岩石静态变形模量估算及其在不同岩体中的适用性研究进展

IF 0.4 Q4 ENGINEERING, MULTIDISCIPLINARY Engineer-Journal of the Institution of Engineers Sri Lanka Pub Date : 2023-09-25 DOI:10.4038/engineer.v56i3.7608
M. N. C.  Samarawickrama, U. G. A. Puswewala, H. S. Thilakasiri, K. M. L. A. Udamulla
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引用次数: 0

摘要

本研究的目的是回顾在岩石工程应用中估计静态岩体变形模量(𝑚)所采用的不同机制,并探讨所确定的机制在不同岩体中的适用性。本文通过实验、实证等方法对不同的评价标准进行了探讨,分析了其优缺点及影响因素。已知完整岩石的变形模量取决于施加在岩石试样上的应力、应变速率和围应力以及岩石的纹理和结构。不同的原位试验得出的𝑚的结果是不同的,应根据岩体条件进行适当的原位试验,以获得合理的结果。经验准则在特定的岩体条件下,如果采用适当的方法,可以得到合理精度的结果,而反分析方法作为一种原位估计方法,被广泛应用于岩穴和巷道支护的设计中。也有报道称,由于片理性和更大的测试体积,𝑚会出现大幅降低,同时对应力和不连续条件很敏感。本文在文献综述的基础上,对不同类型岩体的𝑚值的估计提出了具体建议。
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Review on the Estimation of Static Deformability Modulus of Rocks and their adoptability in Different Rock Masses
The aim of this study is to review the different mechanisms employed in the estimation of static rock mass deformability modulus (𝐸𝑚) in rock engineering applications and to investigate the adoptability of the identified mechanisms in different rock masses. The paper discusses different evaluation criteria through experimental, empirical and other means, with their merits and demerits, including influential factors. It is known that deformability modulus of intact rock depends on the imposed stress, strain rate and the confining stress on the rock sample as well as the rock texture and structure. The results generated for 𝐸𝑚 by different in-situ tests are different and an appropriate in-situ test based on the rock mass conditions should be employed to obtain reasonable results. Empirical criteria are found to produce results of reasonable precision if appropriately adopted for specific rock mass conditions, while the back analysis method is widely adopted as an insitu estimation measure for the design of rock-sockets and tunnel support. It has also been reported that substantial reduction in 𝐸𝑚 occurs due to schistosity and larger test volumes, while it is sensitive to stress and discontinuity conditions. In this work, specific recommendations are made on the estimation of 𝐸𝑚 for different types of rock masses based on the findings and reviews reported in the literature.
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