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A new correction method for mercury injection capillary pressure (MICP) to characterize the pore structure of shale

机译:一种新的汞注入毛细管压力(MICP)的校正方法,以表征页岩孔隙结构

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The economic and accurate measurement of micron or submicron size pores in shale is still a challenge. The mercury injection capillary pressure (MICP) measurement of shale particles is an effective method to evaluate the macropore structure, but it is questionable without proper data interpretation. In this study, the fractal theory was applied to identify the four stages of MICP measurement Stage A is controlled by the interparticle voids in the particle assemblage; Stage B can reflect mercury intrusion into the pores of the shale; and Stage C and D indicate the shale matrix compression and pore structure change induced by high pressure, respectively. Based on the consistent fractal dimension derived from Stage A, the conformance volume induced by interparticle voids at each pressure step in Stage B was quantitatively simulated using the linear fitting method. The correction results show that simultaneous mercury filling of interparticle voids has an important impact on the pore volume in the pore size range larger than 1 mu m. To cover the complete pore size range, the MICP data in Stage C and D were substituted by gas adsorption data.
机译:页岩中微米或亚微米尺寸毛孔的经济和准确测量仍然是一项挑战。页岩颗粒的汞注射毛细管压力(MICP)测量是评估大孔结构的有效方法,但没有适当的数据解释,它是可疑的。在该研究中,分形理论被应用于鉴定MICP测量阶段A的四个阶段由颗粒组件中的颗粒间隙控制; B阶段可以将汞侵入物体反映到页岩的毛孔中;阶段C和D分别表示高压诱导的页岩基质压缩和孔结构变化。基于阶段A的一致分形尺寸,使用线性配合方法定量模拟B阶段B中的每个压力步骤中的颗粒间隙诱导的一致体积。校正结果表明,颗粒间隙的同时汞填充对大于1μm的孔径范围内的孔体积具有重要影响。为了覆盖完整的孔径范围,阶段C和D中的MICP数据被气体吸附数据取代。

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