Abstract

An approach for the identification of the origin of iron sulfides formation on iron surfaces using Time-of-Flight Secondary Ions Mass Spectrometry (ToF-SIMS) is reported here in. Two different sulfidation processes of iron surfaces are presented (both at room temperature): the first abiotic procedure was carried out using chronoamperometry (E = −0.8 V/SCE) of pure iron in 10 mM of Na2S,9H2O (pH = 11) while the second biotic procedure was accomplished by immersing a pure iron sample in a medium containing HS− ions produced by a sulfate-reducing bacterium (SRB) of the genus Desulfovibrio at an open circuit potential (OCP). A surface analytical method using Time-of-Flight Secondary Ions Mass Spectrometry (ToF-SIMS) coupled with ToF-SIMS spectra peak-fitting and data processing was developed to calculate an accurate sulfur isotopic fractionation δ34SV-CDT on iron sulfide layers formed on iron surfaces, thus allowing to discriminate between abiotically versus biotically generated sulfides. This approach contributes to a better understanding of iron surface interactions with sulfur containing environmental species of abiotic or biotic origin.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.