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一种测量克努森扩散和机械变形对页岩渗透率综合影响的高效实验室方法。

An efficient laboratory method to measure the combined effects of Knudsen diffusion and mechanical deformation on shale permeability.

机构信息

Aramco Services Company, Aramco Research Center, Houston.

Aramco Services Company, Aramco Research Center, Houston.

出版信息

J Contam Hydrol. 2020 Jun;232:103652. doi: 10.1016/j.jconhyd.2020.103652. Epub 2020 May 5.

Abstract

In a shale gas reservoir, the rock matrix has a relatively large porosity and gas in place, but extremely low permeability. Thus, the rock matrix is a bottleneck for shale gas flow from the reservoir to hydraulic fractures and then to the production well. We speculate that the next big thing after hydraulic fracturing for unconventional resources development is to enhance the matrix permeability in an economically feasible way. Consequently, the efficient and accurate characterization of rock matrix permeability in the laboratory is a critical task. The current laboratory techniques for source rock permeability measurement follow a "point-by-point" approach. They need multiple test runs to obtain a permeability-pressure curve, because they can only measure one permeability data point for one test run, and are thus time consuming. The root cause of this "point-by-point" approach is that these laboratory techniques are based on linearized gas flow theory requiring only small pore pressure disturbances to the experiment system. Liu et al. (2019) and this work introduce a new methodology that is based on the nonlinear gas flow theory and allows for direct measurement of the permeability-pressure curve with a single test run. This makes the approach highly time efficient. The feasibility and validity of the methodology are demonstrated in this work based on laboratory measurement results and their consistency with theoretical expectations and other independent measurements. The observed permeability exhibits a complex relationship with pore pressure as a result of the combined effects of Knudsen diffusion and mechanical deformation. For a given confining pressure, the observed permeability initially decreases with pore pressure because of Knudsen diffusion and then increases with pore pressure owing to the mechanical deformation. A rock sample with a lower permeability corresponds to a stronger Knudsen diffusion effect and weaker mechanical diffusion effect. This complex behavior highlights the need to accurately and efficiently measure the combined effects that may have important impacts on shale gas production.

摘要

在页岩气藏中,岩石基质具有较大的孔隙度和原地气量,但渗透率极低。因此,岩石基质是页岩气从储层流向水力裂缝再到生产井的流动的瓶颈。我们推测,非常规资源开发水力压裂之后的下一个大事件是以经济可行的方式提高基质渗透率。因此,在实验室中高效准确地描述岩石基质渗透率是一项关键任务。目前用于源岩渗透率测量的实验室技术采用“逐点”方法。它们需要多次测试运行才能获得渗透率-压力曲线,因为它们一次测试运行只能测量一个渗透率数据点,因此非常耗时。这种“逐点”方法的根本原因是这些实验室技术基于仅需要对实验系统进行小的孔隙压力干扰的线性化气流理论。刘等人(2019 年)和这项工作引入了一种新的方法,该方法基于非线性气流理论,允许通过单次测试运行直接测量渗透率-压力曲线。这使得该方法非常高效。在这项工作中,基于实验室测量结果及其与理论预期和其他独立测量结果的一致性,证明了该方法的可行性和有效性。观察到的渗透率由于克努森扩散和机械变形的综合影响,与孔隙压力呈现出复杂的关系。对于给定的围压,观察到的渗透率最初由于克努森扩散而随孔隙压力降低,然后由于机械变形而随孔隙压力增加。渗透率较低的岩石样品对应更强的克努森扩散效应和较弱的机械扩散效应。这种复杂的行为突出了需要准确和有效地测量可能对页岩气生产产生重要影响的综合效应。

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