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Application of low pressure gas adsorption to the characterization of pore size distribution of shales: An example from Southeastern Chongqing area, China

机译:低压气体吸附在页岩孔隙分布特征表征中的应用:以重庆东南地区为例

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Pore size distribution is vital in the preservation and exploitation of shale gas; the pores in shales are mainly of nanometer scale. This study focuses on the pore structures of the Upper Ordovician-Lower Silurian black shales that were sampled from the Well YC7 in southeastern Chongqing area. Nitrogen and carbon dioxide gas adsorption were conducted at 77.4?K and 273.15K, respectively. Pore structures were characterized by the modified BET, BJH, DFT, and Stoeckli methods. The results show that: (1) micropores, mesopores, and macropores are all well developed in both the Lower Silurian and Upper Ordovician shales; (2) the mean diameter of micropores for our samples is approximately 1.26?nm; and (3) the micropore size distribution curves derived from the Stoeckli method together with the CO2 adsorption data at 273.15K can be well connected with the calculated DFT model values through nitrogen adsorption data at 77.4?K, indicating that a full pore size distribution curve could be achieved for micropores, mesopores, and a portion of macropores in the shales by combing the N2 and CO2 adsorption data.
机译:孔径分布对于页岩气的保存和开采至关重要。页岩中的孔隙主要是纳米级的。本研究的重点是从重庆东南地区的YC7井采样的上奥陶纪-下志留统黑色页岩的孔隙结构。氮气和二氧化碳气体的吸附分别在77.4?K和273.15K进行。用改进的BET,BJH,DFT和Stoeckli方法表征孔结构。结果表明:(1)下志留统和上奥陶统页岩中的微孔,中孔和大孔均发育良好; (2)我们样品的平均微孔直径约为1.26?nm; (3)Stoeckli方法得到的微孔尺寸分布曲线与273.15K处的CO2吸附数据可以通过77.4?K处的氮吸附数据与计算出的DFT模型值很好地联系在一起,表明了完整的孔径分布曲线页岩中的微孔,中孔和部分大孔可以通过结合N2和CO2吸附数据来实现。

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