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Nano-Pore Structure and Fractal Characteristics of Shale Gas Reservoirs: A Case Study of Longmaxi Formation in Southeastern Chongqing, China

机译:纳米孔隙结构和页岩气藏的分形特征 - 以中国东南部的龙曼氏植物形成为例

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摘要

Pore structure and fractal dimensions can characterize the adsorption, desorption and seepage characteristics of shale gas reservoirs. In this study, pore structure, fractal characteristics and influencing factors were studied of the Longmaxi formation shale gas reservoir in southeasternChongqing, China. Scanning electron microscopy was used to describe the characteristics of various reservoirs. High pressure mercury intrusion and low temperature liquid N2 and CO2 adsorption experiments were used to obtain pore structure parameters. V–Smodel, FHH model and Menger sponge model were selected to calculate the micropore, mesopore and macropore fractal dimensions, respectively. The results show that organic matter pores, inter-granular pores, intra-granular pores and micro-fractures are developed within the shale, and the poremorphology is mostly ink pores and parallel plate pores with aperture essentially in the 1–2 nm and 2–50 nm ranges. Moreover, macropores are the most complex in these samples, with mesopores being less complex than macropores, and the micropores being the simplest. D1(micropore fractal dimension) ranges from 2.31 to 2.50, D2 (mesopore fractal dimension) ranges from 2.74 to 2.83, D3 (macropore fractal dimension) ranges from 2.87 to 2.95, and Dt (comprehensive fractal dimension) ranges from 2.69 to 2.83of fractal characteristics. D1 and D2 are mainly controlled by TOC content, while D3 and Dt are mainly controlled by brittle and clay mineral content. These results may be helpful for exploration and the development ofshale gas in southeastern Chongqing, China.
机译:孔隙结构和分形维数可以表征页岩气储层的吸附、解吸和渗流特征。本文研究了重庆东南部龙马溪组页岩气储层的孔隙结构、分形特征及其影响因素。扫描电子显微镜被用来描述各种储层的特征。采用高压压汞和低温液态N2、CO2吸附实验获得了孔结构参数。选择V-Smodel、FHH模型和Menger海绵模型分别计算微孔、中孔和大孔分形维数。结果表明,页岩内部发育有机质孔隙、粒间孔隙、粒内孔隙和微裂缝,孔隙形态主要为墨孔和平行板孔,孔径基本在1-2nm和2-50nm范围内。此外,在这些样品中,大孔是最复杂的,中孔比大孔复杂,微孔是最简单的。D1(微孔分形维数)范围为2.31至2.50,D2(中孔分形维数)范围为2.74至2.83,D3(大孔分形维数)范围为2.87至2.95,Dt(综合分形维数)范围为2.69至2.83。D1和D2主要受TOC含量控制,D3和Dt主要受脆性和粘土矿物含量控制。这些结果可能有助于重庆东南部页岩气的勘探和开发。

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  • 作者单位

    Key Laboratory of Coalbed Methane Resources and Accumulation Process Ministry of Education China University of Mining and Technology;

    Key Laboratory of Coalbed Methane Resources and Accumulation Process Ministry of Education China University of Mining and Technology;

    Key Laboratory of Coalbed Methane Resources and Accumulation Process Ministry of Education China University of Mining and Technology;

    School of Resources and Earth Geosciences China University of Mining and Technology;

    Key Laboratory of Coalbed Methane Resources and Accumulation Process Ministry of Education China University of Mining and Technology;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 特种结构材料;
  • 关键词

    Southeastern Chongqing; Shale Gas Reservoir; Nano-Pore Structure; Fractal Dimension;

    机译:重庆东南部;页岩气藏;纳米孔结构;分形维数;

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