The Time-Varying Variation Characteristics of Methane during Nitrogen Injection Process: An Experimental Study on Bituminous Coals

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2023-12-11 DOI:10.1155/2023/5075888
Aoxiang Zhang, Longyong Shu, Zhonggang Huo, Xin Song
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Abstract

The existing research on CH4 displacement by N2 mainly focuses on the gas injection displacement mechanism and the factors affecting displacement efficiency. And most of them are theoretical analyses at the model level or multifactor analyses at the simulation test level, while there are few targeted physical simulation tests and quantitative analyses. Given the above problems, the experiment system was used to study the gas migration evolution law and time-varying characteristics of CH4 displacement by N2 in coal under different injection pressures. The experimental results show that the whole process of CH4 displacement by N2 can be divided into three stages: stage I (original equilibrium stage); stage II (dynamic balance stage); stage III (new equilibrium stage). The concentration of CH4 and N2 presents an opposite variation trend, and the variation rate of CH4 and N2 increased first and then decreased. The breakthrough time was 50 minutes, 45 minutes, 35 minutes, 25 minutes, and 20 minutes, respectively, under different injection pressures. The displacement efficiency increased with the injection pressures, while the replacement ratio decreased with the injection pressures. The maximum flow rate of CH4 was 0.085 mL/min, 0.110 mL/min, 0.130 mL/min, 0.222 mL/min, and 0.273 mL/min, respectively, under different injection pressures. The accumulated production of CH4 was 3.59 mL, 3.91 mL, 4.39 mL, 5.58 mL, and 5.94 mL, respectively, under different injection pressures. The effective injection pressure range was 1.6~2 MPa. This research can provide a reference for the theoretical research of N2-ECBM-related technology in low permeability reservoirs and the selection of injection pressure in the field technology implementation.
注氮过程中甲烷的时变特性:沥青煤的实验研究
现有的 N2 对 CH4 的置换研究主要集中在气体注入置换机理和影响置换效率的因素上。且多为模型层面的理论分析或模拟试验层面的多因素分析,有针对性的物理模拟试验和定量分析较少。鉴于上述问题,本文利用实验系统研究了不同注入压力下煤中 N2 置换 CH4 的气体迁移演化规律和时变特征。实验结果表明,N2置换CH4的整个过程可分为三个阶段:第一阶段(原始平衡阶段);第二阶段(动态平衡阶段);第三阶段(新平衡阶段)。CH4 和 N2 的浓度呈相反的变化趋势,CH4 和 N2 的变化率先增大后减小。在不同注入压力下,突破时间分别为 50 分钟、45 分钟、35 分钟、25 分钟和 20 分钟。置换效率随注入压力的增加而提高,置换率则随注入压力的增加而降低。在不同注入压力下,CH4 的最大流速分别为 0.085 mL/min、0.110 mL/min、0.130 mL/min、0.222 mL/min 和 0.273 mL/min。在不同的注入压力下,CH4 的累积产量分别为 3.59 mL、3.91 mL、4.39 mL、5.58 mL 和 5.94 mL。有效注入压力范围为 1.6~2 MPa。该研究可为低渗透油藏中 N2-ECBM 相关技术的理论研究和现场技术实施中注入压力的选择提供参考。
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来源期刊
Geofluids
Geofluids 地学-地球化学与地球物理
CiteScore
2.80
自引率
17.60%
发文量
835
期刊介绍: Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.
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