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A comprehensive analysis on the relationships between elastic wave velocities and petrophysical properties of sedimentary rocks based on laboratory measurements

机译:基于实验室测量的弹性波速度与沉积岩岩石物性关系的综合分析

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This paper is an attempt to find the interdependence existing between petrophysical properties and ultrasonic wave velocities. Porosity and permeability, apart from other properties, are the two fundamental physical properties of rock responsible for storing and producing hydrocarbon. Understanding the elastic properties of such rocks is essential in developing a deep understanding about the rock and fluid models that describe the seismic response to realistic hydrocarbon reservoirs under different environmental conditions. Therefore, in this study, a detailed state-of-the-art review of the existing association between compressional and shear wave (also known as P wave and S wave) velocities (Vp and Vs) and different petrophysical properties (porosity, density, permeability, water absorption and clay content) has been summarized for carbonate and sandstone rock types of different regions. The relationships discussed are based on datasets measured in laboratory by various researchers under ambient conditions. An effort is made to propose a general trend (global trends) for porosity versus Vp and bulk density versus Vp, which is independent of the type of datasets. However, it is clear that trends do exist, but the prediction is difficult. The empirical relationships derived by various researchers are valid only to the particular dataset for which the relationship was derived. The influence of other factors like mineralogy, rock framework, pore geometry has not been studied by the researchers in their respective studies. Nevertheless, these relationships and correlations can be useful in hydrocarbon exploration industry where direct measurements may not be possible. Moreover, an accurate reservoir description can only be achieved by the integration of geological, petrophysical and geotechnical data.
机译:本文试图找到岩石物理性质与超声波速度之间的相互依存关系。除了其他特性外,孔隙率和渗透率是负责储存和生产碳氢化合物的岩石的两个基本物理特性。了解这种岩石的弹性特性对于深入理解岩石和流体模型至关重要,这些模型描述了在不同环境条件下对真实油气藏的地震反应。因此,在这项研究中,对压缩波和剪切波(也称为P波和S波)速度(Vp和Vs)与不同岩石物理特性(孔隙度,密度,总结了不同地区碳酸盐和砂岩类型的渗透率,吸水率和黏土含量)。所讨论的关系基于各种研究人员在环境条件下在实验室中测得的数据集。努力提出孔隙率与Vp和体积密度与Vp的总体趋势(整体趋势),而与数据集的类型无关。但是,很明显趋势确实存在,但是预测很困难。各种研究人员得出的经验关系仅对得出该关系的特定数据集有效。研究人员尚未在各自的研究中研究其他因素(如矿物学,岩石骨架,孔隙几何形状)的影响。然而,这些关系和相关性在无法进行直接测量的油气勘探行业中可能很有用。而且,只有通过整合地质,岩石物理和岩土数据才能获得准确的储层描述。

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