2019
DOI: 10.1016/j.jiec.2019.06.015
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New perspectives on supercritical methane adsorption in shales and associated thermodynamics

Abstract:  Adsorption isotherms under different pressures and temperatures can be represented by a 2D surface. Adsorbed methane density in shales is a function of pressure and temperature. Maximum adsorption uptake of shales is independent of temperature and pressure. Isosteric enthalpy and entropy depend on surface coverage and temperature.

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Cited by 38 publications
(57 citation statements)
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“…Ad-/desorption behaviors of methane molecules in shale pores are controlled by many factors. Many experimental results have confirmed that the total organic carbon (TOC) in shale is positively correlated with an amount of methane adsorption. The type of organic matter also affects the methane adsorption behavior. The Langmuir pressure is the highest for type I organic matter, followed by type II, and finally the lowest for type III .…”
Section: Introductionmentioning
confidence: 99%
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“…Ad-/desorption behaviors of methane molecules in shale pores are controlled by many factors. Many experimental results have confirmed that the total organic carbon (TOC) in shale is positively correlated with an amount of methane adsorption. The type of organic matter also affects the methane adsorption behavior. The Langmuir pressure is the highest for type I organic matter, followed by type II, and finally the lowest for type III .…”
Section: Introductionmentioning
confidence: 99%
“…Increasing illite content also typically results in less methane adsorption with shale . Yet, the maximum absolute adsorption amount of methane in shale is independent of temperature and pressure, although increased temperatures and pressures lead to a decrease in the adsorption rate …”
Section: Introductionmentioning
confidence: 99%
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“…The shale in Yichang is a fine-grained sedimentary rock, generally characterized by large specific surface area and high porosity. Most previous studies are conducted with a focus on methane adsorption behavior on shale matrix [11]. To the best of our knowledge, there is no data available in literature about the removal of pyridines by shale.…”
Section: Introductionmentioning
confidence: 99%
“…According to relevant research, shale gas reserves in 41 countries or regions in the world have been estimated at approximately 35,782 trillion cubic feet available for exploitation. 3 The main component of shale gas is CH 4 , which is usually stored in underground shale in three different states: free state, adsorbed state, and dissolved state, 4 where the amount of adsorbed gas accounts for up to 85% of the total shale gas reservoir. 5 At a depth of 1500−2500 m underground in Longmaxi Formation shale gas field in China, it was found that the reservoir temperature was approximately 330−360 K, and the gas pressure could well reach 38 MPa.…”
Section: Introductionmentioning
confidence: 99%