Molecular fractionation of a soil fulvic acid (FA) and competitive sorption of trace metals (Cu, Zn, Cd, Pb) in hematite-solution systems: effect of the FA-to-mineral ratio

5 years ago

Molecular fractionation of a soil fulvic acid (FA) and competitive sorption of trace metals (Cu, Zn, Cd, Pb) in hematite-solution systems: effect of the FA-to-mineral ratio

$Molecular fractionation of a soil fulvic acid (FA) and competitive sorption of trace metals (Cu, Zn, Cd, Pb) in hematite-solution systems: effect of the FA-to-mineral ratio$

Remi Barillon, Mirella Del Nero, Guillaume Fleury

Understanding of the interactions occurring between fulvic acids (FAs) and trace metals in mineral-solution systems is a major issue for cycles of organic matter and micro-pollutants in surface media.

Publisher URL: http://feeds.rsc.org/~r/rss/ra/~3/WuNMnR6Qapc/C7RA06838G

DOI: 2017/RA/C7RA06838G

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