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ABSTRACT
Infrared (IR) spectroscopy, between 2,000 and 1,000 cm–1, was used to identify the mode by which carboxylates of a soil humic acid (HA) complexed Cu2+ and Fe3+. Carboxylic acid groups of HA (R-COOH) were converted to carboxylates (R-COO-) by forming coordinate bonds with Cu2+ and Fe3+. The separation
of the antisymmetrical and symmetrical stretching vibrations of R-COO- was obtained from the IR spectra of the metal-HA complexes. The
values for the metal-HA complexes were significantly larger than the corresponding reference value of
for uncomplexed -COO-, demonstrating that R-COO- formed a unidentate complex (i.e., a single M-O bond) with Cu2+ and Fe3+. The formation of bidentate or bridging complexes between R-COO- of HA and Cu2+ or Fe3+ was not observed.
1 Contribution from the Purdue Agric. Exp. Stn., West Lafayette, IN 47907. Journal Paper no. 8388. This research was supported in part by Grant no. R804547030 from the U.S. Environmental Protection Agency.
2 Graduate Research Assistant, and Professors, respectively, Dep. of Agronomy, Purdue Univ., W. Lafayette, IN 47907. The Senior Author is now Assistant Professor, Dep. of Crop and Soil Sci., Michigan State Univ., East Lansing, MI 48824.
Received for publication February 20, 1981. Accepted for publication June 18, 1981.
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