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 46:583-588 (1982)
© 1982 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 Adepoju, A. Y.
Right arrow Articles by Mattigod, S. V.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Adepoju, A. Y.
Right arrow Articles by Mattigod, S. V.
Agricola
Right arrow Articles by Adepoju, A. Y.
Right arrow Articles by Mattigod, S. V.

Availability and Extractability of Phosphorus from Soils Having High Residual Phosphorus1

A. Y. Adepoju, P. F. Pratt and S. V. Mattigod2

ABSTRACT

Surface soil materials from the 0- to 15-cm depth of 12 sites were cropped in the greenhouse to determine quantities of phosphorus (P) removed in harvested forage and to correlate chemical soil tests with P removal by crops. Soil samples taken before and after cropping were analyzed for P extracted by NaHCO3 and by an anion-exchange resin (AER). Quantities of P extracted by NaHCO3 and by AER before cropping were significantly correlated with total P removed by cropping, with the NaHCO3-extracted P producing the higher correlation coefficients. However, in terms of relationships of P removed by cropping with extractable P, the soils separated into two groups. The first group, characterized by relatively high ratios of P removal in crops to extractable P, particularly for soil samples taken after cropping, tended to have relatively high pH, high soluble Ca, and clayey textures. The second group, having lower ratios of P removal to extractable P, tended to have neutral pH values and relatively low soluble Ca and sandy textures. The data suggest that the estimation of quantities of available P from soil analysis might be highly dependent on soil characteristics and the nature of the P compounds that have accumulated.


NOTES

1 Contribution from the Dep. of Soil and Environmental Sciences, University of California, Riverside, CA 92521. The financial support of the National Fertilizer Development Center, Tennessee Valley Authority, is hereby gratefully acknowledged.

2 Former Graduate Student, Professor, and Assistant Professor of Soil Science, respectively. The Senior Author is now Senior Research Officer, Soil Science Section, National Cereals Research Institute, Ibadan, Nigeria.

Received for publication October 13, 1981. Accepted for publication February 1, 1982.







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
and Life Sciences Education
Journal of
Environmental Quality
Copyright © 1982 by the Soil Science Society of America.