H-binding of size- and polarity-fractionated soil and lignite humic acids after removal of metal and ash components

Drosos, Marios; Leenheer, J. A.; Avgeropoulos, Apostolos; Deligiannakis, Yiannis

H-binding of size- and polarity-fractionated soil and lignite humic acids after removal of metal and ash components

2014

Drosos, Marios | Leenheer, J. A. | Avgeropoulos, Apostolos | Deligiannakis, Yiannis

A fractionation technique, combining dialysis removal of metal and ash components with hydrofluoric acid and pH 10 citrate buffer followed by chromatography of dialysis permeate on XAD-8 resin at decreasing pH values, has been applied to lignite humic acid (lignite-HA) and soil humic acid (soil-HA). H-binding data and non ideal competitive adsorption-Donnan model parameters were obtained for the HA fractions by theoretical analysis of H-binding data which reveal a significant increase of the carboxyl and the phenolic charge for the lignite-HA fractions vs. the parental lignite humic acid (LPₐᵣₑₙₜₐₗHA). The fractionated lignite-HA material consisted mainly of permeate fractions, some of which were fulvic acid-like. The fractionated soil-HA material consisted mainly of large macromolecular structures that did not permeate the dialysis membrane during deashing. Chargeable groups had comparable concentrations in soil-HA fractions and parental soil humic acid (SPₐᵣₑₙₜₐₗHA), indicating minimal interference of ash components with carboxyl and phenolic (and/or enolic) groups. Fractionation of HA, combined with theoretical analysis of H-binding, can distinguish the supramolecular vs. macromolecular nature of fractions within the same parental HA.

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