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Published online 8 October 2007
Published in Vadose Zone J 6:687-693 (2007)
DOI: 10.2136/vzj2007.0080
© 2007 Soil Science Society of America
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Central Ideas of Buckingham (1907): A Century Later

T. N. Narasimhan*

Dep. of Materials Science and Engineering, Dep. of Environmental Science, Policy and Management, Earth Sciences Division, Lawrence Berkeley National Lab., 210 Hearst Mining Bldg., Univ. of California at Berkeley, Berkeley, CA 94720-1760

Figure 1
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FIG. 1. Distribution of water in 48-inch columns of soil after 53 to 68 d. The figure shows imbibition (distinct from drainage) curves. (Buckingham, 1907, Fig. 7, p. 32).

 

Figure 2
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FIG. 2. Schematic relation between capillary conductivity, {lambda}, and water content {theta}. (Buckingham, 1907, Fig. 14, p. 43).

 

Figure 3
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FIG. 3. Dependence of the parameter {chi} on water saturation (Bishop and Blight, 1963) (reproduced with kind permission of Geotechnique).

 





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