Abstract
Evapotranspiration is considered to depend on three factors: the capillary movement of water through the unsaturated soil to the root surface, the trans-missibility of the stomata and the evaporative capacity of the atmosphere.
This is a preview of subscription content, log in via an institution to check access.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
References
Visser, W. C.: A method to determine evapotranspiration in soil monoliths. Paper read at the Colloque sur la Méthodologie de l’Ecophysiologie Végétale Montpellier, April 1962.
Visser, W. C.: Die Entwicklung der Zielsetzung und der Methoden bei Lysimeteranterraehungen. Paper read at the German-Dutch Lysimeter Colloquium, Wageningen, May 1963a.
Visser, W. C.: Moisture requirements and rate of moisture depletion of crops. Paper read at the 16th Internationale Studiedagen over Waterproblemen, Liege, May 1981, In French: Cebédeau,. Nr. 235—236, 1963 b. English versioa. Technical Bull. I.C.W. 32, 1964.
Visser, W. C.: Soil moisture content and evapotranspiration. Paper presented at the Xlllth General Assembly of the I.A.S.H., Berkeley, August 1963, Publ. 62 I.A.S.H. Comm. Evap., and Technical Bull. I.C.W. 31, 1963 c.
Author information
Authors and Affiliations
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 1965 Springer Science+Business Media Dordrecht
About this chapter
Cite this chapter
Visser, W.C. (1965). The Moisture Consumption of Plants Described as a Hydrological Phenomenon. In: SlavÃk, B. (eds) Water Stress in Plants. Springer, Dordrecht. https://doi.org/10.1007/978-94-010-3593-4_27
Download citation
DOI: https://doi.org/10.1007/978-94-010-3593-4_27
Publisher Name: Springer, Dordrecht
Print ISBN: 978-94-010-3595-8
Online ISBN: 978-94-010-3593-4
eBook Packages: Springer Book Archive