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479297 
Journal Article 
Oxidation and incorporation of hydrogen sulfide by dissolved organic matter 
Heitmann, T; Blodau, C 
2006 
Yes 
Chemical Geology
ISSN: 0009-2541 
235 
1-2 
12-20 
English 
Redox reactions of sulfide with dissolved organic matter (DOM) are potentially important for sulfur cycling in anoxic environments. We investigated the chemical oxidation of H2S With a peat humic acid in batch experiments at pH 6, quantified the electron accepting capacity (EAC), and applied a first order kinetic model to estimate reaction constants. Dissolved ferric iron was used to quantify electron donating capacities (EDC). Hydrogen sulfide was oxidized to thiosulfate and also incorporated into DOM. Fourier-transformed infi-ared (FTIR) spectroscopy suggested formation of aryl polysulfide. Electron transfer was significantly correlated to DOM concentration and amounted to 0.60 (EAC) and 0.63 (EDC) meq g(-1) C. DOM concentrations > 60 mgl(-1) lead to decreased capacities per unit mass carbon. The overall reaction of sulfide with DOM could be adequately described by a kinetic model comprising a redox-active and an Sincorporating DOM pool. The overall reaction was fast, with H2S half-lives on the order of several hours. The results suggest that DOM may chemically reoxidize H2S in organic rich soils and sediments at significant rates. (c) 2006 Elsevier B.V. All rights reserved. 
sulfide oxidation; DOM; humic acids; thinsulfate; fresh-water sediments; humic substances; iron(iii) reduction; electron-acceptors; aqueous-solution; natural-waters; sulfur; iron; kinetics; quinone