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Published online 26 May 2006
Published in Vadose Zone J 5:777-783 (2006)
DOI: 10.2136/vzj2005.0145
© 2006 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Characterization of the Specific Solid–Water Interfacial Area–Water Saturation Relationship and Its Import to Reactive Transport

K. P. Saripalli*, V. L. Freedman, B. P. McGrail and P. D. Meyer

Pacific Northwest National Lab., Richland, WA 99352

Figure 1
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  		Fig. 1. Specific solid–water interfacial area as a function of saturation (B-R stands for Eq. [22], derived based on the Brooks–Corey relationship).

 

Figure 2
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  		Fig. 2. Final concentration distributions after 10 d for the quartz dissolution column for both the variable solid–water interfacial area (asw) and baseline simulations. Sat refers to the degree of water saturation. (On the y axis, distance = 0 corresponds to column inlet).

 

Figure 3
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  		Fig. 3. Final dissolution rates after 10 d for the quartz dissolution column for both the variable solid–water interfacial area (asw) and baseline simulations. More highly negative numbers indicate faster rates of dissolution. Sat refers to the degree of water saturation. (On the y axis, distance = 0 corresponds to column inlet).

 




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