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Numerical Simulation of Evaporation Process in Stony Soil


An older version of this resource http://www.hydroshare.org/resource/88c4b48519d24ef3a9fbb2641ad2cafe is available.
Authors: Kshitij Parajuli · Scott B. Jones · Morteza Sadeghi
Owners: Kshitij Parajuli
Resource type:Generic
Created:March 16, 2017, 6:18 p.m.
Last updated: March 21, 2017, 11:08 p.m. by Kshitij Parajuli

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.

Subject

HYDRUS-3D,Stony Soil,Evaporation Experiment,HYPROP,Water Retention Curve

How to cite

Parajuli, K., S. B. Jones, M. Sadeghi (2017). Numerical Simulation of Evaporation Process in Stony Soil, HydroShare, http://dx.doi.org/10.4211/hs.72fa9b3835264b11b8661f2655997346

This resource is shared under the Creative Commons Attribution CC BY.

 http://creativecommons.org/licenses/by/4.0/
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Authors

The people or organizations that created the intellectual content of the resource.

Name Organization Address Phone
Kshitij Parajuli
Scott B. Jones Utah State University
Morteza Sadeghi Utah State University 4820 Old Main Hill

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http://www.hydroshare.org/resource/88c4b48519d24ef3a9fbb2641ad2cafe

Credits

This resource was created using funding from the following sources:
Agency Name Award Title Award Number
iUTAH

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