花岗岩粘弹性特性及均匀化分析

Y. Seo, N. Fujii, T. Seiki, Y. Ichikawa
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引用次数: 2

摘要

花岗岩是一种具有晶界和微裂纹等不连续节理的造岩矿物的复合材料。这些微观结构的研究在与地下空间开发有关的地球物理学和岩土工程中日益引起人们的兴趣。首先利用石英、石英/长石和长石三种岩石进行了单轴压缩和松弛试验,以估计不连续节理的物理性质。其次,采用均质化方法分析了含节理花岗岩的粘弹性特性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Viscoelastic Behavior of Granite and the Homogenization Analysis
Granite is a composite material of rock-forming minerals with discontinuous joints such as grain boundaries and microcracks. Studies of these microstructures are of increasing interest in geophysics and geotechnical engineering relating to underground space development. We first performed uniaxial compressive and relaxation tests for estimating physical properties of discontinuous joints by using three kinds of rocks that consist of quartz, quartz/feldspar and feldspar, respectively. Next a homogenization method is applied to analyze a viscoelastic behavior of granite including these joints.
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