Diffuse flux of cationic micronutrients in two Oxisols as affected by low-molecular-weight organic acids and cover-crop residue

Weinheim

Wiley VCH Verlag

2005

S. 334-340

2 Abb., 44 Lit. Ang.

Artikel aus einer ZeitschriftUnselbständiges Werk

200124733

Journal of Plant Nutrition and Soil Science 2005, 168(3), S. 334-340

Low-mulecular-weigth organic acids with one or more carboxylic groups are ubiquitous. In soils, they can originate from leaching of plants, litter decomposition, plant-roots exudation, and microbial activity. Their presence in the soil may favor the formation of soluble organo-metallic complexes that improve the transport of Zn, Cu, Fe, and Mn to plant-root surfaces via diffusion. The current study sought to determine if some of the organic acids (OA) in soils and a cover-crop residue influence the diffusive flux (DF) of Zn, Cu, Mn, and Fe. Two OA were added to two Oxisols (Typic Haplustox): a clayey Dark Red Latosol (DRL) and a sandy-loam Red Yellow Latosol (RYL). Acetic and citric acid were added to achieve concentrations of 0, 250, 500, 1000, and 2000 mmol (mß soil)-1. The effect of adding plant material (pearl millet) on the soil DF of the cationic micronutrients was also determined. Soil diffusive flux was evaluated by incubating positively charged and negatively charged exchange-resin membranes with the soil PVC diffusion chambers for 15 d. Desorption of Zn, Cu, Fe, Mn, and OA from the resins was performed with 0.5 mil I-1 HCI. The results demonstrated that the DF of the cationic micronutrients increased with the addition of organic acid. The DF of Zn and Mn occurred mostly towards the cationic resin, whereas the diffusive flux of Cu and Fe occurred mostly towards the anionic resin. Apparently, the dissolution of oxides and/or complexation of micronutrients adsorbed to the solid phase or in the soil solution contributed to the obtained results. Citric acid was more efficient than acetic acid in maintaining a larger DF value for Zn, Cu, and Fe. The addition of millet plant material to the soil increased the DF in the following order: Mn > Cu > Fe > Zn; Mn moved towards the cationic resin, and the other micronutrients moved towards the anionic resin. These findings suggest that organic compounds play an important role in the short-distance transport of cationic micronutrients in highly weathered soils.