软质沉积岩动、静态杨氏模量的岩石物理建模

Toru Takahashi, Soichi Tanaka
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引用次数: 0

摘要

为了解释软质沉积岩的动态和静态杨氏模量,将Dvorkin-Gutierrez粉质页岩模型和颗粒模型中的一种应用于动态模量的测速数据和静态模量的实验室力学试验数据的实测杨氏模量。岩石的杨氏模量由Hashin-Strikman下界、Hertz-Mindlin接触模型和Gassmann方程计算。对于静态杨氏模量的建模,在Hertz-Mindlin接触模型中,通过将摩擦和无摩擦颗粒接触的混合物纳入模型来计算剪切模量。计算得到的动态和静态杨氏模量与日本三种不同软质沉积岩的实测数据吻合较好。这一结果表明,岩石物理模型可以用地震速度得到的动态模量来预测土木工程应用所需的静态模量。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Rock Physics Modeling of Dynamic and Static Young's Moduli of Soft Sedimentary Rocks
To interpret dynamic and static Young's moduli of soft sedimentary rocks, the Dvorkin-Gutierrez silty shale model, one of granular models is applied to the measured Young's moduli obtained from velocity logging data for the dynamic modulus and from laboratory mechanical test data for the static modulus. The Young's modulus for the rock is calculated by the Hashin-Strikman lower bound, Hertz-Mindlin contact model and Gassmann's equation. For modeling static Young's modulus, in the Hertz-Mindlin contact model, the shear modulus is calculated by incorporating the mixture of frictional and frictionless grain contacts into the model. The calculated dynamic and static Young's moduli are well consistent with the measured data for three different soft sedimentary rocks in Japan. This result demonstrates that the rock physics model can be used to predict the static moduli required in civil engineering applications from dynamic ones obtained from seismic velocities.
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