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Effects of matrix moisture on gas diffusion and flow in coal

机译:基质水分对煤中瓦斯扩散和流动的影响

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摘要

Gas production from coal is a complex process whereby gas, initially adsorbed in the coal matrix, desorbs and diffuses through the matrix into the cleat and eventually flows through the cleat system into a production well or a drainage borehole. Hence, the gas production rate is mainly controlled by the gas dif-fusivity in the matrix and gas permeability in the cleat system. Moisture in the coal matrix has significant impact on gas adsorption capacity and would also play a key role in desorption and migration of gas. However, how moisture affects gas desorption and diffusion in the coal matrix is still poorly understood. In this work, experimental study is performed to investigate effects of moisture on gas sorption rate for an Australian coal. Coal seam gases, CH_4 and CO_2, are used in the study. The experimental results show that moisture content in the matrix has significant impact on the gas sorption rate and the impact of moisture content on the diffusion rate is stronger for CH_4 than CO_2. Moreover, the impact of moisture on gas diffusivity in pores with different size is different, suggested from the modelling results using the bidisperse approach. Furthermore, moisture in coal matrix would cause coal swelling/shrinkage and mechanical properties change that could impact on coal permeability under reservoir conditions. Experimental measurements of coal matrix swelling and Young's modulus on the same coal sample show that matrix moisture content has significant impact on those properties and may have significant implications on coalbed methane recovery and CO_2 storage in coal.
机译:煤的天然气生产是一个复杂的过程,最初吸附在煤基质中的气体通过基质解吸并扩散到煤层中,最后通过煤层系统流入生产井或排水井。因此,产气率主要由基质中的气体扩散率和夹板系统中的气体渗透率控制。煤基质中的水分对气体的吸附能力有重要影响,并且在气体的解吸和运移中也起着关键作用。然而,对于水分如何影响煤基质中的气体解吸和扩散仍知之甚少。在这项工作中,进行了实验研究以调查水分对澳大利亚煤炭的气体吸附率的影响。研究中使用了煤层气CH_4和CO_2。实验结果表明,CH_4基质中的水分含量对气体吸附速率有显着影响,水分含量对扩散速率的影响比CO_2强烈。此外,使用双分散方法的模拟结果表明,水分对不同尺寸孔隙中气体扩散系数的影响是不同的。此外,煤基质中的水分会引起煤溶胀/收缩和机械性能的变化,从而影响储层条件下的煤渗透率。在相同的煤样上对煤基质膨胀和杨氏模量进行的实验测量表明,基质含水量对这些性质具有显着影响,并且可能对煤层气的采收率和煤中的CO_2储存产生重大影响。

著录项

  • 来源
    《Fuel》 |2010年第11期|P.3207-3217|共11页
  • 作者单位

    CSIRO Earth Science and Resource Engineering, Ian Wark Laboratory, Bayview Avenue, Clayton, Victoria 3168, Australia;

    rnCSIRO Earth Science and Resource Engineering, Ian Wark Laboratory, Bayview Avenue, Clayton, Victoria 3168, Australia;

    rnCSIRO Earth Science and Resource Engineering, Ian Wark Laboratory, Bayview Avenue, Clayton, Victoria 3168, Australia;

    rnCSIRO Earth Science and Resource Engineering, Ian Wark Laboratory, Bayview Avenue, Clayton, Victoria 3168, Australia;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    gas drainage; bidisperse diffusion model; coalbed methane; CO_2 storage; coal swelling;

    机译:瓦斯抽放;双分散扩散模型煤层气CO_2储存;煤溶胀;

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