We present a new
chemical mechanism for Hg0/HgI/HgII atmospheric cycling, including recent laboratory
and computational data, and implement it in the GEOS-Chem global atmospheric
chemistry model for comparison to observations. Our mechanism includes
the oxidation of Hg0 by Br and OH, subsequent oxidation
of HgI by ozone and radicals, respeciation of HgII in aerosols and cloud droplets, and speciated HgII photolysis
in the gas and aqueous phases. The tropospheric Hg lifetime against
deposition in the model is 5.5 months, consistent with observational
constraints. The model reproduces the observed global surface Hg0 concentrations and HgII wet deposition fluxes.
Br and OH make comparable contributions to global net oxidation of
Hg0 to HgII. Ozone is the principal HgI oxidant, enabling the efficient oxidation of Hg0 to HgII by OH. BrHgIIOH and HgII(OH)2, the initial HgII products of Hg0 oxidation,
respeciate in aerosols and clouds to organic and inorganic complexes,
and volatilize to photostable forms. Reduction of HgII to
Hg0 takes place largely through photolysis of aqueous HgII–organic complexes. 71% of model HgII deposition
is to the oceans. Major uncertainties for atmospheric Hg chemistry
modeling include Br concentrations, stability and reactions of HgI, and speciation and photoreduction of HgII in
aerosols and clouds.
Six of the eleven possible cyclic isomers (CH) 2 B 2 N 2 are found, by geometric optimization at a correlated level of theory, to have planar closed-shell ground states. Current density maps calculated with distributed-origin coupled Hartree± Fock theory wavefunctions show that all six of these have delocalized p-electron systems supporting diamagnetic ring currents. In comparison with benzene at the same level of theory, the isomer with lowest energy, 1; 3; 2; 4 diazadiborinine, has a 5% greater centre of ring shielding, but 20± 25% smaller mean magnetizability, mean polarizability and polarizability anisotropy.
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