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ABSTRACT
A study about the competition between organic anions (oxalate and malate)—currently present in the rhizosphere and phosphate for adsorption sites in tropical soils—indicate that in the presence of organic anions, phosphate adsorption by soils is reduced. The extent of such reduction is dependent on the way in which either phosphate or the organic anion are added to the soil. The organic oxyanions studied are more rapidly adsorbed to the soil surface than the phosphate; consequently those anions, when existing in the rhizosphere, can improve the phosphate status of soil.
1 Contribution from the Laboratorio de Estudios Ambientales IZT, Facultad de Ciencias UCV. This work was supported by CONICIT Proyecto 0460 and CDCH.
2 Professor and Soil Scientist. Laboratorio de Estudios Ambientales IZT, Fac. de Ciencias Caracas UCV., Instructor Fac. Ingenieria UCV and Quimico INTEVEP Los Teques, respectively.
Received for publication August 12, 1985.
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