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


     


Published online 6 January 2006
Published in Soil Sci Soc Am J 70:222-234 (2006)
DOI: 10.2136/sssaj2005.0012
© 2006 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Figures Only
Right arrow Full Text Free
Right arrow Full Text (PDF) Free
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 Similar articles in ISI Web of Science
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 ISI Web of Science (6)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Johnson, S. E.
Right arrow Articles by Loeppert, R. H.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Johnson, S. E.
Right arrow Articles by Loeppert, R. H.
Agricola
Right arrow Articles by Johnson, S. E.
Right arrow Articles by Loeppert, R. H.
Related Collections
Right arrow Plant and Soil Interactions
Right arrow Soil Surface Chemistry
Right arrow Plant Nutrition

Soil Chemistry

Role of Organic Acids in Phosphate Mobilization from Iron Oxide

Sarah E. Johnson* and Richard H. Loeppert

Soil & Crop Sciences Dep., 2474-TAMU, Texas A&M University, College Station, TX 77843-2474

* Corresponding author (sarah.johnson{at}cgiar.org)

Phosphate deficiency often limits crop production in acid tropical soils because of the strong bonding of phosphate by Fe and Al oxides. Organic-acid exudation from roots is one reported plant adaptation to P deficiency. The objective of this study was to predict the efficacy of this P-deficiency stress response in different soil types by investigating the mechanism of organic-acid-induced P mobilization from different oxide minerals. Greater proportions of Fe and initially adsorbed P were released from ferrihydrite when compared with goethite. More P was released and Fe dissolved at pH 4.0 than pH 5.5 or 7.0 from both oxides. For ferrihydrite, the order of effectiveness of the organic ligands for P release at pH 4 was citrate (19% of the total initially adsorbed P) > malate (14%) > tartrate (5%)>> oxalate = malonate = succinate (0.3–1.2%). For Fe release at pH 4, the order was oxalate (18% of total oxide suspension Fe dissolved) {approx} citrate (17%) > malonate (13%) > malate (8%) > tartrate (5%) >> succinate (0.02%). Faster phosphate readsorption in the case of oxalate than citrate probably accounted for the low apparent release of P by oxalate in spite of its greater Fe dissolution. At the smaller adsorbed-P concentration (1/4 of the adsorption maximum), the predominant mechanism of organic-acid induced P release was ligand-enhanced dissolution of the Fe oxide rather than ligand exchange. At 3/4 of the adsorption maximum, ligand exchange contributed to a greater extent to P release. Under low P-fertility conditions, organic-acid exudation would be more effective at increasing P availability in soils dominated by poorly crystalline than well-crystalline Fe oxides.




This article has been cited by other articles:


Home page
Soil Sci.Home page
Y. Wang, Y. He, H. Zhang, J. Schroder, C. Li, and D. Zhou
Phosphate Mobilization by Citric, Tartaric, and Oxalic Acids in a Clay Loam Ultisol
Soil Sci. Soc. Am. J., September 1, 2008; 72(5): 1263 - 1268.
[Abstract] [Full Text] [PDF]




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 © 2006 by the Soil Science Society of America.