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Effective porosity for Gassmann fluid substitution

机译:Gassmann流体取代的有效孔隙度

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In this study, we have analyzed the complexity of pore structure and its interaction with pore fluid. The specific surface area is an important parameter related to water retention in reservoir rocks. The surface tension between mineral surface and pore fluids might be so strong that some portion of pore fluids does not respond as fluid under small pressure disturbance. Integrated study of ultrasonic lab measurement data, petrographic data, mercury injection capillary pressure (MICP) data and NMR T_2 data shows the rationality of using an effective porosity as input for Gassmann equation. The effective porosity for Gassmann equation should be frequency-dependent. Knowing the pore geometry, if an empirical correlation between frequency and threshold pore throat size or NMR T_2 is set up, Gassmann equation can be applicable to data of any frequency measurement. Without information of pore geometry, the irreducible water saturation can be used to estimate effective porosity; the "modified" Gassmann equation should give more reliable prediction of saturation effect.
机译:在这项研究中,我们已经分析了孔隙结构的复杂性及其与孔隙液的相互作用。比表面积是与水库岩石中的水保持有关的重要参数。矿物表面和孔隙流体之间的表面张力可能是如此强,即孔隙流体的某些部分不会在小的压力扰动下作为流体响应。超声波实验室测量数据,岩体数据,汞注射毛细管压力(MICP)数据和NMR T_2数据的综合研究显示了使用有效孔隙率作为Gassmann方程输入的合理性。 Gassmann方程的有效孔隙率应依赖于频率。知道孔几何形状,如果建立频率和阈值孔喉部喉部尺寸或NMR T_2之间的经验相关性,则Gassmann等式可以应用于任何频率测量的数据。如果没有孔隙几何形状,则不可挽回的水饱和度可用于估计有效的孔隙率; “修改”Gassmann方程应该提供更可靠的饱和效应预测。

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