Impact of gas adsorption on coal relative permeability: a laboratory study

IF 7.5 1区 工程技术 Q1 ENGINEERING, GEOLOGICAL
Tiancheng Zhang , Jimmy Xuekai Li , Yiran Zhu , Victor Rudolph , Zhongwei Chen
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Abstract

CO2 geo-sequestration and compressed air energy storage in depleted coal seam gas reservoirs are promising techniques for mitigating the greenhouse effect and combating climate change. However, gas adsorption-induced swelling in coal matrices poses challenges to gas injectivity by reducing both coal absolute permeability and relative permeability. While the sorption-induced impact on absolute permeability has been extensively studied, its impact on relative permeability remains little explored. To address this gap, a suite of two-phase flow experiments was conducted with both absorbing and non-absorbing gases. A series of relative permeability curves for helium-water, nitrogen-water, and CO2-water systems were obtained. The results show lower relative permeability for absorbing gas-water systems (nitrogen and CO2) compared to non-absorbing gas (helium) due to the sorption-induced swelling impact. Specifically, the relative permeability of helium-water systems is more than two times higher than that of nitrogen-water systems, followed by CO2-water injection due to differences in adsorption capacity. Finally, quantitative correlations for estimating the relative permeability of nitrogen-water and CO2-water systems were obtained, based on four newly introduced coefficients. These coefficients enable direct estimation of absorbing gas-water two-phase flow behavior (e.g., CO2 sequestration and compressed air storage) in coal. The applicability of these coefficients was further validated using data from other studies, providing useful insights for assessing the injectivity of CO2 geo-sequestration and underground compressed air energy storage.
气体吸附对煤相对渗透率影响的实验室研究
枯竭煤层天然气储层的二氧化碳地质封存和压缩空气储能技术是缓解温室效应和应对气候变化的有前途的技术。然而,煤基质中气体吸附引起的膨胀会降低煤的绝对渗透率和相对渗透率,从而对瓦斯注入性构成挑战。虽然吸附对绝对渗透率的影响已经被广泛研究,但对其对相对渗透率的影响却知之甚少。为了解决这一问题,我们对吸收型和非吸收型气体进行了两相流实验。得到了氦-水、氮-水和co2 -水体系的一系列相对渗透率曲线。结果表明,与非吸附性气体(氦气)相比,吸附性气体(氮气和CO2)的相对渗透率较低,这是由于吸附引起的膨胀影响。具体而言,氦-水体系的相对渗透率比氮-水体系高2倍以上,其次是co2 -水注入,因为吸附能力不同。最后,基于4个新引入的系数,得到了估算氮-水和二氧化碳-水系统相对渗透率的定量相关性。这些系数可以直接估计煤中吸收气水两相流动的行为(例如CO2封存和压缩空气储存)。利用其他研究的数据进一步验证了这些系数的适用性,为评估二氧化碳地质封存和地下压缩空气储能的注入性提供了有用的见解。
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来源期刊
CiteScore
14.00
自引率
5.60%
发文量
196
审稿时长
18 weeks
期刊介绍: The International Journal of Rock Mechanics and Mining Sciences focuses on original research, new developments, site measurements, and case studies within the fields of rock mechanics and rock engineering. Serving as an international platform, it showcases high-quality papers addressing rock mechanics and the application of its principles and techniques in mining and civil engineering projects situated on or within rock masses. These projects encompass a wide range, including slopes, open-pit mines, quarries, shafts, tunnels, caverns, underground mines, metro systems, dams, hydro-electric stations, geothermal energy, petroleum engineering, and radioactive waste disposal. The journal welcomes submissions on various topics, with particular interest in theoretical advancements, analytical and numerical methods, rock testing, site investigation, and case studies.
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