滲透性

流体力学地球科学中,渗透性(通常符号为k)是衡量多孔介質(通常是岩石)是否能讓流体順利穿透的一種指標。介质的滲透性与孔隙率有关,也与介质中孔隙的形状有关。[1]

参考文献

  1. Bense, V.F.; Gleeson, T.; Loveless, S.E.; Bour, O.; Scibek, J. . Earth-Science Reviews. 2013, 127: 171–192 [2021-04-11]. Bibcode:2013ESRv..127..171B. doi:10.1016/j.earscirev.2013.09.008. (原始内容存档于2020-08-29) (英语).
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