声波速度在静态储层建模中渗透率估计的应用——一个现场实例

S. Prakoso, M. Burhannudinnur, T. Irano, F. Herdiansyah
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引用次数: 0

摘要

几项研究表明,P波速度携带了岩石孔隙几何形状和孔隙结构复杂性的信息。它们的复杂性可以用临界孔隙度来表征。因此,使用P波速度来估计渗透率。本研究使用了中苏拉威西邦盖苏拉盆地Tomori组的数据,该组为碳酸盐岩储层。此外,本研究旨在利用声波速度立方体数据获得三维渗透率模型。结果表明,利用声波速度数据可以很好地模拟渗透率。此外,与渗透率的原始数据日志相比,基于临界孔隙度的波速建模结果显示出良好的结果。如果声波速度立方体数据可用,该方法是渗透率建模的另一种替代方法
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Utilization of Acoustic Wave Velocity for Permeability Estimation in Static Reservoir Modeling: A Field Case
Several researches have shown that P-wave velocity carries information on the complexity of the rock's pore geometry and pore structure. Their complexity can be characterized by critical porosity. Therefore, the P-wave velocity is used to estimate permeability. This research uses data taken from the Tomori formation from Banggai-Sula basin, Central Sulawesi, which is a carbonate rock reservoir. Also, this research aims to obtain a 3D permeability model by using acoustic wave velocity cube data. The results show that permeability can be modeled well using acoustic wave velocity data. Furthermore, compared to the raw data log of permeability, the modeling results using wave velocity based on critical porosity show good results. This method is another alternative to permeability modeling if acoustic wave velocity cube data is available
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