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Phosphorus saturation and pH differentially regulate the efficiency of organic acid anion-mediated P solubilization mechanisms in soil
Journal article   Peer reviewed

Phosphorus saturation and pH differentially regulate the efficiency of organic acid anion-mediated P solubilization mechanisms in soil

Eva Oburger, David L. Jones and Walter W. Wenzel
Plant and soil, Vol.341(1-2), pp.363-382
2011

Abstract

Agriculture Agronomy Life Sciences & Biomedicine Plant Sciences Science & Technology Soil Science
Exudation of organic acid anions by plants as well as root-induced changes in rhizosphere pH can potentially improve phosphate (P-i) availability in the rhizosphere and are frequently found to occur simultaneously. In non-calcareous soils, a major proportion of P-i is strongly sorbed to metal oxi(hydr)oxides of mainly iron (Fe) and aluminium (Al) and organic anions are known to compete with P-i for the same sorption sites (ligand exchange) or solubilize P-i via ligand-promoted mineral dissolution. Root-induced co-acidification may also further promote P-i release from soil. The relative efficiency of these different solubilization mechanisms, however, is poorly understood. The aims of this study were to gain a better mechanistic understanding of the solubilizing mechanisms of four carboxylates (citrate, malate, oxalate, malonate) in five soils with high and low P surface site saturation. Results indicate that at a lower P saturation of solid phase sorption sites, ligand-promoted mineral dissolution was the main P-i solubilization mechanism, while ligand exchange became more important at higher soil P concentrations. Co-acidification generally increased P-i solubility in the presence of carboxylates; however the relative solubilizing effect of carboxylates compared to the background electrolyte (KCl) control decreased by 20-50%. In soils with high amounts of exchangeable calcium (Ca), the proton-induced Ca solubilization reduced soluble P-i, presumably due to ionic-strength-driven changes in the electric surface potential favoring a higher P-i retention. Across a wider soil pH range (pH 3-8), P-i solubility increased with increasing alkalinity, as a result of both, more negatively charged sorption sites, as well as DOC-driven changes in Fe and Al solubility, which were further enhanced by the presence of citrate. Overall, the relative efficiency of carboxylates in solubilizing P-i was greatest in soils with medium to high amounts of anionic binding sites (mainly Fe- and Al-oxy(hydr)oxides) and a medium P sorption site coverage, with citrate being most effective in solubilizing P-i.

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Collaboration types
Domestic collaboration
International collaboration
Citation topics
3 Agriculture, Environment & Ecology
3.45 Soil Science
3.45.473 Soil Phosphorus Dynamics
Web Of Science research areas
Agronomy
Plant Sciences
Soil Science
ESI research areas
Agricultural Sciences
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