| Literature DB >> 35412772 |
Xiang Zhang1, Michael J Borda2, Martin Aa Schoonen2, Daniel R Strongin1.
Abstract
The effect of a diacetylene-containing phospholipid on the oxidation of pyrite, FeS2, was investigated. Earlier work reported by our research group showed that the adsorption of l,2-bis(10,12-tricosadiynoyl)-sn-glycero-3-phosphocholine on pyrite suppressed the extent of its oxidation by about 75% over a specific time period. Results presented here show that the pre-exposure to UV radiation of this lipid after sorption onto pyrite results in a 90% suppression. Attenuated total reflection (ATR) Fourier transform infra-red spectroscopy (FTIR) suggests that the UV irradiation of the lipid does not result in degradation of the adsorbed layer. It is believed that the UV exposure results in the cross-linking and polymerization of the adsorbed phospholipid into a relatively impermeable barrier that separates the pyrite from the aqueous phase. The results of this study might have implications for the protection of pyrite from oxidation in the environment.Entities:
Year: 2003 PMID: 35412772 PMCID: PMC1475633 DOI: 10.1186/1467-4866-4-8
Source DB: PubMed Journal: Geochem Trans ISSN: 1467-4866 Impact factor: 4.737
Figure 1Fe solution concentration as a function of time for lipid/pyrite, lipid/pyrite with UV, and for two control experiments, pyrite alone, and pyrite that was exposed to UV radiation. The amount of iron release for a given time interval is lowest for the lipid/pyrite surface that had been exposed to UV radiation prior to the start of the Fe release measurements.
Figure 2FTIR of lipid covered pyrite (a) before and (b) after exposure to UV radiation. Association of specific vibrational modes with functional groups of the lipid are indicated.
Figure 3Schematic representation of a proposed model for the cross-linked lipid/pyrite surface. UV irradiation leads to the cross-linking (indicated by dashed line) and the stabilization of the lipid layer compared to the lipid layer without UV exposure. Whether a bilayer structure forms at the pyrite surface cannot be ascertained from the experimental results.