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Frontiers of Earth Science

ISSN 2095-0195

ISSN 2095-0209(Online)

CN 11-5982/P

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2018 Impact Factor: 1.205

Front. Earth Sci.    2021, Vol. 15 Issue (2) : 224-236    https://doi.org/10.1007/s11707-021-0910-0
REVIEW ARTICLE
Desorption hysteresis of coalbed methane and its controlling factors: a brief review
Weikai XU1(), Junhui LI1(), Xiang WU2, Du LIU1, Zhuangsen WANG1
1. College of Geoscience and Surveying Engineering, China University of Mining and Technology, Beijing 100083, China
2. China Coalbed Methane Co. Ltd, Beijing 100011, China
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Abstract

Most coal reservoirs show high gas content with relatively low desorption efficiency, which restricts the efficiency of coalbed methane (CBM) extraction and single-well productivity. This review highlights the desorption hysteresis mechanism and its controlling factors as well as methods and models to reveal desorption hysteresis and potential solutions. Methane adsorption and desorption can be recorded by both gravimetric and volumetric experiments. Although different adsorption models are used, desorption is generally considered with the Langmuir model. Desorption hysteresis is influenced by the petrophysical composition, thermal maturity, pore structure distribution of the coal, reservoir temperature, and moisture and water content. Methods for calculating desorption hysteresis include the area index, hysteresis index and introduction of a hysteresis factor and a hysteresis coefficient. Molecular dynamics simulations of methane desorption are mainly based on theories of kinetics, thermodynamics, and potential energy. The interaction forces operating among coal, water, and methane molecules can be calculated from microscopic intermolecular forces (van der Waals forces). The desorption hysteresis mechanism and desorption process still lack quantitative probe methodologies, and future research should focus on coal wettability under the constraints of liquid content, potential energy adjustment mechanism, and quantitative analysis of methane desorption rates. Further research is expected to reveal the desorption kinetics of methane through the use of the solid–liquid–gas three-phase coupling theory associated with the quantitative analysis of methane desorption hysteresis, thereby enhancing the recovery rate and efficiency of CBM wells.

Keywords desorption hysteresis      diffusion process      kinetics      multiphase coupling      coalbed methane production     
Corresponding Author(s): Weikai XU,Junhui LI   
Online First Date: 28 September 2021    Issue Date: 26 October 2021
 Cite this article:   
Weikai XU,Junhui LI,Xiang WU, et al. Desorption hysteresis of coalbed methane and its controlling factors: a brief review[J]. Front. Earth Sci., 2021, 15(2): 224-236.
 URL:  
https://academic.hep.com.cn/fesci/EN/10.1007/s11707-021-0910-0
https://academic.hep.com.cn/fesci/EN/Y2021/V15/I2/224
Fig.1  Schematic diagram of the isothermal adsorption experimental system. (a) High pressure capacity experiment; (b) gravimetric experiment, from Lafortune et al. (2014) and Shi et al. (2019).
Adsorption model Equation Notation Sources
Langmuir V= VLPPL+P V: adsorption quantity;
VL: Langmuir volume constant, cm3/g;
P: gas pressure, MPa;
PL: Langmuir pressure constant, 1/MPa
Langmuir (1917)
DR V=V0e xp [Dln 2( P0/P)] V0: coal micropore volume, cm3/g;
P0: saturated vapor pressure, MPa
Sakurovs et al. (2007)
DA V=V0e xp [Dln n(P0/ P)] n: temperature and coal pore distribution of model parameters Terzyk et al. (2002)
BET V= VmCp (P0P)[1+(C1)(P /P0)] Vm: BET equation of monolayer adsorption capacity, cm3/g;
C: adsorption heat correlation constant
Clarkson et al. (1997)
Curve fitting Quadratic equation:V=b0+ b1P+b2P2;
Cubic equation: V=b0+ b1P+b2P2+b3P3
Logarithmic equation: V=b0+ b1lnP
b0: constant term;
b1: coefficient;
b2: quadratic coefficient;
b3: cubic term coefficient
Ma et al. (2011)
Tab.1  Adsorption mechanism of different adsorption models
Fig.2  Adsorption and desorption isotherms of studied coal samples. Note: ad, adsorption; de, desorption; Vad, adsorbed gas content; Vr,ad, residual gas content; C1, C2, C3, Coal sample number (Referenced from Zhao et al., 2017).
Factors Main conclusions Sources
Temperature Adsorption capacity α (1/temperature)
CH4 isotherm maximum for lowest rank at highest temperature
Temperature affects Langmuir pressure constant P
Nonlinear change in adsorption capacity and temperature
Krooss et al. (2002); Li et al. (2010)
Pressure Adsorption capacity α pressure
Saturation pressure is a key factor
Chattaraj et al. (2016)
Petrographic
composition
Vitrinite-rich groups show stronger adsorption capacity than inert groups
Adsorption capacity α vitrinite content
Vitrinite of higher surface area
Crosdale et al. (1998); Bustin and Clarkson (1998)
Rank Gas sorption increases with the rank
Coal structure changes due to sorption to attain a stable thermodynamic system
Levy et al. (1997); Czerw (1997)
Moisture Water entering coal pores reduces gas diffusivity, porosity, and permeability
Methane adsorption capacity increases nonlinearly with the decrease in moisture content
Gas diffusion rate α (1/moisture)
Busch et al. (2004); Crosdale et al. (2008)
Mineral matter Mineral matter has a negative impact on gas sorption on coal
Pore adsorption capacity increases with the increase of minerals
Adsorption capacity α (1/mineral matter)
Faiz et al. (2007)
Pore structure Desorbed gas gathers in the micropore spaces in the coal matrix
Adsorption-desorption only occurred in small pores and micropores
Followed the Langmuir equation
Clarkson and Bustin (1999b)
Tab.2  Factors influencing coalbed methane desorption
Fig.3  Diagram showing methane adsorption and desorption hysteresis under different influencing factors (Moore, 2012).
Calculation method Equation Notation Sources
Area index HI=100( Ade AadAad) Ade: area under the adsorption isotherm;
Aad: area under the desorption isotherm
Zhu and Selim (2000)
Hysteresis index HI=A deA adAsfA ad× 100% Ade: area under the adsorption isotherm;
Aad: area under the desorption isotherm;
Asf: measure hysteresis area
Wang et al. (2014a)
Introducing hysteresis factor P1=αP;
Q= QmbP11+bP1
α: hysteresis factor;
P: adsorption equilibrium pressure;
P1: desorption equilibrium pressure;
Q: molality of the adsorbed gas during desorption;
Qm: saturation adsorption capacity of single molecule;
b: adsorption constant
Qi et al. (2016)
Hysteresis coefficient Hc= PdcdPacd Pdcd: isothermal desorption curve critical desorption pressure;
Pacd: isothermal adsorption curve critical desorption pressure
Lin et al. (2016)
Tab.3  Calculation method of the hysteresis coefficient of methane desorption
Fig.4  Stress analysis of methane adsorption on the coal matrix under different water content conditions.
Fig.5  Schematic diagram of factors influencing coalbed methane desorption.
Fig.6  Schematic of the hydrodynamic sealing mechanism (Li and Horne, 2007).
Fig.7  Schematic diagram of modeling types for molecular simulation.
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