| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4699772 | Chemical Geology | 2011 | 8 Pages |
Abstract
⺠Volcanic Hg(0) (i.e., Hg(g)) may be rapidly oxidised to Hg(II) (as HgCl2(g)) at the vent. ⺠Hg(II) production at volcanic vents is enhanced in lower temperature, HCl-rich magmatic gases. ⺠Near-source Hg speciation can be explained without invoking rapid, low temperature oxidation.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
R.S. Martin, M.L.I. Witt, D.M. Pyle, T.A. Mather, S.F.L. Watt, E. Bagnato, S. Calabrese,