The Rock Mechanical Properties of Lacustrine Shales from Ordos Basin

Hongyan Yu, Xiaolong Li, Zhenliang Wang, R. Rezaee, L. Gan
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引用次数: 4

Abstract

Abundant shale oil and gas resources have been discovered in the Zhangjiatan shale of the Yanchang formation in ordos basin in recent years. Zhangjiatan shale is a typical lacustrine shale, which is different from Marine shale in physical properties. Most previous research has focused on Marine shale. In order to understand the rock mechanical properties of Zhangjiatan shale, we conducted dynamic and static elastic properties experiments. We selected argillaceous shale and silty laminae shale in Zhangjiatan shale as samples. In order to obtain the static Young's modulus and Poisson's ratio, we use the triaxial pressure test. We use the dipole log to measure the acoustic velocity down the hole, and then we calculate the dynamic Young's modulus and Poisson's ratio of the sample based on acoustic velocity. Young's modulus of argillaceous shale is slightly smaller than that of silty laminae shale and the Poisson's ratio of argillaceous shale is also smaller than that of silty laminae shale. The brittleness of argillaceous shale are greater than that of silty laminae shale, as a result, argillaceous shale is much easier fracturing under pressure. We plotted the cross-plot of RCS, elastic properties and TOC and reached a conclusion that the mass ratio of clay to quartz and feldspar determined the brittleness and deformability of rock, while organic matters also affected the elastic properties of rock. Therefore, the elastic properties of shale are not controlled by a single factor, instead of multiple factors.
鄂尔多斯盆地湖相页岩岩石力学性质研究
近年来在鄂尔多斯盆地延长组张家滩页岩中发现了丰富的页岩油气资源。张家滩页岩是典型的湖相页岩,其物性与海相页岩不同。以前的大多数研究都集中在海相页岩上。为了解张家滩页岩岩石力学特性,开展了动、静态弹性特性实验。选取张家滩页岩中的泥质页岩和粉砂质纹层页岩作为样品。为了得到静杨氏模量和泊松比,我们采用了三轴压力试验。利用偶极子测井测量了井下的声速,并基于声速计算了样品的动态杨氏模量和泊松比。泥质页岩的杨氏模量略小于粉质纹层页岩,泥质页岩的泊松比也小于粉质纹层页岩。泥质页岩脆性大于粉砂质纹层页岩,在压力作用下更易破裂。我们绘制了RCS、弹性性质和TOC的交叉图,得出粘土与石英和长石的质量比决定了岩石的脆性和可变形性,有机质也影响岩石的弹性性质。因此,页岩的弹性性质不是由单一因素控制,而是由多种因素控制。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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