Improved apparatus for measuring hydraulic conductivity at low water content

Soil Science Society of America Journal
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Abstract

A modification of the steady-state centrifuge method (SSCM) for unsaturated hydraulic conductivity (K) measurement improves the range and adjustability of this method. The modified apparatus allows mechanical adjustments to vary the measured K by a factor of 360. In addition, the use of different flow-regulating ceramic materials can give a total K range covering about six orders of magnitude. The increment of K adjustment is a factor of about 1.6. This makes it potentially useful for measuring targeted values of K or, through a trial and error procedure, of water content (θ). The range extension afforded by this modification has led to the lowest steady-state K measurement to date: 1.1 × 10−11 m/s at θ of 0.068 m3water/m3 for a sandy soil of the Delhi series (mixed, thermic Typic Xeropsamment).

Suggested Citation

Nimmo, J., Akstin, K., Mello, K., 1992, Improved apparatus for measuring hydraulic conductivity at low water content: Soil Science Society of America Journal, v. 56, no. 6, p. 1758-1761, https://doi.org/10.2136/sssaj1992.03615995005600060017x.

Publication type Article
Publication Subtype Journal Article
Title Improved apparatus for measuring hydraulic conductivity at low water content
Series title Soil Science Society of America Journal
DOI 10.2136/sssaj1992.03615995005600060017x
Volume 56
Issue 6
Year Published 1992
Language English
Publisher ACSESS
Contributing office(s) Toxic Substances Hydrology Program
Description 4 p.
First page 1758
Last page 1761
Additional publication details