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 September 1972
Published in Agron J 64:588-591 (1972)
© 1972 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 Giskin, M.
Right arrow Articles by Kafkafi, U.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Giskin, M.
Right arrow Articles by Kafkafi, U.
Agricola
Right arrow Articles by Giskin, M.
Right arrow Articles by Kafkafi, U.

Crop Response to Phosphate Fertilization and to Residual Phosphate Levels: I. Field Experiments1

M. Giskin2, J. Hagin3 and U. Kafkafi4

Intensive phosphate fertilization practices over the last two decades have resulted in large quantities of phosphates accumulating in soils. The objective of two field experiments was to evaluate yield response to various levels of residual phosphorus.

The experiments were carried out within an irrigated rotation having two crops per year. The initial experimental treatments consisted of four rates of superphosphate equivalent to O, 48, 144, and 432 kg P/ha, applied prior to each of three crops. Following the harvest of the third crop the original plots were quartered and six additional crops were grown on each of the two soils. Superphosphate was added before the seeding of each crop in amounts equal to O, 13, 26, and 52 kg P/ha.

Out of the 18 crops harvested, there were only four yield responses to P fertilization significant at either the 0.05 or 0.01 level. The high initial residual P level (10-11 ppm NaHCO3-soluble P) and the low P fixing power of the soils (68 and 75% of the added P remained exchangeable) could explain the low frequency of response to phosphate fertilization. It was only after five to six successive crops were grown, that the bicarbonate-soluble P in the control plots dropped below 8 ppm. In these cases plant response to residual P was found. Accepted agronomic fertilizer rates (13 to 52 kg P/ha) applied to crops 4 to 9 were capable of maintaining soil residual P levels between 6.3 and 17.5 ppm P (NaHCO3-soluble). At residual P levels of 26.2 to 97.5 ppm P (NaHCO3-soluble) similar fertilizer rates were not capable of maintaining or recharging the soil "phosphate pool" which had been achieved by the heavy fertilizations (48 to 432 kg P/ha) applied to crops 1 to 3.

Key Words: Phosphate availability


1 This research was sponsored by the USDA in the PL-480 program Project No: A10 - SWC - 22 Grant No: FG-Is-208.

2 Technion-Israel Institute of Technology (present address: Volcani Institute of Agricultural Research, Neve Yaar, Israel).

3 Technion-Israel Institute of Technology, Haifa, Israel.

4 Volcani Institute of Agricultural Research, Beth Dagan, Israel.

Received for publication September 21, 1971.





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 © 1972 by the American Society of Agronomy.