Density Analysis of Adsorption Phase in the Thermodynamic Study of Shale Gas Adsorption

• Published in: Langmuir Vol. 40; no. 16; pp. 8593 - 8607
• Main Authors: Zhou, Yu, Xie, Yonggang, Wang, Jiale, Zhou, Changjing, Shi, Huaqiang, Li, Xiaoping, Jing, Dengwei
• Format: Journal Article
• Language: English
• Published: United States American Chemical Society 23.04.2024
• ISSN: 0743-7463; 1520-5827
• DOI: 10.1021/acs.langmuir.4c00293

Understanding the adsorption mechanism and precisely predicting the thermodynamic adsorption properties of methane at high pressure are crucial while very challenging for shale gas development. In this study, we demonstrated that the Langmuir adsorption model combining with different empirical methods to determine the adsorption phase density makes the calculated isothermal adsorption heat violate Henry’s law at low pressure. For instance, the isothermal adsorption heat calculated by the Langmuir–Freundlich model contradicts Henry’s law when the absolute adsorption quantity is zero. Given the current challenge in accurately calculating the adsorption phase density, it is necessary to impose constraints on the parameters of the adsorption model by adhering to Henry’s law to maintain thermodynamic consistency. We found that the adsorption phase volume of methane molecules lies between the micropore volume and the total pore volume when shale adsorption reaches saturation. The adsorption mechanism involves not only filling micropores but also monolayer adsorption in meso-macro pores. The high-energy adsorption sites for methane are primarily concentrated in organic matter, while within these methane adsorption areas in shale, the high-energy adsorption sites for water are mainly located in kaolinite within clay minerals. The zero-pressure heat of adsorption is a temperature-independent thermodynamic index, yet it is influenced by the water content. It can therefore be selected as a quantitative measure to evaluate the impact of methane adsorption on water.