A Comparison of Soybean Leaf Water Potential and Leaf Temperature under Progressive Drought1

Abstract
Information is limited on the relationship between leaf water potential (Ψ) and leaf temperature (T) of soybeans [Glycine max (L.) Merr.] grown in the field. Therefore, measurements of Ψ and T were made with a pressure chamber and infrared thermometer, respectively, in five study periods during a field study in 1978. The season was characterized by progressive drought. ‘Forrest’ soybeans were grown at two moisture regimes on a Crowley silt loam (Typic Albaqualf).Linear relationships were found between T and Ψ. Leaf temperature of the nonirrigated soybeans was more sensitive to changes in Ψ than that of the irrigated soybeans and became more sensitive as the drought progressed. The regression equations relating Ψ to T in each of the five study periods were not unique for a given moisture treatment. However, the regression equations expressing the Ψ vs. T relationship for the single linear equation would suffice for describing the Ψ vs. T relationship throughout the season for each moisture treatment, but a different one would be required to express that relationship for a different moisture treatment.