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Pore Structure and Limit Pressure of Gas Slippage Effect in Tight Sandstone

机译:致密砂岩的孔隙结构和气滑效应极限压力

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摘要

Gas slip effect is an important mechanism that the gas flow is different from liquid flow in porous media. It is generally considered that the lower the permeability in porous media is, the more severe slip effect of gas flow will be. We design and then carry out experiments with the increase of backpressure at the outlet of the core samples based on the definition of gas slip effect and in view of different levels of permeability of tight sandstone reservoir. This study inspects a limit pressure of the gas slip effect in tight sandstones and analyzes the characteristic parameter of capillary pressure curves. The experimental results indicate that gas slip effect can be eliminated when the backpressure reaches a limit pressure. When the backpressure exceeds the limit pressure, the measured gas permeability is a relatively stable value whose range is less than 3% for a given core sample. It is also found that the limit pressure increases with the decreasing in permeability and has close relation with pore structure of the core samples. The results have an important influence on correlation study on gas flow in porous medium, and are beneficial to reduce the workload of laboratory experiment.
机译:气体滑脱效应是气体在多孔介质中流动不同于液体流动的重要机制。通常认为多孔介质中的渗透率越低,气流的滑移效应将越严重。我们根据气滑效应的定义并考虑到致密砂岩储层渗透率的不同,设计并进行了岩心样品出口反压增加的实验。本文研究了致密砂岩中气滑作用的极限压力,并分析了毛细管压力曲线的特征参数。实验结果表明,当背压达到极限压力时,可以消除气滑效应。当背压超过极限压力时,测得的气体渗透率是一个相对稳定的值,对于给定的岩心样品,其范围小于3%。还发现极限压力随着渗透率的降低而增加,并且与岩心样品的孔结构密切相关。该结果对多孔介质中气体流动的相关性研究具有重要影响,有利于减少实验室实验的工作量。

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