1. ToF-SIMS analysis of abiotic and biotic iron sulfide layers formed in aqueous conditions on iron surfaces.
- Author
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El Menjra, Anne-Ilham, Seyeux, Antoine, Mercier, Dimitri, Beech, Iwona, Makama, Zakari, and Marcus, Philippe
- Subjects
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IRON sulfides , *SECONDARY ion mass spectrometry , *SILVER sulfide , *CHRONOAMPEROMETRY , *IRON alloys - 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 Na 2 S,9H 2 O (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 δ34S V-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. • ToF-SIMS is used to study abiotically and biotically (from SRB) generated iron sulfide layers formed on iron surfaces. • A peak-fitting method and data processing was developed and applied on ToF-SIMS spectra. • Different sulfur isotopic fractionations δ34S (-0.23 ‰ and -13.69 ‰) were obtained for abiotic and biotic iron sulfide layers. • The ToF-SIMS approach presented allows the identification of bacterial contribution in sulfur corrosion products. • The ToF-SIMS approach allows a better understanding of biocorrosion to sulfur originated from abiotic and biotic sources in aqueous medium. [ABSTRACT FROM AUTHOR]
- Published
- 2019
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