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Role of air-water interfaces in colloid transport in porous media: A review

机译:空气-水界面在多孔介质胶体运输中的作用

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摘要

Air-water interfaces play an important role in unsaturated porous media, giving rise to phenomena like capillarity. Less recognized and understood are interactions of colloids with the air-water interface in porous media and the implications of these interactions for fate and transport of colloids. In this review, we discuss how colloids, both suspended in the aqueous phase and attached at pore walls, interact with air-water interfaces in porous media. We discuss the theory of colloid/air-water interface interactions, based on the different forces acting between colloids and the air-water interface (DLVO, hydrophobic, capillary forces) and based on thermodynamic considerations (Gibbs free energy). Subsurface colloids are usually electrostatically repelled from the air-water interface because most subsurface colloids and the air-water are negatively charged. However, hydrophobic interactions can lead to attraction to the air-water interface. When colloids are at the air-water interface, capillary forces are usually dominant over other forces. Moving air-water interfaces are effective in mobilizing and transporting colloids from surfaces. Thermodynamic considerations show that, for a colloid, the air-water interface is the favored state as compared with the suspension phase, except for hydrophilic colloids in the nanometer size range. Experimental evidence indicates that colloid mobilization in soils often occurs through macropores, although matrix transport is also prevalent in absence of macropores. Moving air-water interfaces, e.g., occurring during infiltration, imbibition, or drainage, have been shown to scour colloids from surfaces and translocate colloids. Colloids can also be pinned to surfaces by thin water films and capillary menisci at the air-water-solid interface line, causing colloid retention and immobilization. Air-water interfaces thus can both mobilize or immobilize colloids in porous media, depending on hydrodynamics and colloid and surface chemistry.
机译:空气-水界面在不饱和多孔介质中起重要作用,引起毛细现象。胶体与多孔介质中的空气-水界面的相互作用以及这些相互作用对胶体的命运和运输的影响的认识和了解较少。在这篇综述中,我们讨论了既悬浮在水相中又附着在孔壁上的胶体如何与多孔介质中的空气-水界面相互作用。我们基于胶体与空气-水界面之间的不同作用力(DLVO,疏水力,毛细作用力)和热力学因素(吉布斯自由能)讨论胶体/空气-水界面相互作用的理论。通常,地下胶体和空气与水带负电,因此通常从空气-水界面处将其排斥。但是,疏水相互作用会导致吸引到空气-水界面。当胶体在空气-水界面处时,毛细作用力通常比其他作用力更重要。移动的空气-水界面有效地从表面动员和运输胶体。热力学考虑表明,对于胶体,与空气相的悬浮相相比,空气-水界面是有利的状态,除了纳米尺寸范围内的亲水胶体。实验证据表明,土壤中的胶体动员通常通过大孔发生,尽管在没有大孔的情况下基质运输也很普遍。例如在渗透,吸收或排水过程中发生的移动的空气-水界面已经显示出从表面冲刷胶体并使胶体移位。胶体还可以通过薄的水膜和空气-水-固体界面处的毛细管半月板固定在表面上,从而导致胶体滞留和固定。因此,取决于水动力,胶体和表面化学性质,空气-水界面可以使胶体在多孔介质中动员或固定。

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  • 来源
    《Water resources research》 |2017年第7期|5247-5275|共29页
  • 作者

    Flury Markus; Aramrak Surachet;

  • 作者单位

    Washington State Univ, Dept Crop & Soil Sci, Puyallup, WA 98371 USA|Washington State Univ, Dept Crop & Soil Sci, Pullman, WA 99164 USA;

    Kasetsart Univ, Dept Soil Sci, Fac Agr, Bangkok, Thailand;

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