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


     


Published in Soil Sci Soc Am J 41:713-717 (1977)
© 1977 Soil Science Society of America
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 Russo, D.
Right arrow Articles by Bresler, E.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Russo, D.
Right arrow Articles by Bresler, E.
Agricola
Right arrow Articles by Russo, D.
Right arrow Articles by Bresler, E.

Effect of Mixed Na-Ca Solutions on the Hydraulic Properties of Unsaturated Soils1

David Russo and Eshel Bresler2

ABSTRACT

The effects of mixed Na-Ca solutions on soil water diffusivity and unsaturated hydraulic conductivity were tested for a loamy soil from Gilat, Israel. Soil water diffusivity functions, D({theta}), were determined by the horizontal infiltration method. Unsaturated hydraulic conductivity functions, K({theta}), were determined both directly (by vertical infiltration for suction heads of 0–50 cm H2O) and indirectly (from diffusivity functions and soil water retention curves). Prior to determinations, soil samples were equilibrated with solutions containing a given concentration and composition of Ca and Na. The results show that D({theta}) and K({theta}) are independent of solution concentrations in a Ca-saturated system. In mixed Na-Ca systems, hydraulic conductivity and soil water diffusivity functions are highly dependent on the composition and concentration of the soil solution, in addition to their dependence on soil water content, {theta}. For any given {theta}, both K({theta}) and D({theta}) decrease as either soil solution concentration decreases or the sodium fraction in the soil solution increases. The negative effect of a combination of high Na-to-Ca ratio and low soil solution concentration on K({theta}) is directly related to the degree of water saturation of the soil. Low values of {theta} can compensate for the negative effects of high Na-to-Ca ratio and low solution concentration.


NOTES

1 Contribution from the Agricultural Research Organization. The Volcani Center, Bet Dagan, Israel. 1976 Ser. no. 221-E. This research was supported by a grant from the United States-Israel Binational Science Foundation (BSF), Jerusalem, Israel.

2 Research Assistant and Soil Physicist, Div. of Soil Physics, ARO, Bet Dagan, respectively E. Bresler is also Associate Professor of Irrigation, The Hebrew Univ. of Jerusalem, Faculty of Agriculture, Rehovot, Israel.

Received for publication September 9, 1976. Accepted for publication March 30, 1977.







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 1977 by the Soil Science Society of America.