Technical Papers
Mar 26, 2012

Modeling Soil Solute Release into Runoff and Transport with Runoff on a Loess Slope

Publication: Journal of Hydrologic Engineering
Volume 18, Issue 5

Abstract

Rainfall results in the transfer of chemicals from soil to surface runoff. A physically-based solute transport model was developed for estimating the solute concentration in runoff originating from the soil surface. The model accounts for the effects of soil infiltration, raindrops, the water runoff rate, and the return flow, all of which influence the concentration of the solutes in the runoff. It was assumed that the depth of mixing zone changed with the varieties of the raindrop hits, return flow, and overland flow. It was also assumed that runoff and soil in the mixing zone mixed instantaneously and that the solute in the soil beneath the mixing zone was moved to the mixing zone by diffusion. The mixing zone was included in the model and was based on the deposited layer or shield concept. To test the model, laboratory experiments were carried out that used two soil types that were exposed to simulated rainfall. The results simulated by the model were highly correlated with the experimental data. In the first few minutes after rainfall began, the solute concentration in the runoff was mainly controlled by the rainfall rate and solute concentration in the mixing zone; higher solute levels in the mixing zone resulted in higher solute concentrations in runoff. When the solute concentration in the runoff stabilized, the solute concentration in the runoff was mainly controlled by the diffusion of solutes from the soil beneath the mixing zone. The simulated data showed a high level of correlation with the measured data for both runoff volume and solute concentration in the runoff. This demonstrates that the model captured the temporal behavior of the runoff and solute transport in the runoff.

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Acknowledgments

This research was supported by the projects of the National Basic Research Program of China (2011CB411903). Thanks to the referees for suggestions and helpful comments.

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Published In

Go to Journal of Hydrologic Engineering
Journal of Hydrologic Engineering
Volume 18Issue 5May 2013
Pages: 527 - 535

History

Received: Sep 8, 2011
Accepted: Mar 23, 2012
Published online: Mar 26, 2012
Published in print: May 1, 2013

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Authors

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Wencai Dong [email protected]
Ph.D. Student, State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences, Yangling, Shaanxi 712100, China; and Graduate Univ. of Chinese Academy of Sciences, Beijing 100049, China. E-mail: [email protected]
Quanjiu Wang [email protected]
Professor, Institute of Water Resources, Xi’an Univ. of Technology, Xi’an, Shannxi 710048, China; and State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences, No. 26 Xinong Rd., Yangling, Shaanxi 712100, China (corresponding author). E-mail: [email protected]

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