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Pore-Scale Visualization of Colloid Transport and Retention in Partly Saturated Porous Media

John T. Crista, John F. McCarthyb, Yuniati Zevia, Philippe Baveyec, James A. Throopa and Tammo S. Steenhuis*,a

a Dep. of Biological and Environmental Engineering, Riley-Robb Hall, Cornell University, Ithaca, NY 14853
b Dep. of Geological Sciences, Univ. of Tennessee, Knoxville, TN 37996
c Dep. of Crop and Soil Sciences, Cornell Univ., Ithaca, NY 14853



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Fig. 1. Principal components of the experimental setup. Not shown are the CDC camera and the computer system.

 


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Fig. 2. Moisture content of packed-sand layers 2 h after application of the colloidal suspension. Values reflect the average of five experiments; error bars shown are one standard deviation.

 


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Fig. 3. Menisci or air–water interfaces connecting sand grains after application.

 


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Fig. 4. (a) Menisci or air–water interfaces after 6 h of drainage; (b) colloid–water distribution after application of the colloidal suspension. Rewetting of the sand eliminated the static air–water interfaces.

 


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Fig. 5. Distribution of 0.8-µm hydrophilic colloids ({approx}3 x 107 particles mL–1) after application of the colloidal suspension. Values shown are depths below the top layer of the sand column.

 


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Fig. 6. (a) Blue banding patterns of 0.8-µm hydrophilic colloids ({approx}3 x 107 particles mL–1) after application of the colloidal suspension; (b) 1 h later. With time and continued drainage, the banding patterns widened and darkened to a deeper blue hue.

 


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Fig. 7. Water films at cross section of two grains with pendular ring.

 


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Fig. 8. Trapped air bubble between narrowly separated, hydrophilic solid surfaces.

 





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The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Soil Science Society of America Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2004 by the Soil Science Society of America.