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Land Resource Research Centre, Agriculture Canada, Ottawa, ON, Canada K1A 0C6
Dep. of Land Resource Science, Univ. of Guelph, Guelph, ON, Canada N1G 2W1
*Corresponding author.
ABSTRACT
A new analysis of steady, ponded infiltration from within a single ring takes soil hydraulic properties, ring radius, depth of ring insertion, and depth of ponding into account. It also provides a means for determining the field-saturated hydraulic conductivity (Kfs) and the matric flux potential (
m). The analysis employs numerically determined shape factors (G) that are found to depend significantly on ring radius (a) and depth of ring insertion (d), but only slightly on depth of ponding (H) and soil hydraulic properties. As a consequence, averaged G values (Ge) can be developed for specified d and a that apply to a wide range of ponded heads and soil types. Procedures for calculating Kfs and
m are based on G or Ge, and on the ponding of one, two, or multiple H levels in the ring. Test calculations based on Ge suggest that Kfs can be obtained with an accuracy of about ±20% for H = 0.05 to 0.25 m and
= 1 to 36 m–1, where
is the soil parameter of the exponential hydraulic conductivity-pressure head relationship. A similar level of accuracy (using Ge) is obtained for
m when
is small (
4 m–1), and when both
and H are large (
> 4 m–1, H
0.20 m). Significant errors in
m can occur, however, when
is large but H is small. Potentially important features of this single ring method include low sensitivity of the Kfs calculation to errors in Ge, reduced measurement errors resulting from small-scale soil variability, and the ability to pond large heads in order to increase flow rates in low-permeability materials.
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