Accurate Carbonate Pore System Characterization by Nuclear Magnetic Resonance and Micro-CT Techniques

Jun Gao, H. Kwak, M. AlSinan
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引用次数: 1

Abstract

Carbonate reservoir rocks usually have complex pore systems of broad size distributions, which determine many aspects of oil exploitation, from petrophysical properties to oil/water displacements. An accurate and complete description of these pore systems remains a challenge. A single technique often gives one measurement of complicated microscopic pore space. The new techniques (i.e., micro-CT and NMR) are utilized together with conventional methods (e.g., MICP, BET) to capture a more accurate and complete picture of pore structures. MICP measures the pore throat while the NMR T2 mainly measures the pore body. Micro-CT provides a 3D image of a limited sample size. Recently, NMR DDIF (decay due to diffusion in the internal field) for direct pore body size is extended from high to low magnetic field, which overcomes many limitations in pore system characterization. This study obtains pore throat size distributions from in-situ centrifuge capillary pressure and pore body size distributions from low field DDIF measurement and verifies them with micro-CT and BET/T2 in different types of carbonate rocks. The pore throat size distribution of the conventional sample is obtained from in-situ centrifuge capillary pressure. The major features of both macro and micro pore throat size distributions are captured. Pore size distributions are directly obtained from glass beads and carbonate rocks without calibration. Combined analysis of the pore size distribution from two methods reveals the underlying causes of their different petrophysical properties. The pore throat size distribution from in-situ centrifuge capillary pressure and pore size distribution from NMR DDIF can be employed to obtain a better understanding of conventional carbonate pore systems.
用核磁共振和微ct技术精确表征碳酸盐孔隙系统
碳酸盐岩储层通常具有尺寸分布广泛的复杂孔隙系统,这决定了石油开采的许多方面,从岩石物性到油水驱替。准确、完整地描述这些孔隙系统仍然是一个挑战。一种技术通常只能对复杂的微观孔隙空间进行一次测量。新技术(如micro-CT和NMR)与传统方法(如MICP, BET)一起使用,以捕获更准确和完整的孔隙结构图像。MICP测量的是孔喉,而NMR T2主要测量的是孔体。Micro-CT提供有限样本量的三维图像。近年来,直接表征孔体大小的核磁共振DDIF(衰减由于扩散在内场)从高磁场扩展到低磁场,克服了孔隙系统表征的许多局限性。本研究通过原位离心毛细压力得到孔喉尺寸分布,通过低场DDIF测量得到孔体尺寸分布,并通过micro-CT和BET/T2对不同类型碳酸盐岩进行验证。常规样品的孔喉尺寸分布是由原位离心毛细管压力得到的。捕获了宏观和微观孔喉尺寸分布的主要特征。孔径分布直接从玻璃珠和碳酸盐岩中获得,无需校准。结合两种方法对孔隙尺寸分布的分析,揭示了形成不同岩石物性的根本原因。利用原位离心毛细管压力测得的孔喉尺寸分布和核磁共振DDIF测得的孔喉尺寸分布可以更好地了解常规碳酸盐孔隙系统。
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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