Composition and metal ion complexation behavour of humic fractions derived from corn tissue

• Published in: Plant and soil Vol. 229; no. 1; pp. 13 - 24
• Main Authors: Evangelou, V. P., Marsi, M.
• Format: Journal Article
• Language: English
• Published: Dordrecht Kluwer Academic Publishers 01-02-2001; Springer; Springer Nature B.V
• Subjects: Acid soils; Acidity; Agronomy. Soil science and plant productions; Applied sciences; Bioavailability; Biological and medical sciences; Biological and physicochemical properties of pollutants. Interaction in the soil; Cadmium; Chemical, physicochemical, biochemical and biological properties; Clay soils; Corn; Decomposition; Exact sciences and technology; Forest soils; Functional groups; Fundamental and applied biological sciences. Psychology; Heavy metals; Inflection points; Metal concentrations; Metal ions; Organic matter; Organic soils; Phenols; Physics, chemistry, biochemistry and biology of agricultural and forest soils; Pollution; Sedimentary soils; Soil and sediments pollution; Soil and water pollution; Soil biochemistry; Soil management; Soil science; Plant tissue; Soil chemistry; Monocotyledones; Fractionation; Zea mays; Organomineral complex; Metal ion; Cereal crop; Humus; Gramineae; Angiospermae; Plant origin; Spermatophyta; Chemical composition
• ISSN: 0032-079X; 1573-5036
• DOI: 10.1023/A:1004862100925

Decomposition of fresh plant residues produces humic fractions with different molecular size and composition. It was hypothesized that the functional group-type and content of humic fractions depended on molecular size, which was expected to influence heavy-metal complexation behavior. In this study, corn (Zea mays L.) stalks and leaves were collected from the field and decomposed for an 8-month period to produce humic substances which were separated into three water soluble fractions, HF1, HF2 and HF3, from highest to lowest relative molecular size. Functional group determination showed that total, carboxylic and phenolic OH acidity increased as relative molecular size of humic fractions decreased. Furthermore, C/O ratios decreased, whereas N/C and H/C ratios remained relatively unaffected as relative molecular size of humic fractions decreased. Formation of Ca²⁺, Cd²⁺ and Cu²⁺ -humic fraction complexes and how these complexes were affected by pH and relative (humic fraction) molecular size were studied using potentiometric titration. Metal-humic complexes exhibited at least two types of sites with respect to Ca²⁺, Cd²⁺ and Cu²⁺ complexation. Relative molecular size had a large significant influence on total metal-ion complexation, but it had a relatively small influence on complex stability at low levels of metal-ion complexation. Strength of metal-ion humic complexes followed the order Cu²⁺ > Cd²⁺ > Ca²⁺ and was affected by pH, especially for low affinity sites. Carboxylic and phenolic OH groups were most likely involved in complex formation. Magnitude of the metal-humic formation constants at the lowest equilibrium metal-ion concentration, under the various pH values tested, varied from 5.39 to 5.90 for Ca²⁺, from 5.36 to 6.01 for Cd²⁺ and from 6.93 to 7.71 for Cu²⁺. Furthermore, the formation constants appeared to be positively influenced by decreasing molecular size of water-soluble humic fraction, and increasing pH. These results inferred that soil management practices causing build-up of humic substances would affect mobility and bioavailability of metal-ions.