GEM, with an atmospheric lifetime in the range of 5 — 24 months, can be transported across long distances to remote locations before conversion to divalent Hg species by
atmospheric oxidation processes (4).
Not exact matches
Reactions in and on sea - salt aerosol particles may have a strong influence on
oxidation processes in the marine boundary layer through the production of halogen radicals, and reactions on mineral aerosols may significantly affect the cycles of nitrogen, sulfur, and
atmospheric oxidants.
Currently, the role of CH4
oxidation (a microbial
process that consumes methane) in mediating
atmospheric CH4 fluxes during lake turnover events is also not well understood.
(if 20 % of geologic burial of C (0.2 Gt / year) is organic C and if that is nearly balanced by
oxidation of geologic organic C, that would be a C flux of 0.04 Gt / year, which is 0.08 % of 50 Gt / year, so the oxygen depletion, as a fraction of total
atmospheric O2, would be 0.08 % * 0.011 % / year = 0.0000088 % / year — or 8.8 E-6 % / year; it would take a bit more than 10 million years to use up all
atmospheric O2 by such a
process.