{"title":"CO2, CH4, and N2 Desorption Characteristics in a Low-Rank Coal Reservoir","authors":"Zhaoying Chen, Junqiang Kang, Xuehai Fu, Mingjie Liu, Qingling Tian, Jiahao Wu","doi":"10.1007/s11053-024-10357-x","DOIUrl":null,"url":null,"abstract":"<p>With increasing emphasis on low-carbon environmental protection, CO<sub>2</sub> enhanced coalbed methane production and methane reuse in abandoned mines (rich in N<sub>2</sub>) have gradually become one of the future development directions. These scenarios involve the coordinated migration of different gases such as CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>, and the differences in properties of different gases that affect the flow process. Previous studies often focused on the adsorption differences between gases, neglecting the differences during desorption process. In view of this, the current work conducted experiments and finite element numerical analysis on the desorption process of CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub>, clarified the differences and influencing factors of desorption among the gases, and analyzed the flow change rules under different permeability and diffusion capabilities. The results indicated that the main differences among CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub> during desorption are reflected in the parameters of Langmuir volume, permeability, and diffusion coefficient. These parameters showed that CO<sub>2</sub> has the highest value during desorption, while N<sub>2</sub> has the lowest. The factors affecting the magnitude of differences between CO<sub>2</sub>, CH<sub>4</sub>, and N<sub>2</sub> are mainly their compositions. Specifically, ash content significantly affects the difference in adsorption capacity, while moisture content influences permeability and diffusion coefficient. During desorption, permeability plays a continuous role throughout the whole process, while diffusion coefficient is exhibited mainly in the initial stage of desorption. Different gases have varying sensitivities to permeability and diffusion coefficients during desorption. Changes in permeability and diffusion coefficient significantly affect the CO<sub>2</sub> desorption process. N<sub>2</sub>, on the other hand, is the least sensitive, especially to changes in diffusion coefficient. During gas flow, when reservoir permeability is less than 0.01 mD (= 9.869233 × 10<sup>−18</sup> m<sup>2</sup>), permeability becomes the main factor that affects flow. When the diffusion coefficient is less than 5 × 10<sup>−9</sup> m<sup>2</sup>/s, increasing the diffusion coefficient is necessary to effectively promote gas outflow. To effectively increase gas production, it is necessary to comprehensively consider the magnitudes of permeability and diffusion coefficient.</p>","PeriodicalId":54284,"journal":{"name":"Natural Resources Research","volume":"58 1","pages":""},"PeriodicalIF":4.8000,"publicationDate":"2024-05-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Natural Resources Research","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1007/s11053-024-10357-x","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0
Abstract
With increasing emphasis on low-carbon environmental protection, CO2 enhanced coalbed methane production and methane reuse in abandoned mines (rich in N2) have gradually become one of the future development directions. These scenarios involve the coordinated migration of different gases such as CO2, CH4, and N2, and the differences in properties of different gases that affect the flow process. Previous studies often focused on the adsorption differences between gases, neglecting the differences during desorption process. In view of this, the current work conducted experiments and finite element numerical analysis on the desorption process of CO2, CH4, and N2, clarified the differences and influencing factors of desorption among the gases, and analyzed the flow change rules under different permeability and diffusion capabilities. The results indicated that the main differences among CO2, CH4, and N2 during desorption are reflected in the parameters of Langmuir volume, permeability, and diffusion coefficient. These parameters showed that CO2 has the highest value during desorption, while N2 has the lowest. The factors affecting the magnitude of differences between CO2, CH4, and N2 are mainly their compositions. Specifically, ash content significantly affects the difference in adsorption capacity, while moisture content influences permeability and diffusion coefficient. During desorption, permeability plays a continuous role throughout the whole process, while diffusion coefficient is exhibited mainly in the initial stage of desorption. Different gases have varying sensitivities to permeability and diffusion coefficients during desorption. Changes in permeability and diffusion coefficient significantly affect the CO2 desorption process. N2, on the other hand, is the least sensitive, especially to changes in diffusion coefficient. During gas flow, when reservoir permeability is less than 0.01 mD (= 9.869233 × 10−18 m2), permeability becomes the main factor that affects flow. When the diffusion coefficient is less than 5 × 10−9 m2/s, increasing the diffusion coefficient is necessary to effectively promote gas outflow. To effectively increase gas production, it is necessary to comprehensively consider the magnitudes of permeability and diffusion coefficient.
期刊介绍:
This journal publishes quantitative studies of natural (mainly but not limited to mineral) resources exploration, evaluation and exploitation, including environmental and risk-related aspects. Typical articles use geoscientific data or analyses to assess, test, or compare resource-related aspects. NRR covers a wide variety of resources including minerals, coal, hydrocarbon, geothermal, water, and vegetation. Case studies are welcome.