用自动声学测试系统测量的实验室数据验证了新的岩石物理模型

J. Molnár, M. Dobróka, A. Kiss
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摘要

了解压力与岩石物理参数(如声速、吸收系数、弹性模量、孔隙度)之间的关系对于勘探和开发自然储量至关重要。本文介绍了描述声波纵波速度、横波速度以及质量因子与压力之间关系的岩石物理模型。这些模型的控制方程是基于岩石的孔隙体积随着压力的增加而减小的思想。为了证明模型的适用性,我们在实验室用自动声测试系统对砂岩样品进行了单轴载荷下的纵波和横波速度测试。样品的加载由DION 7软件的自由可编程接口模块完成。速度由GMuG/GL Test Systems PCUSpro软件自动测量。我们采用256倍堆叠来提高信噪比。采用脉冲传输技术测量声速。通过应用程序算法和声学软件,测量已完全自动化。另一方面,文献中发表的质量因子数据集作为压力的函数也被反转。通过联合反演方法对模型参数进行估计后,可以计算任意应力下的速度和质量因子,并推导出与压力相关的弹性模量和损失角。经质量校核的联合反演结果表明,实测值与计算值的拟合误差较小,所建立的岩石物理模型可以很好地应用于实际。
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New petrophysical models verified on laboratory data measured by an automatic acoustic test system
Understanding the relationship between pressure and rock physical parameters, such as acoustic velocities, absorption coefficients, elastic moduli, porosity is essential for exploring and exploiting of natural reserves. In this study petrophysical models are introduced which describe the relationship between acoustic longitudinal (P), transverse (S) wave velocities as well as quality factors and pressure. The governing equations of the models are based on the idea that the pore volume of a rock is decreasing with increasing pressure. To prove the applicability of the models, we measured P and S wave velocities in laboratory on sandstone samples by an automatic acoustic test system under uniaxial load. The loading of the samples were carried out by the Freely Programmable Interface module of the software DION 7. The velocities were measured automatically by the software GMuG/GL Test Systems PCUSpro. We applied 256-fold stacking to increase the signal/noise ratio. Acoustic velocities were measured by using the pulse transmission technique. By applying the programmed algorithm and the acoustic software the measurements have become completely automatic. On the other hand quality factor data set - published in literature - as a function of pressure was inverted too. After estimating the model parameters by joint inversion method, the velocities and quality factors can be calculated at any arbitrary stresses and the pressure dependent elastic moduli as well as loss angles can be derived. The quality checked joint inversion results showed that the misfits between measured and calculated data are small, the suggested petrophysical models can be applied well in practice.
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