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Reactivity of synthetic Fe chelates with soils and soil components
Ana Álvarez-Fernández, Miguel A. Sierra and Juan J. Lucena
Plant and Soil
Vol. 241, No. 1, 10th International Symposium on Iron Nutrition and Interactions in Plants (April (I) 2002), pp. 129-137
Published by: Springer
Stable URL: http://www.jstor.org/stable/24122550
Page Count: 9
You can always find the topics here!Topics: Chelates, Acid soils, Calcareous soils, Soil solution, pH, Peat soils, Soil composition, Agricultural soils, Soil interactions, Ferrihydrite
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The most effective and common Fe fertilisers in general are EDDHA and EDDHMA Fe chelates because they are highly stable ferric complexes in neutral and alkaline solutions. EDDHSA and EDDCHA iron chelates were introduced in the market recently. Commercial Fe chelates have two Fe fractions, chelated Fe and non-chelated Fe. The latter is bonded to by-products produced during the synthesis of the chelating agent. The effectiveness of Fe chelates depends on their ability to maintain Fe in the soil solution despite simultaneous equilibrium of Fe chelate with many cations, such as Ca2+. The main aim of this work was to test the possible agricultural use of EDDHSA and EDDCHA Fe chelates. The pH-Ca2+ effect on soluble and chelated Fe (pH ranging from 2 to 12) and the interaction of Fe chelates with soils and soil phases (ferrihydrite, acid peat, calcium carbonate and Ca montmorillonite) are presented. The results demonstrated that EDDHA, EDDHMA, EDDHSA and EDDCHA in solution remain fully associated with Fe from pH 4 to 9 despite competition with Ca. Among soil materials, ferrihydrite and acid peat retain both chelated and non-chelated Fe to the greatest extent. The type of chelating agent is a factor that affects chelated Fe availability in soil. FeEDDHA and FeEDDHMA were retained more by soil surfaces than FeEDDHSA and FeEDDCHA. Commercial Fe chelates present a large amount of soluble, non-chelated Fe and make Cu soluble in soils, which may be due to non-chelated Fe being displaced by Cu.
Plant and Soil © 2002 Springer