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Diffusion characteristics of nanoscale gas flow in shale matrix from Haenam basin, Korea

机译:韩国海南盆地页岩基质中纳米级气流的扩散特征

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To develop a shale gas reservoir, the gas flow in shale matrix essentially needs to be analyzed. The shale matrix consists of fractures and nanopores that have separate flow mechanisms. The purpose of this study is to investigate the gas diffusion in the nanopores of a shale matrix from the Haenam basin, Korea. To examine gas diffusion, an apparatus was developed to measure shale properties at the nanopore-scale. Subsequently, the measured properties were used to describe gas diffusion based on the Knudsen and Fick diffusion models. During the investigations, the pressure condition ranged from 0.69 to 41.37 MPa, setting temperature condition of 298.15 K. From the results, it was revealed that Knudsen diffusion was controlled by the pore sizes and pressure, while the Fick diffusion was governed by gas molecular radius and temperature. Therefore, shale gas diffusion should be evaluated by considering the parameters such as pore size, pressure, temperature, and gas molecular radius.
机译:为了开发页岩气储层,基本上需要分析页岩基质中的气流。页岩基质由具有独立流动机制的裂缝和纳米孔组成。这项研究的目的是研究韩国海南盆地页岩基质的纳米孔中的气体扩散。为了检查气体扩散,开发了一种在纳米孔尺度上测量页岩性质的设备。随后,基于Knudsen和Fick扩散模型,将测量的特性用于描述气体扩散。在研究过程中,压力条件为0.69至41.37 MPa,设定温度条件为298.15K。结果表明,Knudsen扩散受孔径和压力控制,而Fick扩散受气体分子半径控制和温度。因此,应通过考虑诸如孔径,压力,温度和气体分子半径等参数来评估页岩气的扩散。

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