TOTAL POROSITY AND MATRIX PARAMETERS OF CARBONATE ROCKS BASED ON THE ELASTIC WAVE VELOCITY AND DENSITY MEASUREMENTS

J. Jarzyna, E. Puskarczyk, Ewa Ogórek, J. Motyka
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Abstract

The purpose of the research was to find relationship between elastic waves velocities obtained from lab measurements and parameters from hydrogeological research. Measurements were conducted on 73 rock samples originating mostly from Jurassic limestone of the Olkusz area. Additional information about the rock samples was obtained when the elastic wave velocities were compared with reservoir parameters such as porosity, permeability and density. Plots of elastic waves velocities vs. porosity and bulk density vs. porosity gave information about the range of P wave velocities from the boundary velocity to the values when porosity is equal to zero. Matrix velocity and density values were introduced into the formulas used to calculate porosity. Anisotropy analysis was made on the basis of elastic wave velocities measured on cores cut in two perpendicular directions. This allowed for identification of fractures in rocks. Results showed that by comparing various petrophysical parameters it was possible to get better information about reservoir properties of aquifers.
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基于弹性波速和密度测量的碳酸盐岩总孔隙度和基质参数
研究的目的是找出实验室测量得到的弹性波速与水文地质研究参数之间的关系。对73个岩石样品进行了测量,这些岩石样品大多来自奥尔库什地区的侏罗纪石灰岩。将弹性波速与储层参数(如孔隙度、渗透率和密度)进行比较,可以获得岩石样品的其他信息。弹性波速与孔隙度的关系图和体积密度与孔隙度的关系图给出了纵波速度从边界速度到孔隙度为零的范围的信息。在计算孔隙度的公式中引入了基体速度和密度值。根据岩心在两个垂直方向上所测得的弹性波速进行了各向异性分析。这样就可以识别岩石中的裂缝。结果表明,通过比较各种岩石物性参数,可以更好地了解含水层的储层性质。
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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