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Copper complexing properties of melanoidins and marine humic material (CROSBI ID 114619)

Prilog u časopisu | izvorni znanstveni rad | međunarodna recenzija

Plavšić, Marta ; Ćosović, Božena ; Cindy, Lee Copper complexing properties of melanoidins and marine humic material // Science of the total environment, 366 (2006), 1; 310-319. doi: 10.1016/j.scitotenv.2005.07.011

Podaci o odgovornosti

Plavšić, Marta ; Ćosović, Božena ; Cindy, Lee

engleski

Copper complexing properties of melanoidins and marine humic material

Melanoidins, condensation products of sugars and amino acids, represent a key link in the transformation of polysaccharides to humic material in the marine environment. We investigated the complexing capacity of melanoidins that were prepared in deionized water and seawater and separated into different molecular mass fractions. The copper complexing properties of humic material isolated from marine lagoon sediments were determined for comparison. Melanoidins prepared using condensation times longer than two days exibit complexation properties towards copper ions that appear to depend on the basicity of the amino acid precursor and the molecular mass of the product. Pseudomelanoidins, prepared from glucose only, do not complex copper ions at all, regardless of the molecular mass. The highest copper complexing capacity value among melanoidins was measured for a glucose-lysine melanoidin with molecular mass fraction >10 kD (L T= 2.1x10-7 molCu2+ /L). Melanoidin prepared from glucose and glutamic acid >10 kD was similar in complexing capacity to fulvic acid (1-20kD molecular mass) isolated from lagoon sediments. The presence of calcium and magnesium ions and other macro and microconstituents in the seawater used to prepare melanoidins influences its complexing properties towards metal ions.

humic matter; copper ions; complexation; electrochemistryhumic matter; copper ions; complexation; electrochemistryhumic matter; copper ions; complexation; electrochemistry

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Podaci o izdanju

366 (1)

2006.

310-319

objavljeno

0048-9697

1879-1026

10.1016/j.scitotenv.2005.07.011

Povezanost rada

Geologija

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