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ABSTRACT
A theoretical analysis shows that by imposing certain boundary conditions it should be possible to eliminate the major effects of temperature fluctuation on psychrometric measurements of soil water potential. Tests on a psychrometer constructed to meet these boundary conditions were carried out on a soil column in a greenhouse. Although diurnal fluctuation of soil temperature was as great as 5C, water potential was measured with an apparent accuracy of ±0.5 bars throughout two irrigation cycles.
1 Contribution from the US Salinity Laboratory, Soil and Water Conserv. Res. Div., ARS, USDA, Riverside, Calif. 92502. This work was supported in part by the Atmospheric Sciences Laboratory, Res. Div., US Army Electronics Command, Fort Huachuca, Ariz.
2 Research Soil Scientist and Physicist, respectively.
Received for publication October 18, 1966. Accepted for publication November 30, 1966.
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