Psychrometric Measurement of Soil Water Potential: Temperature and Bulk Density Effects1
- G. S. Campbell and
- Walter H. Gardner2
Changes in soil water potential with temperature were determined using thermocouple psychrometers on samples of four soils. Results indicate that change in soil water potential with temperature becomes greater as soils become drier. The finer textured soils showed a greater change in water potential with temperature than did coarser soils at similar water potentials.
Water potential change with bulk density also was determined for samples of three soils. Little change was noted except on a clay subsoil sample.
These results indicate that in most cases negligible differences will arise from measuring water potential at laboratory temperature rather than at the temperature existing in the field and from use of disturbed field samples with altered bulk density rather than undisturbed field soil. However, at water potentials below about −20 bars, temperature effects may become significant, especially in fine textured soils, and measurements on clay subsoils may be significantly affected by changes in bulk density.Please view the pdf by using the Full Text (PDF) link under 'View' to the left.
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