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Osmotically Driven Water Vapor Transport in Unsaturated Soils

Shaun F. Kelly* and John S. Selker

Department of Bioresource Engineering, Gilmore Hall, Oregon State Univ., Corvallis, OR 97331



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  		Fig. 1. Gravimetric water content distributions for (a) KCl and (b) Na2CO3 in medium sand from the broken column data of Wheeting (1925).

 


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  		Fig. 2. Gravimetric water content distributions for (a) KCl and (b) Na2CO3 in clay loam from the broken column data of Wheeting (1925).

 


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  		Fig. 3. Observed and predicted cumulative water vapor transport across a 12.7-mm air gap from a salt-free section to the saline section of the broken column for (a) KCl and (b) Na2CO3 in medium sand.

 


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  		Fig. 4. Observed and predicted cumulative water vapor transport across a 12.7-mm air gap from a salt-free section to the saline section of the broken column for (a) KCl and (b) Na2CO3 in clay loam.

 


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  		Fig. 5. Water vapor density of salt solutions at 25°C calculated using Eq. [21].

 


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  		Fig. 6. Predicted cumulative water vapor transport across a 12.7-mm air gap from salt-free section to saline section of a broken column in a medium sand.

 




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