SSSAJ Grow Your Career with SSSA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 54:131-135 (1990)
© 1990 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 HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Kuo, S.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Kuo, S.
Agricola
Right arrow Articles by Kuo, S.

Phosphate Sorption Implications on Phosphate Soil Tests and Uptake by Corn

S. Kuo*

Washington State Univ. Research and Extension Center, 7612 Pioneer Way East, Puyallup, WA 98371-4998

* Corresponding author.

ABSTRACT

Phosphate sorption greatly affects P availability in soils. This greenhouse study was conducted to determine the influence of the quantity of P added and P sorption capacity on P soil tests and P accumulation by corn (Zea mays L.). Seven soils with varying contents of amorphous Al oxide were treated with 0 to 4 mmol P kg–1, incubated for 9 wk, and planted with corn in pot culture after uniform fertilization with N and K. Corn plants were harvested 4 wk after sowing. The dry-matter yields, P concentration in the plants, as well as sodium bicarbonate extractable P (NaHCO3-P) and sodium acetate extractable P (NaOAc-P) were determined. The P-sorption capacities of the soils were closely related to their amorphous Al oxide contents, and the average affinity coefficient was close to the intrinsic equilibrium constant for the formation of neutral surface species. While increasing in proportion to the amounts of P added, the concentration of NaHCO3-P and NaOAc-P decreased as the P-sorption capacities of the soils increased. Both soil tests were a function of the fraction of P coverage on soil surfaces ({Theta}), defined as the ratio of the amount of P sorbed to the P-sorption capacity. As with the soil tests, the plant P concentration and P uptake were all highly correlated with {Theta}. The quantity of P added and P-sorption capacities of the soils affected the plant P concentration, dry-matter yield, and P uptake in the same manner as they did the soil tests. As a single measurement, {Theta} was more successful than the two soil tests in predicting P accumulation and P uptake by the plants.


NOTES

Scientific Paper no. 8901-01. Dep. of Agronomy and Soils, College of Agric. and Home Economics Research Center, Washington State Univ., Pullman, WA 99164.

Received for publication January 27, 1989.


This article has been cited by other articles:


Home page
J. Environ. Qual.Home page
E. O. Young and D. S. Ross
Phosphate Release from Seasonally Flooded Soils: A Laboratory Microcosm Study
J. Environ. Qual., January 1, 2001; 30(1): 91 - 101.
[Abstract] [Full Text]


Home page
Soil Sci.Home page
F.R. Magdoff, C. Hryshko, W.E. Jokela, R.P. Durieux, and Y. Bu
Comparison of Phosphorus Soil Test Extractants for Plant Availability and Environmental Assessment
Soil Sci. Soc. Am. J., July 1, 1999; 63(4): 999 - 1006.
[Abstract] [Full Text]




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 © 1990 by the Soil Science Society of America.