Abstract
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 versus water saturation relationship with the van Genuchten equation relating water saturation and capillary pressure. This equation produced reasonable simulations of the measured data.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 829-832 |
| Number of pages | 4 |
| Journal | Journal of Hydrologic Engineering |
| Volume | 17 |
| Issue number | 7 |
| DOIs | |
| State | Published - 2012 |
Keywords
- Interfacial
- Soil water
- Vadose zone
ASJC Scopus subject areas
- Environmental Chemistry
- Civil and Structural Engineering
- Water Science and Technology
- General Environmental Science