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Model construction of micro-pores in shale: A case study of Silurian Longmaxi Formation shale in Dianqianbei area, SW China

机译:页岩中微孔的模型构造-以中国西南千店北志留系龙马溪组页岩为例

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AbstractBased on scanning electron microscopy and nitrogen adsorption experiment at low temperature, the pore types and structures of the Longmaxi Formation shale in the Dianqianbei area, SW China were analyzed, and a molecular model was built. According to mathematical statistics, the validation of the model was solved by converting it into a mathematical formula. It is found by SEM that the pores in clay mineral layers and organic pores occupy most of the pores in shale; the nitrogen adsorption experiment at low temperature reveals that groove pores formed by flaky particles and micro-pores are the main types of pores, and the results of the two are in good agreement. A molecular model was established by illite and graphene molecular structures. Moreover, based on the fractal theory and the Frenkel-Halsey-Hill formula, a modified Frenkel-Halsey-Hill formula was proposed. The reliability of the molecular model was verified to some extent by obtaining parameters such as the fractal dimension, replacement rate and fractal coefficients of correction, and mathematical calculation. This study provides the theoretical basis for quantitative study of shale reservoirs.
机译:摘要基于扫描电子显微镜和低温氮吸附实验,分析了中国西南地区滇黔北地区龙马溪组页岩的孔隙类型和结构,并建立了分子模型。根据数学统计,通过将模型转换为数学公式来解决模型的验证问题。 SEM结果表明,粘土矿物层孔隙和有机孔隙占据了页岩的大部分孔隙;低温氮吸附实验表明,片状颗粒和微孔形成的槽孔是主要的孔类型,两者的结果吻合良好。通过伊利石和石墨烯分子结构建立了分子模型。此外,基于分形理论和Frenkel-Halsey-Hill公式,提出了一种改进的Frenkel-Halsey-Hill公式。通过获得分形维数,置换率和分形校正系数以及数学计算等参数,可以一定程度上验证分子模型的可靠性。该研究为页岩储层定量研究提供理论依据。

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