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Synopsis: A decrease in transpiration rate, which could not be explained on the basis of physical factors of the environment, was observed. Root impedance to water absorption and transmission was found to be approximately five times greater at the time of day when transpiration rate was greatly attenuated than at the time when transpiration was at a maximum. Transpiration rate was directly proportional to evaporative demand early in the day but later in the day when root: impedance was high, an inverse and less well denned relationship existed.
2 Instructor and Associate Professor, Department of Agronomy, Oklahoma State University, Stillwater, Okla. The senior author is presently Research Soil Scientist, USDA. Manhattan, Kansas.
Received for publication January 24, 1964.
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