SSSAJ Journal of Natural Resources and Life Sciences Education
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Soil Science Society of America Journal 64:24-29 (2000)
© 2000 Soil Science Society of America

DIVISION S-1-SOIL PHYSICS

A New Solution for Water Storage to a Fixed Depth for Constant Flux Infiltration

Bing Cheng Sia and R.Gary Kachanoskia

a Dep. of Soil Science, Univ. of Saskatchewan, Saskatoon, SK, Canada S7H 5A8

gary.kachanoski{at}usask.ca

A quantitative description of water infiltration under constant flux boundary conditions is useful for predicting water flow and chemical transport processes occurring in surface soils. A new quasi-analytical solution for water storage to a fixed depth for constant flux infiltration is presented. The solution, based on the flux–concentration relationship, allows general forms of soil hydraulic functions to be used and provides a direct interpretation of measurements from vertically installed time domain reflectometry probes. To evaluate the solution, a constant flux infiltration experiment was conducted and the hydraulic parameters for the experimental site were determined independently. The solution predictions using the approximate flux–concentration relationship for linear soils were essentially identical to an existing analytical solution using the Broadbridge and White form of hydraulic functions and to the measurements.

Abbreviations: TDR, time domain reflectometry




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B.C. Si and R.G. Kachanoski
Estimating Soil Hydraulic Properties During Constant Flux Infiltration: Inverse Procedures
Soil Sci. Soc. Am. J., March 1, 2000; 64(2): 439 - 449.
[Abstract] [Full Text]




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