Molecular simulation of methane adsorption within illite minerals in the Longmaxi Formation shale based on a grand canonical Monte Carlo method and the pore size distribution in southeastern Chongqing, China

In order to investigate the pore structure and the adsorption capacity of illite with respect to the methane in the Longmaxi Formation, isothermal adsorption experiments utilizing mercury intrusion, liquid nitrogen, and low-temperature carbon dioxide techniques were applied to the shale samples from...

Full description

Bibliographic Details
Main Authors: Xin Tang, Xiaoyi Zhou, Yujie Peng
Format: Article
Language:English
Published: Elsevier 2019-04-01
Series:Journal of Natural Gas Geoscience
Online Access:http://www.sciencedirect.com/science/article/pii/S2468256X19300136
id doaj-2329f2a75bf8413f823d412649247d83
record_format Article
spelling doaj-2329f2a75bf8413f823d412649247d832020-11-24T21:23:55ZengElsevierJournal of Natural Gas Geoscience2468-256X2019-04-0142111119Molecular simulation of methane adsorption within illite minerals in the Longmaxi Formation shale based on a grand canonical Monte Carlo method and the pore size distribution in southeastern Chongqing, ChinaXin Tang0Xiaoyi Zhou1Yujie Peng2School of Civil Engineering, Chongqing Three Gorges University, Chongqing, 404100, ChinaSchool of Civil Engineering, Chongqing Three Gorges University, Chongqing, 404100, China; Corresponding author.Construction Equipment College, Guizhou Polytechnic of Construction, Guiyang, 551400, ChinaIn order to investigate the pore structure and the adsorption capacity of illite with respect to the methane in the Longmaxi Formation, isothermal adsorption experiments utilizing mercury intrusion, liquid nitrogen, and low-temperature carbon dioxide techniques were applied to the shale samples from southeastern Chongqing. The adsorption characteristics of illite slit pores varying in diameters were simulated using a Monte Carlo method. The results reveal that the pore volume and the specific surface area of the shale are primarily supplied by pore diameters measuring less than 2 nm. Illite is one of the primary components of the clay mineralogy within the shale that forms parallel or nearly-parallel plate pores. For pore sizes ranging from 0.5 nm to 0.9 nm (at conditions of 303.15 K and 8 MPa), the methane molecules are affected by van der Waals and electrostatic forces that leads to a large excess in the adsorption capacity of methane. Once the pore size becomes less than 0.9 nm, the methane adsorption becomes primarily affected by van der Waals forces. At the said size, the excess adsorption capacity of methane initially decreases, after which it remains constant with an increase in the pore size. The free gas content surges with the growing pore diameters. The average equivalent adsorption heat reflects that the adsorption of methane onto illite is characterized by physical adsorption. During the adsorption process, when the pore size is between 0.5 nm and 1.2 nm, the average equivalent adsorption heat decreases rapidly with an increase in the pore diameter. In pore size that exceeds 1.2 nm, the adsorption intensity between the methane molecules and the illite slit becomes stable. In this case, the average adsorption heat is measured to be 6.72 kJ/mol. Meanwhile, the monolayer of methane is adsorbed onto the pore wall and the local density of methane exhibits the characteristics evident of that of a single peak when the pore size is between 0.5 nm and 0.8 nm. The adsorption mode changes from single-layer adsorption to double-layer adsorption when the pore size is between 0.8 nm and 1.2 nm. In addition, the local density curve changes from unimodal to bimodal. In pores sized larger than 1.2 nm, the free volume of methane adsorption can be larger, wherein the local density curve is bimodal. Keywords: Illite, Monte Carlo method, Molecular simulation, Slit pore structurehttp://www.sciencedirect.com/science/article/pii/S2468256X19300136
collection DOAJ
language English
format Article
sources DOAJ
author Xin Tang
Xiaoyi Zhou
Yujie Peng
spellingShingle Xin Tang
Xiaoyi Zhou
Yujie Peng
Molecular simulation of methane adsorption within illite minerals in the Longmaxi Formation shale based on a grand canonical Monte Carlo method and the pore size distribution in southeastern Chongqing, China
Journal of Natural Gas Geoscience
author_facet Xin Tang
Xiaoyi Zhou
Yujie Peng
author_sort Xin Tang
