Labile/inert metal species in aquatic humic substances: an ion-exchange study

An ion-exchange procedure has been developed for the analytical fractionation of metals (e.g. Al, Co, Cu, Fe, Mn, Ni, Pb, Zn) forming labile/inert complexes with aquatic humic substances (HS) isolated (XAD 2, XAD 8, ultrafiltration) from bog, forest, ground and lake water. Using 1-(2-hydroxyphenylazo)-2-naphthol groups immobilized on cellulose (Cellulose HYPHAN™) as chelating collector (batch and column procedure, resp.) for reactive metal fractions in dissolved HS, the kinetics and the degree of separation (referred to the total metal content) serve for the operational characterization of the metal lability. According to the separation kinetics (96 h), mostly the reactivity order Mn>Zn>Co>Pb>Ni>Cu≫Al>Fe is observed for the above metals in HS, resulting in recoveries of >98% for Mn and Zn, but strongly varying for the other metals (e.g., 44–95% Cu, 18–84% Fe). By means of cellulose HYPHAN four metal fractions (e.g. Cu) can be distinguished kinetically: (a) about 50% of Cu freshly complexed with HS are directly exchanged (2nd order kinetics, k=0.275 1 · mol−1 · s−1) followed by (b) a less labile fraction (20–30%) of 1st to 2nd order exchange; (c) a hardly reactive fraction (5–10%) revealing uniform half times t1/2 of 25 h closes the Cu exchange from HS. Moreover the Cu fraction (d), being exchange-inert in HS, amounts to 5–10% and increases by slow transformation processes of the formed HS/Cu species.