基于多频介电测量的孤立孔隙度油藏表征

G. Jin, S. Ma, R. Antle, S. Al-Ofi
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引用次数: 1

摘要

由于地质成岩作用的作用,岩石中的孔隙可以与其他连通的孔隙网络隔离开来。孤立孔隙的数量和空间分布直接影响储层的物性和性能。本文介绍了一种利用多频(频散)介电测量定量非均质储层孤立孔隙度的新方法。在数值模拟研究的基础上,利用数字岩石物理技术生成了具有不同孤立孔隙度的岩石模型。然后对模型进行三维介电色散建模,得到岩石介电常数的色散。由于孤立孔隙率的增加,孔隙连通性发生变化,介质色散表现不同。当孔隙孤立时,介电常数对频率敏感,而当孔隙连通时,介电常数对频率不敏感。介电常数的变化与孤立孔隙的数量密切相关。对于总孔隙度相同的岩石,其介电常数随着孤立孔隙度的增加而增加。这种介电常数的增强是由于孔隙网络扭曲度的增加,导致固体和孔隙之间界面上电荷的积累增加。建立了分析关系,将孤立孔隙度与介电常数变化率和/或介电常数比(由介电常数的色散导出)联系起来。预测的孤立孔隙度与建立岩石模型所用的真实值一致,证明了所建立方法的有效性和适用性。该方法可用于现代多频介电测井来增强储层特征。
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Reservoir Characterization for Isolated Porosity from Multi-Frequency Dielectric Measurements
Due to processes of geological diagenesis, pores in rocks can be isolated from the rest of the connected pore networks. The amount and spatial distribution of isolated pores can have direct effect on petrophysical properties and performance of the reservoir. This paper introduces a new methodology to quantify the isolated porosity of heterogeneous reservoirs from multi-frequency (dispersion) dielectric measurements. Based on numerical simulation studies, digital rock physics techniques are used to generate rock models with different isolated porosities. 3D dielectric dispersion modeling is then performed on the models to obtain the dispersion of rock’s dielectric constant. Dielectric dispersion behaves differently as the pore connectivity changes due to increase in isolated porosity. Dielectric constant is sensitive to frequency when pores are isolated, while insensitive to frequency when pores are connected. Variation of dielectric constant is strongly related to the amount of isolated pores. For rocks having the same total porosity, their dielectric constant increases as the isolated porosity increases. This enhancement of dielectric constant is attributed to the increase in pore network tortuosity, resulting in increased accumulations of electric charges at the interfaces between solid and pores. Analytical relationships are developed to correlate isolated porosity with the rate of permittivity change and/or the permittivity ratio, derived from the dispersion of dielectric constants. The validity and applicability of the established method are demonstrated by the agreement of predicted isolated porosity with the true values used in building the rock models. Potentially, this method can be used for enhancing reservoir characterization with modern multifrequency dielectric logs.
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