李志清, 孙洋, 胡瑞林, 赵颖, 彭宇. 2018: 基于核磁共振法的页岩纳米孔隙结构特征研究. 工程地质学报, 26(3): 758-766. DOI: 10.13544/j.cnki.jeg.2017-126
    引用本文: 李志清, 孙洋, 胡瑞林, 赵颖, 彭宇. 2018: 基于核磁共振法的页岩纳米孔隙结构特征研究. 工程地质学报, 26(3): 758-766. DOI: 10.13544/j.cnki.jeg.2017-126
    LI Zhiqing, SUN Yang, HU Ruilin, ZHAO Ying, PENG Yu. 2018: QUANTITATIVE ANALYSIS FOR NANOPORE STRUCTURE CHARACTERISTICS OF SHALES USING NMR AND NMR CRYOPOROMETRY. JOURNAL OF ENGINEERING GEOLOGY, 26(3): 758-766. DOI: 10.13544/j.cnki.jeg.2017-126
    Citation: LI Zhiqing, SUN Yang, HU Ruilin, ZHAO Ying, PENG Yu. 2018: QUANTITATIVE ANALYSIS FOR NANOPORE STRUCTURE CHARACTERISTICS OF SHALES USING NMR AND NMR CRYOPOROMETRY. JOURNAL OF ENGINEERING GEOLOGY, 26(3): 758-766. DOI: 10.13544/j.cnki.jeg.2017-126

    基于核磁共振法的页岩纳米孔隙结构特征研究

    QUANTITATIVE ANALYSIS FOR NANOPORE STRUCTURE CHARACTERISTICS OF SHALES USING NMR AND NMR CRYOPOROMETRY

    • 摘要: 选取威远海相页岩(1#)、焦石坝海相页岩(2#)、瑶曲凝灰岩(4#)及瑶曲陆相页岩(5#和6#),采用场发射扫描电镜(FE-SEM)与低场核磁共振(NMR),研究中国海相页岩和陆相页岩之间的孔隙结构特征的差异化特征。核磁共振冻融法(NMRC)可以精细探测页岩的纳米范围的孔隙结构。该方法可以拓展到结合核磁共振弛豫分析进行微观测量,详细探测不同孔径尺度下页岩的孔隙结构。测试温度梯度变化越小,孔隙分布测量的结果越精细。测试结果表明,从样品5#,2#,6#,1#至样品4#的孔隙率逐个减小。NMRC,LFNMR,压汞法(MIP),气体吸附法(GA)在它们各自的有效测量范围内,孔径分布表现出良好的一致性。因此,将NMRC,LFNMR与GA和MIP等方法组合,可以更准确地评估储层页岩的孔隙结构。研究结果表明,陆相页岩(5#瑶曲页岩)的纳米孔隙更发育,与海相页岩相比也许具有更高的商业开发价值。

       

      Abstract: Based on the differences in pore structure characteristics between marine and continental shale in China, Weiyuan marine shale(1#), Jiao Shiba marine shale(2#), Yaoqu tuff(4#) and Yaoqu continental shale(5# and 6#)were selected to study the pore structure characteristics using cold field emission scanning microscopy(FE-SEM) and nuclear magnetic resonance(NMR). Nuclear magnetic resonance cryoporometry(NMRC)was employed to represent nano-scale pore structure. This method can be extended to microns measurement combining nuclear magnetic resonance relaxation analysis to detect in detail the pore structure of shales under the different aperture scales. The smaller the test temperature gradient is, the finer the result of pore distribution is. Test results show decreasing porosity from sample 5#, 2#, 6#, and 1# to sample 4#. NMRC, low field nuclear magnetic resonance(LFNMR), mercury intrusion porosimetry(MIP) and gas adsorption(GA)methods show good agreement of pore size distribution in their respective scope of application. Hence, the pore structure of the reservoir shale can be evaluated more accurately by combining NMRC, LFNMR with GA and MIP. Thus the nano-pores of continental shale(5# Yaoqu shale) are clearly better developed and will more likely have a higher commercial exploitation value than those of marine shale.

       

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