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FATE OF MERCURY IN THE ARCTIC Michael Evan ... - COGCI

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Fate of Mercury in the Arctic 99<br />

Similarly, the product cannot be Hg2Br2 since this would imply a tri-molecular reaction, which<br />

statistically is highly unlikely to occur in the atmosphere due to the very low concentrations of<br />

elemental mercury and bromine atoms. The combination of Hg and Nr atoms and the dimerization<br />

of HgBr is discussed in Grieg et al., (1970).<br />

Nor would the product be HgO, since this formation is similarly thermodynamically not<br />

favourable.<br />

The final product is the divalent gaseous mercury unknown, HgXY, proposed to be HgBr2.<br />

By modelling the reaction of Hg and Br in the atmosphere, with current rate constant data, and<br />

BrO measurements, i.e., assuming 20 ppt BrO and 2 ppt Br in the atmosphere during a depletion<br />

event, it is calculated that the lifetime of Hg is 4.6 hrs against forming HgBr,<br />

The lifetime of HgBr is 0.35 hrs. against forming HgBr2; comparing with the lifetime of HgBr<br />

of 0.75 hrs, means that 68% of the time HgBr will form HgBr2.<br />

Thus the overall lifetime of removal of Hg to HgBr2 is 4.6 hrs. / .68 = 6.7 hrs. This is in good<br />

agreement with the observed 10 hr lifetime of Hg under depletion, and therefore the above reaction<br />

mechanism is plausible as one of the limiting reactions for the oxidation of elemental mercury to<br />

reactive gaseous mercury in the post polar sunrise atmosphere, though it is realized that given the<br />

dynamics of atmospheric chemistry, that the above scheme is based on a simple model with limited<br />

laboratory kinetics data to carry out the calculations and that HgBr may also be reacting with O2 or<br />

many other elements or compounds in the Arctic atmosphere.<br />

RGM concentration measurements<br />

RGM measurements performed in parallel at Station Nord in 2002 show that the concentration<br />

varies from between values below detection limit and up to 75 ng/m 3 , Figure 13., page 71. These<br />

values are comparable to those found at Barrow before the start of AMDE’s and are comparable to<br />

levels measured in the Dr. Lindbergs’ laboratory in Oak Ridge. These values were measured prior

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