CO2, CH4, and N2 Desorption Characteristics in a Low-Rank Coal Reservoir

IF 4.8 2区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Zhaoying Chen, Junqiang Kang, Xuehai Fu, Mingjie Liu, Qingling Tian, Jiahao Wu
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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.

Abstract Image

低层煤储层中的 CO2、CH4 和 N2 解吸特性
随着人们对低碳环保的日益重视,二氧化碳强化煤层气生产和废弃矿井(富含 N2)甲烷再利用逐渐成为未来的发展方向之一。这些方案涉及 CO2、CH4 和 N2 等不同气体的协调迁移,以及不同气体的特性差异对流动过程的影响。以往的研究通常侧重于气体之间的吸附差异,而忽略了解吸过程中的差异。有鉴于此,本研究对 CO2、CH4 和 N2 的解吸过程进行了实验和有限元数值分析,明确了气体间解吸的差异和影响因素,并分析了不同渗透性和扩散能力下的流动变化规律。结果表明,CO2、CH4 和 N2 在解吸过程中的主要差异体现在朗缪尔体积、渗透性和扩散系数等参数上。这些参数表明,二氧化碳在解吸过程中的值最高,而 N2 的值最低。影响 CO2、CH4 和 N2 之间差异大小的因素主要是它们的成分。具体来说,灰分含量对吸附容量的差异有很大影响,而水分含量则影响渗透性和扩散系数。在解吸过程中,渗透性在整个过程中起持续作用,而扩散系数主要在解吸的初始阶段表现出来。在解吸过程中,不同气体对渗透性和扩散系数的敏感程度各不相同。渗透性和扩散系数的变化对二氧化碳的解吸过程有很大影响。另一方面,N2 的敏感度最低,尤其是对扩散系数的变化。在气体流动过程中,当储层渗透率小于 0.01 mD(= 9.869233 × 10-18 m2)时,渗透率成为影响流动的主要因素。当扩散系数小于 5 × 10-9 m2/s 时,必须提高扩散系数才能有效促进气体流出。要有效提高产气量,必须综合考虑渗透率和扩散系数的大小。
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来源期刊
Natural Resources Research
Natural Resources Research Environmental Science-General Environmental Science
CiteScore
11.90
自引率
11.10%
发文量
151
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.
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