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
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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.
1967 ◽
Vol 47
(3)
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pp. 245-250
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1967 ◽
Vol 47
(2)
◽
pp. 111-116
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1969 ◽
Vol 49
(1)
◽
pp. 151-158
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2009 ◽
Vol 66
(3)
◽
pp. 353-360
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