Full TGIF Record # 217025
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DOI:10.2134/jeq2011.0470
Web URL(s):https://www.dl.sciencesocieties.org/publications/jeq/articcles/42/1/83
    Last checked: 11/02/2016
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https://www.dl.sciencesocieties.org/publications/jeq/pdfs/42/1/83
    Last checked: 11/02/2016
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Publication Type:
i
Refereed
Author(s):Tian, Kun; Huang, Chi-Hua; Wang, Guang-Qian; Fu, Xu-Dong; Parker, Gary
Author Affiliation:Tian: China Water International Engineering Consulting Co. Ltd.; Tian, Wang, and Fu: State Key Lab. of Hydro-Science and Engineering and Dep. of Hydraulic Engineering, Tsinghua Univ., Beijing, China; Huang: National Soil Loss Research Lab, USDA-ARS, West Lafayette, IN; Parker: Dep. of Civil & Environmental Engineering and Dep. of Geology, Univ. of Illinois Urbana, Champaign, IL
Title:Quantification of chemical transport processes from the soil to surface runoff
Section:Technical reports: Groundwater quality
Other records with the "Technical reports: Groundwater quality" Section
Source:Journal of Environmental Quality. Vol. 42, No. 1, January 2013, p. 83-93.
Publishing Information:Madison, Wisconsin: American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
# of Pages:11
Related Web URL:https://www.dl.sciencesocieties.org/publications/jeq/abstracts/42/1/83
    Last checked: 11/02/2016
    Notes: Abstract only
Keywords:TIC Keywords: Seepage; Soil water; Surface runoff
Abstract/Contents:"There is a good conceptual understanding of the processes that govern chemical transport from the soil to surface runoff, but few studies have actually quantified these processes separately. Thus, we designed a laboratory flow cell and experimental procedures to quantify the chemical transport from soil to runoff water in the following individual processes: (i) convection with a vertical hydraulic gradient, (ii) convection via surface flow or the Bernoulli effect, (iii) diffusion, and (iv) soil loss. We applied different vertical hydraulic gradients by setting the flow cell to generate different seepage or drainage conditions. Our data confirmed the general form of the convection-diffusion equation. However, we now have additional quantitative data that describe the contribution of each individual chemical loading process in different surface runoff and soil hydrological conditions. The results of this study will be useful for enhancing our understanding of different geochemical processes in the surface soil mixing zone."
Language:English
References:38
Note:Equations
Figures
Tables
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ASA/CSSA/SSSA Citation (Crop Science-Like - may be incomplete):
Tian, K., C.-H. Huang, G.-Q. Wang, X.-D. Fu, and G. Parker. 2013. Quantification of chemical transport processes from the soil to surface runoff. J. Environ. Qual. 42(1):p. 83-93.
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DOI: 10.2134/jeq2011.0470
Web URL(s):
https://www.dl.sciencesocieties.org/publications/jeq/articcles/42/1/83
    Last checked: 11/02/2016
    Access conditions: Item is within a limited-access website
https://www.dl.sciencesocieties.org/publications/jeq/pdfs/42/1/83
    Last checked: 11/02/2016
    Requires: PDF Reader
    Access conditions: Item is within a limited-access website
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