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Published online 26 July 2006
Published in Vadose Zone J 5:877-885 (2006)
DOI: 10.2136/vzj2005.0086
© 2006 Soil Science Society of America
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Virus Transport in Saturated and Unsaturated Sand Columns

S. Torkzabana,*, S. M. Hassanizadeha, J. F. Schijvenb, H. A. M. de Bruinb and A. M. de Roda Husmanb

a Dep. of Earth Sciences, Utrecht University, P.O. Box 80021, 3508 TA Utrecht, The Netherlands
b Microbiological Laboratory for Health Protection, National Institute of Public Health and the Environment, P.O. Box 1, 3720 BA Bilthoven, The Netherlands

Figure 1
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  		Fig. 1. Schematic of the experimental column apparatus.

 

Figure 2
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  		Fig. 2. Measured (symbols) and fitted (lines) breakthrough curves of salt tracer (NaCl) in Exp. LpHi52 (52% saturation).

 

Figure 3
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  		Fig. 3. Measured (symbols) and fitted (lines) breakthrough curves of MS2 and {phi}X174 at pH 9 and ionic strength 0.6 mM in Exp. HpLi100 (100% saturation) and HpLi65 (65% saturation). Left plots: C/C0 on linear scale. Right plots: C/C0 on log scale.

 

Figure 4
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  		Fig. 4. Measured (symbols) and fitted (lines) breakthrough curves of MS2 and {phi}X174 at pH 7 and ionic strength 19 mM in Exp. LpHi100 (100% saturation), LpHi65 (66% saturation), and LpHi52 (52% saturation). Left plots: C/C0 on linear scale. Right plots: C/C0 on log scale.

 




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