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| Type: | Resource | |
| Storage: | The size of this resource is 88.0 MB | |
| Created: | Mar 14, 2017 at 9:23 p.m. | |
| Last updated: | Mar 16, 2017 at 6:18 p.m. (Metadata update) | |
| Published date: | Mar 15, 2017 at 1:30 p.m. | |
| DOI: | 10.4211/hs.88c4b48519d24ef3a9fbb2641ad2cafe | |
| Citation: | See how to cite this resource |
| Sharing Status: | Published |
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| Views: | 2219 |
| Downloads: | 78 |
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Abstract
The simplified evaporation experiment was simulated using HYDRUS 3D which numerically solves the Richard’s equation (Simunek et al., 2016). A three-dimensional evaporation process simulation (i.e., HYPROP apparatus) was performed for Millville silt loam with 40% coarse sandstone by volume. The soil hydraulic parameters for the Millville silt loam and coarse sandstone were determined by fitting the van Genuchten model to their measured WRC data. The initial condition was set to saturated water content for both soil and stone inclusions. The upper boundary condition was set as the temporally variable evaporation rate measured during the evaporation experiment. The bottom boundary condition was set as zero flux.
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Related Resources
| This resource has been replaced by a newer version | Parajuli, K., S. B. Jones, M. Sadeghi (2017). Numerical Simulation of Evaporation Process in Stony Soil, HydroShare, https://doi.org/10.4211/hs.72fa9b3835264b11b8661f2655997346 |
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This resource was created using funding from the following sources:
| Agency Name | Award Title | Award Number |
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| iUTAH |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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