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首页> 外文期刊>International Journal of Heat and Mass Transfer >Modelling the water transport behavior in organic-rich nanoporous shale with generalized lattice Boltzmann method
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Modelling the water transport behavior in organic-rich nanoporous shale with generalized lattice Boltzmann method

机译:用广义格子玻尔兹曼方法模拟富含有机物的纳米多孔页岩中的水运移行为

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摘要

The hydraulic fracturing fluid could easily infiltrate the ultra-tight shale matrix due to the large slip of the liquid flow, showing higher-than-expected fluid-loss in varieties of shale gas development cases. One possible reason is that the water transport behaviors through the pores with nanoscale significantly deviate from that occurring at larger scales. The classic Darcy law, being widely and successfully used in conventional porous media becomes insufficient for the nanoporous shale. In this study, a generalized lattice Boltzmann method with liquid slip effect incorporated is established to understand the transport behavior of hydraulic fracturing fluid in nanopores dominated shale matrix and to demonstrate a new insight into the transport behaviors. The results show that the flow capability of fracturing fluid in the shale matrix with strong hydrophobic organic nanopores is significantly improved due to the huge wall-fluid interaction. And this would considerably change the flow field (magnitudes and preferred pathway) with and without the micro-fractures, contributing a lot to the huge hydraulic fracturing fluid loss reported from the practical fields. The huge fluid-loss emphasizes the importance for liquid slip effect in organic nanopores of shale matrix. Especially, in the organic-rich shale gas reservoir, the fracturing fluid can be infiltrated into the ultra-tight shale formation easier than commonly expected during the hydraulic fracturing operation.
机译:由于液流的滑动较大,水力压裂液很容易渗透到超致密的页岩基质中,在各种页岩气开发案例中显示出比预期高的流体损失。一个可能的原因是水通过纳米尺度的孔的传输行为明显偏离了较大尺度的行为。被广泛成功地用于常规多孔介质中的经典达西定律不足以用于纳米多孔页岩。在这项研究中,建立了具有滑移效应的广义格子玻尔兹曼方法,以了解水力压裂液在以纳米孔为主的页岩基质中的运移行为,并展示了对运移行为的新见解。结果表明,由于巨大的壁液相互作用,压裂液在具有强疏水性有机纳米孔的页岩基质中的流动能力得到了显着改善。不论有无微裂缝,这都将大大改变流场(幅度和首选路径),从而为实际领域报道的巨大水力压裂液损失做出了很大贡献。巨大的流体损失强调了页岩基质有机纳米孔中液体滑动作用的重要性。特别是,在富含有机物的页岩气储层中,与水力压裂操作中通常期望的相比,压裂液可以更容易地渗透到超致密页岩地层中。

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