Peng Sheng, Brusseau Mark L
School of Environment, Beijing Normal University, Key Laboratory of Water and Sediment Sciences of Ministry of Education, Beijing, 100875, China.
J Hydrol Eng. 2012 Jul 1;17(7). doi: 10.1061/(ASCE)HE.1943-5584.0000515.
The relationship between air-water interfacial area and capillary pressure under higher water-content conditions is investigated for four natural porous media. The results show that the magnitude of the air-water interfacial area increases with increasing capillary pressure, consistent with the decrease in water saturation. The maximum observed air-water interfacial areas are dependent upon the magnitude of residual water saturation, which itself is condition dependent. The more well-sorted porous medium exhibited a greater rate of change of air-water interfacial area with capillary pressure than the more poorly-sorted porous media. The observed relationship between air-water interfacial area and capillary pressure was quantified by coupling an empirical equation describing the air-water interfacial area vs. water saturation relationship with the van Genuchten equation relating water saturation and capillary pressure. This equation produced reasonable simulations of the measured data.
针对四种天然多孔介质,研究了高含水率条件下空气-水界面面积与毛细压力之间的关系。结果表明,空气-水界面面积的大小随毛细压力的增加而增大,这与水饱和度的降低相一致。观测到的最大空气-水界面面积取决于残余水饱和度的大小,而残余水饱和度本身也取决于具体条件。分选较好的多孔介质比分选较差的多孔介质表现出空气-水界面面积随毛细压力变化的更大速率。通过将描述空气-水界面面积与水饱和度关系的经验方程与联系水饱和度和毛细压力的van Genuchten方程相结合,对观测到的空气-水界面面积与毛细压力之间的关系进行了量化。该方程对测量数据进行了合理的模拟。