油气藏评价与开发 ›› 2023, Vol. 13 ›› Issue (5): 636-646.doi: 10.13809/j.cnki.cn32-1825/te.2023.05.011

• 页岩气 • 上一篇    下一篇

龙马溪组页岩干酪根表征初探及干酪根吸附特征研究

侯大力1,2,3(),韩鑫2,5,唐洪明1,郭建春4,龚凤鸣2,孙雷4,强贤宇2   

  1. 1.西南石油大学地球科学与技术学院,四川 成都 610500
    2.成都理工大学能源学院,四川 成都 610059
    3.油气藏地质及开发工程国家重点实验室(成都理工大学),四川 成都 610059
    4.油气藏地质及开发工程国家重点实验室(西南石油大学),四川 成都 610500
    5.中国石油长庆油田第四采油厂,陕西 榆林 718599
  • 收稿日期:2022-08-10 发布日期:2023-11-01 出版日期:2023-10-26
  • 作者简介:侯大力(1983—),男,博士,副教授,主要从事油气藏流体相态、注CO2提高采收率及CO2埋存、油气藏数值模拟等方面研究。地址:四川省成都市成华区二仙桥东三路1号,邮政编码:610059。E-mail:houdali08@163.com
  • 基金资助:
    中国博士后基金项目“高温高压下CO2-近临界原油-地层水三相相平衡表征模型”(2017M612995);四川省科技厅应用基础研究项目“储层条件超临界CO2压裂液-页岩气-页岩多相相互作用复杂机理研究”(2021YJ0352);油气藏地质及开发工程国家重点实验室自由探索项目“储层条件超临界CO2-地层水-页岩气-页岩多相相互作用复杂机理研究”(CZ201910)

Primary research on expression of kerogen in Longmaxi Shale and its adsorption characteristics

HOU Dali1,2,3(),HAN Xin2,5,TANG Hongming1,GUO Jianchun4,GONG Fengming2,SUN Lei4,QIANG Xianyu2   

  1. 1. School of Geoscience and Technology, Southwest Petroleum University, Chengdu, Sichuan 610500, China
    2. College of Energy, Chengdu University of Technology, Chengdu, Sichuan 610059, China
    3. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu, Sichuan 610059, China
    4. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum University, Chengdu, Sichuan 610500, China
    5. No.4 Production Plant of Changqing Oilfield, Petrochina, Yulin, Shaanxi 718599, China
  • Received:2022-08-10 Online:2023-11-01 Published:2023-10-26

摘要:

吸附气是页岩气赋存在页岩中的主要方式之一,而且吸附气是页岩气后期产量的主要来源。吸附气主要赋存在页岩有机质干酪根和黏土矿物中,而有机质干酪根中吸附比例较大。因此,研究页岩有机质干酪根的特征及其吸附机理对页岩气开发有重要作用。以四川盆地龙马溪组页岩干酪根为研究对象,通过固体核磁共振谱分析实验、傅里叶变换红外光谱(FTIR)分析实验、X射线光电子能谱(XPS)实验相结合的方法表征干酪根的微观结构,构建了干酪根的分子结构模型。利用磁悬浮重量法实验、巨正则系综蒙特卡洛(GCMC)和分子动力学(MD)的分子模拟方法,分析CH4在龙马溪组页岩干酪根的吸附机理及特征。研究结果表明:龙马溪组页岩实验样品干酪根的分子式为C237H219O21N5S4;CH4在干酪根中的超额吸附量随着压力的增加先升高后降低;相同孔径和压力条件下,随着温度的升高,CH4的超额吸附量和总气量逐渐变小;干酪根中的C原子和S原子是造成CH4吸附的主要原因;靠近干酪根孔壁的CH4呈现吸附态,远离干酪根孔壁的CH4呈现游离态,随着孔径的增加,CH4密度的两峰之间的距离逐渐变宽,峰值逐渐下降。

关键词: 页岩干酪根, 分子结构, 吸附特征, 分子模拟, 龙马溪组

Abstract:

Adsorbed gas represents a primary mode of shale gas occurrence and is a major source of shale gas production in the later stages of development. It primarily resides within the organic kerogen and clay minerals of shale formations, with organic kerogen being the dominant host. Consequently, the study of organic kerogen characteristics and its adsorption mechanisms is crucial for understanding shale gas development. In this paper, the kerogen of Longmaxi Shale in the Sichuan Basin is taken as the research object. The microstructure of kerogen is expressed by combining methods through the solid-state NMR experiment, Fourier transform infrared spectroscopy experiment, X-ray photoelectron spectroscopy experiment, and the molecular structure model of kerogen is constructed. The adsorption mechanism and characteristics of CH4 in kerogen of Longmaxi Shale are analyzed by magnetic levitation weight experiment, molecular simulation methods of the Grand Canonical Monte Carlo(GCMC), and Molecular Dynamics(MD). The results show that the molecular formula of the kerogen of shale experimental sample of Longmaxi Formation is C237H219O21N5S4. The excess adsorption gas volume of CH4 in kerogen increase first and then decreased with the increase of pressure. Under the same pore size and pressure, the excess adsorption gas volume and total gas volume of CH4 decrease with the increase in temperature. The C and S atoms in kerogen are the main cause of CH4 adsorption. The CH4 near the kerogen pore wall presents an adsorption state, while the CH4 far from the kerogen pore wall presents a free state. As the pore size increase, the distance between the two peaks of CH4 density gradually increases, and the peak value decreases gradually.

Key words: shale kerogen, molecular structure, adsorption characteristics, molecular simulation, Longmaxi Formation

中图分类号: 

  • TE377