Agronomy Journal Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published online 1 November 1979
Published in Agron J 71:1056-1060 (1979)
© 1979 American Society of Agronomy
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Wallender, W. W.
Right arrow Articles by Stromberg, L. K.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Wallender, W. W.
Right arrow Articles by Stromberg, L. K.
Agricola
Right arrow Articles by Wallender, W. W.
Right arrow Articles by Stromberg, L. K.

Estimating the Contribution of a Perched Water Table to the Seasonal Evapotranspiration of Cotton1

W. W. Wallender, D. W. Grimes, D. W. Henderson and L. K. Stromberg2

Water supplied to a growing crop by capillary rise from a shallow water table can be an important resource. Several thousand hectares in the western San Joaquin Valley in California have a perched water table created by irrigation and a slowly permeable subsurface zone. When irrigations are made according to a schedule that is optimum for soils without a shallow water table, cotton (Gossypium hirsutum L.) frequently shows plantgrowth that is characteristic of excessive irrigation. Field studies were conducted to evaluate the contribution of a perched water table to the evapotranspiration (ET) demand of cotton and to develop an irrigation schedule that uses the resource effectively.

Two independent procedures were used to estimate the water table contribution (WT) through capillary rise. A water budget method used a previously developed yield-ET function to estimate ET from observed production levels. Soil moisture depletion (SMD), stored irrigation water (IW), and deep percolation (PW) were determined from neutron thermalization measurements on volumetric soil water content. WT was determined by rearranging the relation ET = SMD + IW – PW + WT. A second approach, associated the chloride in the water table (17.4 meq/l) with increased chloride concentrations in the soil above the water table. The equivalent water depth necessary to effect this change was calculated. Both procedures estimated WT to be near 36 cm for the growing season. A high standard deviation (18.7 cm) was caused, however, by considerable spatial variability for the chloride tracer method.

A revised irrigation schedule for cotton was developed that uses water, of acceptable quality, derived from a water table as a beneficial raource.

Key Words: Irrigation • Water budget analysis • Chloride tracer • Leaf water potential • Pressure chamber


1 contribution from the Department of Land, Air, and Water Resources, Univ. of California, Davis, CA 95616, and Univ. of California Cooperative Extension.

2 Formerly graduate student (now graduate student, Utah State Univ.), water scientists, and farm advisor, Fresno County, respectively.

Received for publication May 7, 1979.


This article has been cited by other articles:


Home page
Soil Sci.Home page
L. Wu, T. H. Skaggs, P. J. Shouse, and J. E. Ayars
State Space Analysis of Soil Water and Salinity Regimes in a Loam Soil Underlain by Shallow Groundwater
Soil Sci. Soc. Am. J., July 1, 2001; 65(4): 1065 - 1074.
[Abstract] [Full Text] [PDF]




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 © 1979 by the American Society of Agronomy.