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Effect of Soil Properties on Saturated and Unsaturated Virus Transport through Columns

Yanjie Chua,c, Yan Jin*,a, Thomas Baumannb and Marylynn V. Yatesc

a Department of Plant and Soil Sciences, University of Delaware, Newark, DE 19717
b Institute of Hydrochemistry, Technical University of Munich, Marchioninistrasse 17, D-81377, Munich, Germany
c Y. Chu, current address), Department of Environmental Sciences, University of California, Riverside, CA 92521



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  		Fig. 1. Transport of bromide tracer through Delaware 1 and 2, California, Arizona, and Georgia soil columns. The term C/C0 refers to the ratio of outflow concentration to input concentration. (Bromide curve was not measured for the saturated experiment with Georgia soil by accident).

 


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  		Fig. 2. Virus breakthrough curves from columns packed with Delaware 1 and 2 soils. The term C/C0 refers to the ratio of outflow concentration to input concentration.

 


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  		Fig. 3. Virus breakthrough curves from columns packed with soils California, Arizona, and Georgia. The term C/C0 refers to the ratio of outflow concentration to input concentration.

 




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The SCI Journals Agronomy Journal Crop Science
Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
and Life Sciences Education		 Soil Science Society of America Journal
Copyright © 2003 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.