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Improved Method for Measuring the Permeability of Nanoporous Material and Its Application to Shale Matrix with Ultra-Low Permeability

机译:纳米多孔材料渗透率的改进测量方法及其在超低渗透率页岩基质中的应用

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Nanoporous materials have a wide range of applications in clean energy and environmental research. The permeability of nanoporous materials is low, which affects the fluid transport behavior inside the nanopores and thus also affects the performance of technologies based on such materials. For example, during the development of shale gas resources, the permeability of the shale matrix is normally lower than 10 ?3 mD and has an important influence on rock parameters. It is challenging to measure small pressure changes accurately under high pressure. Although the pressure decay method provides an effective means for the measurement of low permeability, most apparatuses and experiments have difficulty measuring permeability in high pressure conditions over 1.38 MPa. Here, we propose an improved experimental method for the measurement of low permeability. To overcome the challenge of measuring small changes in pressure at high pressure, a pressure difference sensor is used. By improving the constant temperature accuracy and reducing the helium leakage rate, we measure shale matrix permeabilities ranging from 0.05 to 2 nD at pore pressures of up to 8 MPa, with good repeatability and sample mass irrelevance. The results show that porosity, pore pressure, and moisture conditions influence the matrix permeability. The permeability of moist shale is lower than that of dry shale, since water blocks some of the nanopores.
机译:纳米多孔材料在清洁能源和环境研究中具有广泛的应用。纳米多孔材料的渗透性低,这影响了纳米孔内部的流体传输行为,因此也影响了基于此类材料的技术的性能。例如,在页岩气资源开发期间,页岩基质的渗透率通常低于10?3 mD,并且对岩石参数具有重要影响。在高压下准确测量小压力变化是一项挑战。尽管压力衰减法为测量低渗透率提供了有效的手段,但是大多数设备和实验都难以在1.38 MPa以上的高压条件下测量渗透率。在这里,我们提出了一种改进的测量低渗透率的实验方法。为了克服在高压下测量微小压力变化的挑战,使用了压力差传感器。通过提高恒温精度并降低氦气泄漏率,我们在孔隙压力高达8 MPa的情况下测量的页岩基质渗透率介于0.05到2 nD之间,具有良好的重复性和与样品质量无关。结果表明,孔隙度,孔隙压力和湿度条件会影响基质渗透率。湿页岩的渗透率低于干页岩的渗透率,因为水会阻塞一些纳米孔。

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