Soil Science Society of America Journal · 1973 · 24 citations · 0 references
Natural SciencesSoil SciencesSoil BiogeochemistrySoil ChemistrySoil ScienceMetal SulfidesRedox ProcessesSulfur CycleSulfur OxidesOxidationRedox PotentialRedox Potential ChangesSoil Redox DynamicsSoil Redox PotentialSulfate ReductionSulfate Reduction PathwaysSulfur Transformation
Abstract The effect of various chemical oxidants on inhibition of sulfide (S 2‐ ) in a previously reduced soil was studied. Oxygen, KNO 3 , MnO 2 , ferricitrophosphate, and FePO 4 · 2H 2 O at rates equivalent to 1,000 ppm O 2 (O 2 added at rates of either 300 or 500 ppm) were both added prior to flooding and after soil reduction had reached a maximum. The results indicate that the more soluble oxidants had the greatest effects in maintaining more positive redox potentials and in delaying sulfate (SO 4 2‐ ) reduction to S 2‐ . The soluble oxidants (KNO 3 and ferricitrophosphate) delayed S 2‐ production by 17 and 9 days, respectively. The less soluble compounds (MnO 2 and FePO 4 · 2H 2 O) were less effective in delaying S 2‐ production but persisted longer in preventing maximum S 2‐ buildup. Adding the oxidants after maximum S 2‐ accumulation showed the most pronounced effect on S 2‐ oxidation from KNO 3 and the least effect from MnO 2 . Oxygen at the rate of 500 ppm was also a very effective oxidant. Sulfate reduction to S 2‐ and S 2‐ oxidation were apparently controlled by, or at best related to the redox potential since SO 4 2‐ reduction and S 2‐ oxidation both appeared to commence at potentials in the vicinity of −100 mV.