Abstract
Copper mobility and bioavailability in soil are determined mainly by adsorption on the surface of soil particles (McLaren and Crawford, 1973; McBride, 1981, 1989). Sorption behavior of metals is dependent on interaction with various components of soil solution, especially chelating agents such as fulvic acid, aminoacids, organic acids, and phenolic compounds. Organic ligands are formed in soil during the decomposition of organic matter, root exudation, and microbial synthesis by rhizosphere microorganisms (McKeague et al., 1986; Tan, 1986; Stevenson and Ardakani, 1972; McBride, 1989; Karpukhin et al., 1993). Hodgson et al. (1965) found that as much as 99% of soluble Cu may exist in a complexed form in soil solutions from several mineral soils. Ponomareva (1972), Yashin and Kaurichev (1992) demonstrated an important specific role of water-soluble organic ligands for mobilization and migration of metals in soils and the landscape.
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Pampura, T., Ustinin, M. (1999). Effect of Succinic Acid Produced by Microorganisms and Plant Roots on Copper Sorption by Soil. In: Berthelin, J., Huang, P.M., Bollag, JM., Andreux, F. (eds) Effect of Mineral-Organic-Microorganism Interactions on Soil and Freshwater Environments. Springer, Boston, MA. https://doi.org/10.1007/978-1-4615-4683-2_6
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DOI: https://doi.org/10.1007/978-1-4615-4683-2_6
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