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首页> 外文期刊>International Journal of Greenhouse Gas Control >Effect of the effective stress coefficient and sorption-induced strain on the evolution of coal permeability: Experimental observations
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Effect of the effective stress coefficient and sorption-induced strain on the evolution of coal permeability: Experimental observations

机译:有效应力系数和吸附诱发应变对煤渗透性演化的影响:实验观察

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摘要

Permeability is one of the most important parameters for C02 injection in coal to enhance coalbed methane recovery. Laboratory characterization of coal permeability provides useful information for in situ permeability behavior of coal seams when adsorbing gases such as CO_2 are injected. In this study, a series of experiments have been conducted for coal samples using both non-adsorbing and adsorbing gases at various confining stresses and pore pressures. Our observations have showed that even undercontrolled stress conditions, coal permeability decreases with respect to pore pressure during the injection of adsorbing gases. In order to find out the causes of permeability decrease for adsorbing gases, a non-adsorbing gas (helium) is used to determine the effective stress coefficient. In these experiments using helium, the impact of gas sorption can be neglected and any permeability reduction is considered as due to the variation in the effective stress, which is controlled by the effective stresscoefficient. The results show that the effective stress coefficient is pore pressure dependent and less than unity for the coal samples studied. The permeability reduction from helium experiments is then used to calibrate the subsequent flow-through experiments using adsorbing gases, CH_4 and CO_2 . Through this calibration, the sole effect of sorption-induced strain on permeability change is obtained for these adsorbing gas flow-through experiments. In this paper, experimental results and analyses arereported including how the impact of effective stress coefficient is separated from that of the sorption-induced strain on the evolution of coal permeability.
机译:渗透率是用于煤中CO 2注入以提高煤层甲烷采收率的最重要参数之一。煤渗透率的实验室表征为注入吸附气体(例如CO_2)时煤层的原位渗透行为提供了有用的信息。在这项研究中,已经对煤样品进行了一系列实验,这些煤在不同的围压和孔隙压力下都使用了非吸附和吸附气体。我们的观察表明,即使在受控的应力条件下,在吸附气体注入过程中,煤的渗透性也会相对于孔隙压力而下降。为了找出吸附气体的渗透率降低的原因,使用非吸附气体(氦气)确定有效应力系数。在这些使用氦气的实验中,可以忽略气体吸附的影响,并且认为任何渗透率降低都归因于有效应力的变化,有效应力受有效应力系数控制。结果表明,所研究的煤样品的有效应力系数与孔隙压力有关,且小于1。然后,使用氦气CH_4和CO_2吸收来自氦气实验的渗透率降低,以校准后续的流通实验。通过该校准,对于这些吸附气体通过实验,获得了吸附引起的应变对渗透率变化的唯一影响。本文报告了实验结果和分析结果,包括如何将有效应力系数的影响与吸附引起的应变的影响分开,从而影响煤的渗透性。

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