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 71:936-941 (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 Google Scholar
Google Scholar
Right arrow Articles by Acharya, C. L.
Right arrow Articles by Abrol, I. P.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Acharya, C. L.
Right arrow Articles by Abrol, I. P.
Agricola
Right arrow Articles by Acharya, C. L.
Right arrow Articles by Abrol, I. P.

Effect of Exchangeable Sodium on the Rate and Pattern of Water Uptake by Raya (Brassica juncea L.) in the Field1

C. L. Acharya, S. S. Sandhu and I. P. Abrol2

Sodium can adversely affect crop growth, and the mechanism by which roots obtain water in sodic soils needs further study. Effect of exchangeable Na (ES) on the rate and pattern of water withdrawal by roots of irrigated raya (Brassica juncea L.) was studied in aquic Natrustalfs soils in a field experiment. Root water extraction was measured by monitoring the change in water content and the flux divergence with time in the soil profile. Flux divergence was calculated from the knowledge of the hydraulic conductivity vs. water content relations established in the field for different percent of ES soils and the hydraulic gradients obtained in situ during crop growth. Both the rate (R,) and pattern of water withdrawal from the soil profile by the roots were significantly affected by the amount of Na in the surface and subsurface layers. The R, measured in soil having ES of 38% in the 0 to 15 an layer was 0.141 cm 14C-sucrose compared to 0.233 an day–1 in soil with ES of 4y0. In high ES soil 78y0 of R, came from the 0 to 15 an layer and the layers below 30 cm did not show any change in water content. In low ES soil 0 to 15 and 15 to 30 cm layers contributed about 77% of the total R, and water extraction by the roots was apparent to the 60 an depth.

Key Words: Exchangeable Na • Hydraulic conductivity • Hydraulic gradients • Root water extraction • Sodic soil


1 Contribution from the Central Soil Salinity Research Institute, Karnal 132001 (Haryana), India.

2 Scientist S-1, S and Head, Division of Soils and Agronomy, respectively.

Received for publication October 16, 1978.





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.