Abstract
Background: Pyrite, the most abundant metal sulphide on Earth, is known to spontaneously form hydrogen peroxide when exposed to water. In this study the hypothesis that pyrite-induced hydrogen peroxide is transformed to hydroxyl radicals is tested. Results: Using a combination of electron spin resonance (ESR) spin-trapping techniques and scavenging reactions involving nucleic acids, the formation of hydroxyl radicals in pyrite/aqueous suspensions is demonstrated. The addition of EDTA to pyrite slurries inhibits the hydrogen peroxide-to-hydroxyl radical conversion, but does not inhibit the formation of hydrogen peroxide. Given the stability of EDTA chelation with both ferrous and ferric iron, this suggests that the addition of the EDTA prevents the transformation by chelation of dissolved iron species. Conclusion: While the exact mechanism or mechanisms of the hydrogen peroxide-to-hydroxyl radical conversion cannot be resolved on the basis of the experiments reported in this study, it is clear that the pyrite surface promotes the reaction. The formation of hydroxyl radicals is significant because they react nearly instantaneously with most organic molecules. This suggests that the presence of pyrite in natural, engineered, or physiological aqueous systems may induce the transformation of a wide range of organic molecules. This finding has implications for the role pyrite may play in aquatic environments and raises the question whether inhalation of pyrite dust contributes to the development of lung diseases.
Original language | English |
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Article number | 3 |
Journal | Geochemical Transactions |
Volume | 7 |
DOIs | |
State | Published - 4 Apr 2006 |
Externally published | Yes |
Bibliographical note
Funding Information:This work was funded by the Department of Energy through grants to D.R.S. and M.A.S., Basic Energy Sciences grants DEFG029ER14644 and DEFG0296ER14633, respectively, and the Center for Environmental Molecular Science (NSF CHE 0221934). C.C. acknowledges support from a National Defence Science and Engineering Graduate Fellowship.
Funding
This work was funded by the Department of Energy through grants to D.R.S. and M.A.S., Basic Energy Sciences grants DEFG029ER14644 and DEFG0296ER14633, respectively, and the Center for Environmental Molecular Science (NSF CHE 0221934). C.C. acknowledges support from a National Defence Science and Engineering Graduate Fellowship.
Funders | Funder number |
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Center for Environmental Molecular Science | |
National Defence Science and Engineering | |
National Science Foundation | CHE 0221934 |
U.S. Department of Energy | |
Basic Energy Sciences | DEFG0296ER14633, DEFG029ER14644 |