Poster Number 11
See more from this Division: Joint Sessions
See more from this Session: Soils through Time: Critical Zone Studies of Processes and Their Effects (Posters)
Abstract:
Investigation of the salt deposition mechanism shows that salt crust properties depend on salt species. Salts with high solubility appear to form crusts at the top of the matrix that is very thick and dense, with a resulting decrease in the evaporation rates due to reduction in the matrix permeability. Surface roughness also affects the way in which the salt precipitates. Preliminary results suggest that salts tend to precipitate in micro cracks on the matrix surface. Column experiments indicate that the evaporation rates from heterogeneous matrices with vertical textural interface between fine coarse textures are 1.5 times higher than the evaporation rates from homogeneous fine textured matrices, with salt crust forming in both cases. This was observed for heterogeneous columns which were vertically divided into half fine and half coarse sand, as well as for columns which were divided into quarters.
Our observations show that matrix heterogeneity moderates the effect of salt crust on evaporation relative to homogeneous media, as the large pores in the heterogeneous media remain open for the flow of water vapor.
See more from this Division: Joint Sessions
See more from this Session: Soils through Time: Critical Zone Studies of Processes and Their Effects (Posters)