Salt crystallisation at the surface of a heterogeneous porous medium

S. Veran-Tissoires, M. Marcoux, M. Prat
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引用次数: 40

Abstract

Evaporation of saline solutions from a porous medium often leads to the precipitation of salt at the surface of the porous medium. It is commonly observed that the crystallized salt does not form everywhere at the porous medium surface but only at some specific locations. To explain this phenomenon, we consider efflorescence formation at the surface of a saturated heterogeneous porous column (finer porous medium in coarse porous medium background) in the wicking situation. We study the impact of permeability and porosity contrasts on the efflorescence formation location from a simple visualisation experiment and Darcy's scale numerical simulations. We show that the porosity is the most sensitive parameter for our experiment and that efflorescence forms at the surface of the medium of lower porosity. A simple efflorescence growth model is then used to explain why the efflorescence continues to grow at the surface of the lower porosity medium without spreading over the adjacent surface of the greater porosity medium.
盐在非均质多孔介质表面的结晶
多孔介质中盐溶液的蒸发常常导致多孔介质表面盐的沉淀。通常观察到,盐的结晶不是在多孔介质表面的所有地方形成,而只是在某些特定的位置形成。为了解释这一现象,我们考虑了在吸湿情况下,在饱和非均质多孔柱(粗多孔介质背景中的细多孔介质)表面的花期形成。通过简单的可视化实验和达西比例尺数值模拟,研究了渗透率和孔隙度对比对花期形成位置的影响。我们发现孔隙度是我们实验中最敏感的参数,并且在孔隙度较低的介质表面形成花。然后使用一个简单的花序生长模型来解释为什么花序继续在低孔隙度介质的表面生长,而没有扩散到大孔隙度介质的邻近表面。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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