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Metal Binding in Estuarine Humic and Fulvic Acids: FTIR Analysis of Humic Acid-Metal Complexes
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1998
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Fulvic AcidsEngineeringGreen ChemistryMarine ChemistryHumic Acid-metal ComplexesChemistryOrganic GeochemistryEnvironmental ChemistryEnvironmental GeochemistryCopper Binding CapacitiesAnalytical ChemistrySoutheastern United StatesInorganic ChemistryFtir AnalysisMetal BindingBiochemistryChemical FormTrace MetalNatural SciencesBioactive MetalSoil ChemistryGeochemistry
Humic and fulvic acids isolated from salt marsh estuaries of the southeastern United States had copper binding capacities (CuBC) of 0.16 to 0.26 µg atm Cu2+ mg−1 humic acid and 0.17 to 0.24 µg atm Cu2+ mg−1 fulvic acid. Competitive reactions of humic substances with alkaline earth elements Ca2+ and Mg2+ reduced the CuBC by only 11% for fulvic acids and by 17% for humic acids. Competition with the trivalent metal ions Al3+ and Fe3+ reduced the CuBC in humic substances by 30–40%. Fourier transform infrared (FTIR) spectral analyses of the humic-metal complexes suggest that Cu(II) may be bound preferentially by oxygen-containing functional groups in estuarine fulvic acids, but there is a much higher involvement of nitrogen-containing functional groups in binding Cu(II) to estuarine humic acids. FTIR spectra were also collected for humic acid-metal complexes of Ag, Au, Hg, Mn and Pb.