文摘
Previous studies have demonstrated that gas-phase H2Scan immobilize certain redox-sensitive contaminants (e.g.,Cr, U, Tc) in vadose zone environments. A key issue foreffective and efficient delivery of H2S in these environmentsis the reactivity of the gas with indigenous iron oxides.To elucidate the factors that control the transport of H2Sin the vadose zone, laboratory column experiments wereconducted to identify reaction mechanisms and measurerates of H2S oxidation by iron oxide-coated sands using severalcarrier gas compositions (N2, air, and O2) and flow rates.Most experiments were conducted using ferrihydrite-coatedsand. Additional studies were conducted with goethite-and hematite-coated sand and a natural sediment. Selectiveextractions were conducted at the end of each columnexperiment to determine the mass balance of the reactionproducts. XPS was used to confirm the presence of thereaction products. For column experiments in whichferrihydrite-coated sand was the substrate and N2 wasthe carrier gas, the major H2S oxidation products were FeSand elemental sulfur (mostly S80, represented as S0 forsimplicity) at ratios that were consistent with the stoichiometryof the postulated reactions. When air or O2 were usedas the carrier gas, S0 became the dominant reaction productalong with FeS2 and smaller amounts of FeS, sulfate,and thiosulfate. A mathematical model of reactive transportwas used to test the hypothesis that S0 forming on theiron oxide surfaces reduces access of H2S to the reactivesurface. Several conceptual models were assessed inthe context of the postulated reactions with the final modelbased on a linear surface poisoning model and fittedreaction rates. These results indicate that carrier gasselection is a critical consideration with significant tradeoffsfor remediation objectives.