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Using TDR to Estimate Hydraulic Conductivity and Air Entry in Growing Media and Sand
Author(s) -
Caron Jean,
Rivière Louis-Marie,
Charpentier Sylvain,
Renault Pierre,
Michel Jean-Charles
Publication year - 2002
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj2002.3730
Subject(s) - hydraulic conductivity , saturation (graph theory) , infiltration (hvac) , thermal diffusivity , porous medium , soil science , environmental science , porosity , materials science , geology , geotechnical engineering , mathematics , soil water , composite material , physics , thermodynamics , combinatorics
Gas relative diffusivity measurements are key indicators of the quality of growing media. Previous studies have shown that this property can be estimated indirectly from measurements of the point of air entry (ψ a ), air‐filled porosity (θ a ), and saturated hydraulic conductivity ( K s ). Different tools are required to measure these parameters and this paper investigates how a single tool, time domain reflectrometry (TDR), already used to determine θ a from measurements of volumetric water content (θ), could be utilized to measure ψ a and K s in growing media. Cylinders were filled with 13 different substrates and coarse sand. A transient‐state technique (vertical infiltration at −1 hPa of water potential) was used to calculate K s from θ measurements in time. In growing media, calculated K s values from transient‐state experiment were statistically equal to estimates obtained from steady‐state measurements at a potential of −1hPa. However, both methods underestimated the K s values obtained under steady‐state conditions after a pulse of water had been applied or after prolonged wetting. For sand, TDR‐based measurements and steady‐state infiltration at −1 hPa, provided estimates of K s equal to those obtained after prolonged saturation. To estimate ψ a , TDR probes in a horizontal and a vertical position were tested in addition to a pressure transducer technique. For growing media, the horizontal positioning of the probes provided more consistent estimates of ψ a than the other two techniques. Estimates of ψ a with TDR in sand, both in vertical and horizontal position, were similar.