点之一,是岩体具有内应力.因而,一切与岩体有关的力学问题的合理解决,脆性破裂理论的实际应用,都离不开对岩体应力状态的了解.

关 键 词:岩体应力    现场研究    主应力方向    脆性破裂    弹模    应力调整    最大主应力    力学模型    三维应力    结构面  

In Situ Study on Stress in Rock Mass
li Guang-yu,Bai Shi-wei.In Situ Study on Stress in Rock Mass[J].Rock and Soil Mechanics,1979,1(1):76-90.
Authors:li Guang-yu  Bai Shi-wei
Institution:Institute of Rock and Soil Mechanics, Academia Sinica W uhan, China
Abstract:The Significance of the rock stress measurements for studying state of stress in the crust is elucidated in this paper .A brief introduction on the principles and methods of calculating the rock stress by measuring the deformations of the bore-holes by means of the overcoring technique is given .Generally the error is estimated to be about 10% by the laboratory checking methods .Form the practical examples it is summed up for some laws of the stress distribution within 200 meters of the shallow crust: from the viewpoint of the rock-mass strength and energy accumulation, the relationship between the major principal stress and the elastic modules of the rock is shown in diagrams, and its direction is closed related to the topographical conditions .The practical examples reveal the measurement of rock stress is significant to the ground surface and underground engineering projects .
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