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Published online 1 November 1977
Published in Agron J 69:906-910 (1977)
© 1977 American Society of Agronomy
677 S. Segoe Rd., Madison, WI 53711 USA
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Plant Water Relationships of Spring Wheat as Influenced by Shelter and Soil Water1

A. B. Frank, D. G. Harris and W. O. Willis2

Field windbreaks have been planted primarily for soil erosion control; subsequently, research has shown that windbreaks have an effect on microclimate and on growth and yield of crops. Other research has shown that plant water relations respond to changes in microclimate. The present work was undertaken to determine the effect of microclimate changes induced by a slat-fence windbreak on the plant water relations of field-grown wheat (Triticum aestivum L.). Slat-fence barriers were used as windbreaks for studying effects of shelter-modified microclimte on plant water relations of ‘Waldron’ spring wheat, grown on Parshall fine sandy loam (Pachic Haploboroll), under irrigated and dryland soil water regimes. Data were collected on leaf water potential ({Psi}l), xylem water potential ({Psi}x), stomatal diffusion resistance (rs), canopy temperature (Tc), soil water potential ({Psi}s), soil water extraction, and grain yield.

Plant water status of the wheat crop was strongly affected by shelter and soil water content. The treatment combination of shelter plus irrigation produced a higher {Psi}l and lower Tc and, overall, was the most beneficial treatment in creating a favorable plant water status. The dryland treatments were under considerable water stress from early heading to maturity. The presence of the shelter did not alleviate the water stress on the dryland-grown plants. Water-use efficiency was significantly higher for the irrigated-sheltered as compared with the irrigated-exposed treatments. Water-use efficiency of the dryland treatments was lower than the irrigated treatments, but the dryland treatments did not differ from each other. The results of our study indicated that windbreaks will be most beneficial to a wheat crop only if soil water is adequate for good crop growth throughout the growing season. Because soil water varies considerably from year to year in the northern Great Plains, crop responses to windbreaks can also be expected to vary considerably.

Key Words: Leaf water potential • Stomatal diffusion resistance • Canopy temperature • Windbreaks


1 Contribution from Plant Science and Soil, Water, and Air Sciences, ARS-USDA, North Central Region, Dakotas-Alaska Area.

2 Plant physiologist and soil scientists, respectively, Northern Great Plains Research Center, Mandan, ND 58554.

Received for publication January 24, 1977.





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 © 1977 by the American Society of Agronomy.