title Molecular simulation of methane adsorption within illite minerals in the Longmaxi Formation shale based on a grand canonical Monte Carlo method and the pore size distribution in southeastern Chongqing, China
title_short Molecular simulation of methane adsorption within illite minerals in the Longmaxi Formation shale based on a grand canonical Monte Carlo method and the pore size distribution in southeastern Chongqing, China
title_full Molecular simulation of methane adsorption within illite minerals in the Longmaxi Formation shale based on a grand canonical Monte Carlo method and the pore size distribution in southeastern Chongqing, China
title_fullStr Molecular simulation of methane adsorption within illite minerals in the Longmaxi Formation shale based on a grand canonical Monte Carlo method and the pore size distribution in southeastern Chongqing, China
title_full_unstemmed Molecular simulation of methane adsorption within illite minerals in the Longmaxi Formation shale based on a grand canonical Monte Carlo method and the pore size distribution in southeastern Chongqing, China
title_sort molecular simulation of methane adsorption within illite minerals in the longmaxi formation shale based on a grand canonical monte carlo method and the pore size distribution in southeastern chongqing, china
publisher Elsevier
series Journal of Natural Gas Geoscience
issn 2468-256X
publishDate 2019-04-01
description In order to investigate the pore structure and the adsorption capacity of illite with respect to the methane in the Longmaxi Formation, isothermal adsorption experiments utilizing mercury intrusion, liquid nitrogen, and low-temperature carbon dioxide techniques were applied to the shale samples from southeastern Chongqing. The adsorption characteristics of illite slit pores varying in diameters were simulated using a Monte Carlo method. The results reveal that the pore volume and the specific surface area of the shale are primarily supplied by pore diameters measuring less than 2 nm. Illite is one of the primary components of the clay mineralogy within the shale that forms parallel or nearly-parallel plate pores. For pore sizes ranging from 0.5 nm to 0.9 nm (at conditions of 303.15 K and 8 MPa), the methane molecules are affected by van der Waals and electrostatic forces that leads to a large excess in the adsorption capacity of methane. Once the pore size becomes less than 0.9 nm, the methane adsorption becomes primarily affected by van der Waals forces. At the said size, the excess adsorption capacity of methane initially decreases, after which it remains constant with an increase in the pore size. The free gas content surges with the growing pore diameters. The average equivalent adsorption heat reflects that the adsorption of methane onto illite is characterized by physical adsorption. During the adsorption process, when the pore size is between 0.5 nm and 1.2 nm, the average equivalent adsorption heat decreases rapidly with an increase in the pore diameter. In pore size that exceeds 1.2 nm, the adsorption intensity between the methane molecules and the illite slit becomes stable. In this case, the average adsorption heat is measured to be 6.72 kJ/mol. Meanwhile, the monolayer of methane is adsorbed onto the pore wall and the local density of methane exhibits the characteristics evident of that of a single peak when the pore size is between 0.5 nm and 0.8 nm. The adsorption mode changes from single-layer adsorption to double-layer adsorption when the pore size is between 0.8 nm and 1.2 nm. In addition, the local density curve changes from unimodal to bimodal. In pores sized larger than 1.2 nm, the free volume of methane adsorption can be larger, wherein the local density curve is bimodal. Keywords: Illite, Monte Carlo method, Molecular simulation, Slit pore structure
url http://www.sciencedirect.com/science/article/pii/S2468256X19300136
work_keys_str_mv AT xintang molecularsimulationofmethaneadsorptionwithinillitemineralsinthelongmaxiformationshalebasedonagrandcanonicalmontecarlomethodandtheporesizedistributioninsoutheasternchongqingchina
AT xiaoyizhou molecularsimulationofmethaneadsorptionwithinillitemineralsinthelongmaxiformationshalebasedonagrandcanonicalmontecarlomethodandtheporesizedistributioninsoutheasternchongqingchina
AT yujiepeng molecularsimulationofmethaneadsorptionwithinillitemineralsinthelongmaxiformationshalebasedonagrandcanonicalmontecarlomethodandtheporesizedistributioninsoutheasternchongqingchina
_version_ 1725990446878949376