岩石扩容起始特性与峰值特性的比较

侯文诗; 李守定; 李晓; 赫建明; 潘龙; 刘艳辉; 王瑞青

岩石扩容起始特性与峰值特性的比较 English Version

1. 中国科学院地质与地球物理研究所中国科学院工程地质力学重点实验室，北京 100029; 2. 中国科学院大学，北京 100049; 3. 中国地震局地壳应力研究所，北京 100085; 4. 中国地质环境监测院，北京 100081; 5. 中交公路规划设计院有限公司，北京 100088

基金项目: 国家重点基础研究发展规划项目（973）计划项目（2010CB731501）

详细信息

作者简介:
侯文诗(1988- )，女，辽宁沈阳人，硕士，主要从事岩石力学试验方面的研究工作。E-mail: houwens@163.com。

中图分类号: TU452
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出版历程
- 收稿日期: 2012-11-11
- 发布日期: 2013-08-19

Comparison between dilatancy onset and peak of different rocks

1. Key Laboratory of Engineering Geomechanics, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; 2. University of Chinese Academy of Sciences , Beijing 100049, China; 3. The Institute of Crustal Dynamics, CEA, Beijing 100085, China; 4. China Institute for Geo-Environment Monitoring, Beijing 100081, China; 5. CCCC Highway Consultants Co., Ltd., Beijing 100088, China

摘要

摘要: 边坡、隧洞、矿井等岩土工程的失稳过程都伴随着岩体的扩容现象，研究各种工程岩体的扩容特性对工程岩体稳定性评价有重要意义。采用TAW-2000电液伺服岩石三轴试验机，通过对8种岩样的单轴、三轴压缩试验结果分析，获得了低围压下的应力-体积应变曲线，寻求不同岩石的扩容起始点的的变化规律，揭示岩石扩容起始特性与峰值点特性的对应关系。研究结果表明：①岩石扩容起始点处的应力随着围压的增大而增大，并且相比峰值点应力变化，扩容起始点的应力随着围压的变化更强烈；②分别定义了岩石的扩容起始点与峰值点的应力比和应变比计算公式，应力比和轴向应变比呈现很强的线性相关性，并且与其岩性和围压无关。如果确定了峰值点的应力应变关系，便可以较方便地找到岩石的扩容起始点。通过岩石扩容起始点与峰值点变化规律的研究，找到了一条确定岩石扩容起始点的新思路，对岩石的长期强度预测提供了理论依据。
- 岩石扩容 /
- 扩容起始点 /
- 应力应变比 /
- 长期抗压强度
Abstract: The failure process in geo-engineering, such as slope, tunnel and mine, is always accompanied by rock dilatancy. So the studies on the rock dilantancy can really make sense for evaluating the stability of rock mass. TAW-2000 servo-controlled triaxial rock testing system is employed to reveal the rock dilatancy behaviors through uniaxial or triaxial tests on 8 different kinds of rocks. The following conclusions are drawn through the analysis of the test results. The stress of rock dilatancy onset increases with the confining pressure. Compared with that of the peak stress, the variation of stress increment of the rock dilatancy onset is greater. The formula for the stress ratio-axial strain ratio is defined. The relationship between the stress ratio and the axial strain ratio is linear through the origin point regardless of the lithology and the confining pressure. If the stress-strain relationship of the peak is known, the rock dilatancy onset can be found easily. More and more importance should be attached to the studies on the rock dilatancy onset and the peak, that is the key issue for long-term stability estimation of the rock mass.
- rock dilatancy /
- dilatancy onset /
- stress ratio-strain ratio /
- long-term compressive strength

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参考文献(1)

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