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首页> 外文期刊>Journal of natural gas science and engineering >A fully coupled thermal-hydraulic-mechanical model with two-phase flow for coalbed methane extraction
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A fully coupled thermal-hydraulic-mechanical model with two-phase flow for coalbed methane extraction

机译:煤层气抽采的两相流全热力-水力-力学模型

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Although the interaction of gas and coal has been comprehensively investigated in coalbed methane (CBM) extraction process, fewer scholars have taken the effect of temperature and groundwater into account, which brought a large deviation for CBM extraction design. In this study, a fully coupled thermal hydraulic-mechanical model (THM) including coal deformation, gas seepage, water seepage, and thermal transport governing equations is developed and solved using the finite element (FE) method. The coal mass is simplified as a dual-porosity and single -permeability media while CBM migration is considered as a tandem process of desorption, diffusion and seepage. The dynamic evolution model of permeability serving as the coupled term for THM model is developed under the combined impact of stress, water pressure, gas pressure, gas adsorption/desorption and temperature. The proposed model is first verified by showing that the modeled gas production rate and water production rate match reasonably with the in-situ measured ones. Different coupled models for CBM extraction were comparatively analyzed by accomplishing a series of simulations. It is found that the gas production rate of models ignored water effect monotonously reduces over time; while the model considered water effect rises at beginning and then gradually reduces. The model ignored water effect will overestimate gas production, and the model ignored thermal effect will underestimate gas production, particularly coal seam contains considerable amount of water. The evolution of permeability is the competition result of two opposite effects: the matrix shrinkage effect caused by temperature reduction, the matrix swelling effect caused by gas pressure decrease and methane adsorption increase. A rising permeability resulted from the integrative action of both lower reservoir temperature and pressure during CBM extraction is observed. The impact of initial water saturation on gas production can not be ignored in the whole extraction process, especially during the water drainage period. Gas production rate of CBM well decreases with initial reservoir temperature, initial water saturation and Langmuir volume constant, while increases with the Klinkenberg factor. Permeability rate increases with initial water saturation and Klinkenberg factor, however decreases with initial reservoir temperature. As Langmuir volume constant increases, the peaking value of gas production rate increases and delays. The Klinkenberg effect promotes coalbed methane migration significantly, ignoring which will underestimate the gas production, and the impact of Klinkenberg effect gradually increases with the drop of gas pressure. (C) 2016 Elsevier B.V. All rights reserved.
机译:尽管在煤层气(CBM)的提取过程中已对瓦斯与煤之间的相互作用进行了全面的研究,但很少有学者考虑温度和地下水的影响,这给煤层气提取设计带来了很大的偏差。在这项研究中,建立并使用有限元(FE)方法求解包括煤变形,气体渗流,水渗流和热输运控制方程的完全耦合的热力-力学模型(THM)。煤块简化为双孔隙度和单渗透率介质,而煤层气运移被认为是解吸,扩散和渗漏的串联过程。在应力,水压,气压,气体吸附/解吸和温度共同作用下,建立了渗透率的动态演化模型作为THM模型的耦合项。首先通过显示模型化的天然气生产率和水生产率与现场测量的天然气合理匹配来验证所提出的模型。通过完成一系列模拟,比较分析了煤层气提取的不同耦合模型。结果发现,忽略水效应的模型产气量随时间单调减少;而模型中考虑的水效应在开始时先升高,然后逐渐降低。忽略水效应的模型将高估天然气产量,而忽略热效应的模型将低估天然气产量,特别是煤层中含有大量的水。渗透率的演化是两个相反作用的竞争结果:温度降低引起的基体收缩效应,气压降低引起的基体溶胀效应和甲烷吸附增加。观察到煤层气提取过程中较低的储层温度和压力的综合作用导致渗透率上升。在整个开采过程中,尤其是排水期,不能忽略初始含水饱和度对产气的影响。煤层气井的产气速率随初始储层温度,初始含水饱和度和朗缪尔体积常数而降低,而随克林根贝格因子而升高。渗透率随初始含水饱和度和克林根贝格系数而增加,但随初始储层温度而降低。随着Langmuir体积常数的增加,产气量的峰值会增加并延迟。克林根贝格效应极大地促进了煤层气的运移,而忽略了后者会低估瓦斯的产生,克林根贝格效应的影响随着气压的降低而逐渐增加。 (C)2016 Elsevier B.V.保留所有权利。

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