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Pore structure characteristics of coal-bearing shale using fluid invasion methods: A case study in the Huainan-Huaibei Coalfield in China

机译:流体侵入法研究含煤页岩孔隙结构特征-以淮南-淮北煤田为例

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Organic shale in coal-bearing strata, which was deposited in marine-continental transitional and lacustrine environments, is well developed in China and contains a large amount of shale gas. However, the present research concerning shale predominantly focuses on marine shale. In this research, the pore structure characteristics of coal-bearing shale in the Huainan-Huaibei Coalfield in southeastern North China Block were analyzed using fluid invasion methods, including helium including helium pycnometry, mercury intrusion porosimetry and N-2 physisorption. The methodology is to determine the porosity using helium pycnometry, the pore size distribution (PSD) of pores between 0.1 mu m and 200 mu m using mercury intrusion, and the PSD of pores between 1 nm and 100 nm using N-2 physisorption. It is worth noting that the accuracy decreases for pores less than 1.5 nm. The specific surface area (SSA) and pore volume (PV) for pores between 1 nm and 200 gm are calculated from interpreted PSD data. In addition, the Brunauer-Emmett-Teller (BET) model was used to calculate the SSA of shale pores. The results indicated that (1) silt-shaped pores are dominant, followed by cylindrical and spherical pores; (2) coal-bearing shale PV is primarily from mesopores (2-50 nm) and macropores (50 nm-5 mu m) and the SSA is mainly from mesopores and micropores (<2 nm); (3) even though the PV percentage of megapores (5-200 mu m) is typically less than 2%, the connection of megapores notably affects the shale permeability, and the pores larger than 80 nm have the largest correlation coefficient with shale permeability; and (4) shale gas adsorption predominantly occurs in micropores and mesopores. By combining mercury intrusion and N-2 physisorption, the PSD, SSA and PV of pores between 1 nm and 200 mu m can be determined for shale, which is critical to understand the shale pore structure and its effects on gas storage and flow mechanisms. (C) 2015 Elsevier Ltd. All rights reserved.
机译:含煤地层中的有机页岩沉积在海洋-陆相过渡和湖相环境中,在中国发育较成熟,并含有大量的页岩气。但是,目前有关页岩的研究主要集中在海相页岩上。本研究利用华北地区东南部淮南-淮北煤田的含煤页岩孔隙结构特征,采用氦比重法,压汞法和N-2物理吸附法等流体入侵方法进行了分析。该方法是使用氦比重瓶法测定孔隙度,使用压汞法测定0.1微米至200微米之间的孔的孔径分布(PSD),以及使用N-2物理吸附法测定1纳米至100纳米之间的孔的PSD。值得注意的是,小于1.5 nm的孔的精度会降低。从解释的PSD数据计算出1 nm至200 gm之间的孔的比表面积(SSA)和孔体积(PV)。另外,使用布鲁瑙尔-埃米特-泰勒(BET)模型来计算页岩孔的SSA。结果表明:(1)粉砂状孔隙占主导地位,其次是圆柱形和球形孔隙; (2)含煤页岩PV主要来自中孔(2-50 nm)和大孔(50 nm-5μm),而SSA主要来自中孔和微孔(<2 nm); (3)即使大孔隙(5-20​​0μm)的PV百分比通常小于2%,大孔隙的连接也会显着影响页岩渗透率,大于80 nm的孔隙与页岩渗透率的相关系数最大; (4)页岩气吸附主要发生在微孔和中孔中。通过结合汞入侵和N-2物理吸附,可以确定页岩在1 nm至200μm之间的孔隙的PSD,SSA和PV,这对于了解页岩孔隙结构及其对储气和流动机理的影响至关重要。 (C)2015 Elsevier Ltd.保留所有权利。

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