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Published in Agron J 59:420-423 (1967)
© 1967 American Society of Agronomy
677 S. Segoe Rd., Madison, WI 53711 USA
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Available Water in Soil as Influenced by Extraction of Soil Water by Plants1

D. E. Miller2

Over a two-year period, a study was conducted to evaluate the influence of extraction of soil water by plants on the downward flow of water following irrigation and on the amount of water that may be considered as available to the plant. A conventional estimate of available water at an arbitrary time after irrigation may be increased by about 40% of the evapotranspiration that occurs between irrigation and sampling because of the influence of water extraction on downward flow. The data emphasize the lack of precision in the field capacity concept and that soil drainage following an irrigation does not usually become negligible within reasonable times after irrigation.

Key Words: field capacity • evapotranspiration • deep drainage


1 Contribution from the Soil and Water Conservation Research Division, Aqricultural Research Service, USDA, in cooperation with the College of Agriculture, Washington State University, Pullman. Scientific Paper No. 2923.

2 Research Soil Scientist, USDA, Prosser, Washington.

Received for publication March 2, 1967.





HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Crop Science Vadose Zone Journal
Journal of Natural Resources
and Life Sciences Education
Soil Science Society of America Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 1967 by the American Society of Agronomy.