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首页> 外文期刊>Fresenius environmental bulletin >STUDY ON THE GEOLOGICAL STRESS SENSITIVITY OF WEAK GEOTECHNICAL ENGINEERING IN THE THREE GORGES RESERVOIR AREA, CHINA
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STUDY ON THE GEOLOGICAL STRESS SENSITIVITY OF WEAK GEOTECHNICAL ENGINEERING IN THE THREE GORGES RESERVOIR AREA, CHINA

机译:中国三峡库区弱岩土工程地质应力敏感性研究

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摘要

Soft rock has the characteristics of poor engineering mechanics, and it is easy to change under the action of water or external load. This paper uses the pulse attenuation permeability meter to develop permeability test and coefficient of variation for weak rock with common engineering mechanical properties. Calculate and explore the geological stress sensitivity characteristics of weak rock engineering within the Three Gorges reservoir area. The conclusions are as follows: the permeability of weak rock in the Three Gorges reservoir area is less than 0.1mD, which belongs to the type of compact soft rock, among which the permeability of medium sandstone (0.048mD) bigger than the permeability of fine sandstone (0.0055mD), fine sandstone bigger than the permeability of mud shale (0.0047mD); the rock permeability coefficient of variation is greater than 0.7, with a strong heterogeneity. The permeability of soft rock has obvious anisotropy. The permeability of the vertical layer of medium-fine sandstone and silty mudstone is greater than the permeability parallel to the plane. The difference between the two is closely related to the physical difference between different lithologies. The permeability of siltstone, shale and sandstone rocks decreases exponentially with the increase of effective stress. The relationship between the permeability loss rates of various types of rock is: shale bigger than siltstone, siltstone bigger than sandstone, indicating the same stress condition, page Rocks have higher stress sensitivity than siltstones and sandstones. This is mainly because the fractures in sandstone and siltstone are more developed than shale.
机译:软岩具有工程力学差的特点,在水或外力作用下很容易发生变化。本文使用脉冲衰减渗透率仪开发了具有常见工程力学特性的弱岩石的渗透率测试和变异系数。计算并探索三峡库区弱岩工程的地质应力敏感性特征。结论为:三峡库区弱岩渗透率小于0.1mD,属于致密软岩类型,其中中砂岩渗透率(0.048mD)大于细砂岩渗透率。砂岩(0.0055mD),比泥页岩渗透率(0.0047mD)大的细砂岩;岩石渗透率变异系数大于0.7,具有很强的非均质性。软岩的渗透率具有明显的各向异性。中细砂岩和粉质泥岩垂直层的渗透率大于平行于平面的渗透率。两者之间的差异与不同岩性之间的物理差异密切相关。粉砂岩,页岩和砂岩的渗透率随有效应力的增加呈指数下降。各种类型岩石的渗透率损失率之间的关系为:页岩大于粉砂岩,粉砂岩大于砂岩,表明应力条件相同,页岩比粉砂岩和砂岩具有更高的应力敏感性。这主要是因为砂岩和粉砂岩的裂缝比页岩更发达。

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