Formation of volatile sulfur compounds by microbial decomposition of sulfur-containing amino acids in soils

Abstract

Evolution of volatile sulfur compounds from soils treated with S-containing amino acids was studied by sensitive gas chromatographic techniques involving use of a flame photometric detector fitted with a sulfur filter. The following volatile sulfur compounds were identified as products of microbial decomposition of S-containing amino acids in soils under aerobic or waterlogged conditions: methyl mercaptan, dimethyl sulfide and dimethyl disulfide (evolved from soils treated with methionine, methionine sulfoxide, methionine sulfone or S-methyl cysteine); ethyl mercaptan, ethyl methyl sulfide and diethyl disulfide (evolved from soils treated with ethionine or S-ethyl cysteine); and carbon disulfide (evolved from soils treated with cystine, cysteine, lanthionine or djenkolic acid). Small amounts of dimethyl sulfide and carbon disulfide were evolved from soils treated with homocystine, and trace amounts of carbonyl sulfide were evolved from soils treated with lanthionine or djenkolic acid. No volatile sulfur compounds were evolved from soils treated with cysteic acid, taurine, or S-methyl methionine. The amounts of sulfur volatilized from soils treated with the 14 S-containing amino acids studied represented from less than 0·1 per cent to more than 50 per cent of the sulfur added as amino acid. Hydrogen sulfide could not be detected as a gaseous product of microbial decomposition of S-containing amino acids in soils under aerobic or waterlogged conditions.