Transpiration as a Function of Soil Temperature and Soil Water Stress
- 1 April 1967
- journal article
- research article
- Published by Oxford University Press (OUP) in Plant Physiology
- Vol. 42 (4) , 550-556
- https://doi.org/10.1104/pp.42.4.550
Abstract
An apparatus was developed for the measurement of transpiration rates of Trifolium repens. The transpiration rates were measured under controlled conditions of soil water stress and soil temperature. Other environmental parameters such as air temperature, relative humidity, light intensity and air speed were held constant. Diffusive resistances were calculated and stomatal aperture changes were recorded for all treatment combinations. A significant interaction between soil water stress and soil temperature was observed for stomatal closures. Stomatal closure was observed even in the so-called wet range of soil water stress. An increase in mesophyll resistance or incipient drying was observed for several treatment combinations. The mesophyll resistance was shown to increase as soil water stress increased.This publication has 4 references indexed in Scilit:
- Energy, Plants, and EcologyEcology, 1965
- Leaf temperatures in controlled environmentsPlanta, 1964
- A Re-Examination of the Relative Turgidity Technique for Estimating Water Deficits in LeavesAustralian Journal of Biological Sciences, 1962
- BIOCHEMICAL CONTROL OF STOMATAL OPENING IN LEAVESProceedings of the National Academy of Sciences, 1961