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Published online 13 May 2005
Published in Vadose Zone J 4:434-441 (2005)
DOI: 10.2136/vzj2004.0126
© 2005 Soil Science Society of America
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Buckingham, 1907

An Appreciation

T. N. Narasimhan*

Materials Science and Engineering, University of California, 210 Hearst Memorial Mining Bldg., Berkeley, CA 94526-1760


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Fig. 1. Water retention curves for six different soils obtained from 48-inch columns after 53 to 68 d. Capillary potential {psi} equals elevation x times a constant A (Buckingham, 1907, Fig. 7).

 


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Fig. 2. Schematic variation of capillary conductivity {lambda} with water content {theta} (Buckingham, 1907, Fig. 14).

 


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Fig. 3. Hypothetical relation between {lambda} and {theta} for {alpha}ß = 1 and {theta}1 = 1 (Buckingham, 1907, Fig. 16).

 


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Fig. 4. Relation between electrical conductance and water content for a moist soil (Buckingham, 1907, Fig. 20).

 





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