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

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demonstrating that BrO and ClO with GEM are endothermic (27) and thus reaction 2 and 3 are most<br />

probably not important for the removal of Hg o in the atmosphere.<br />

Instead of BrO and ClO, GEM may react with Cl and/or Br. Therefore the data were analysed<br />

assuming relative rate conditions between ozone and GEM. The method is widely used under<br />

laboratory conditions, where the reaction of interest is proceeding in competition with another<br />

reaction with a well-known reaction rate constant. So the system here is:<br />

and<br />

O + X → product<br />

3 (4)<br />

Hg + X → product<br />

(5),<br />

where X is either Br or Cl and assuming that all other reactions are of negligible importance for the<br />

removal of ozone and GEM.<br />

The kinetic equations for reaction 4 and 5 are:<br />

and<br />

[ GEM ]<br />

∫<br />

[ GEM ]<br />

[ O ]<br />

3<br />

∫<br />

[ O ]<br />

t<br />

t<br />

d ln [ O ] = −k<br />

[ X ]dt<br />

(6)<br />

3 0<br />

3<br />

t<br />

∫<br />

4<br />

0<br />

t<br />

d ln [ GEM ] = −k<br />

[ X ]dt<br />

(7),<br />

0<br />

respectively.<br />

∫<br />

5<br />

0<br />

Integrating equation and dividing equation 6 with 7 the relative rate expression is obtained.<br />

[ GEM ]<br />

[ GEM ]<br />

[ ]<br />

[ ] ⎟⎟<br />

O ⎞ 3 0<br />

O<br />

⎛<br />

⎛<br />

0 ⎞ k5<br />

ln ⎜ ⎟ = • ln⎜<br />

⎜<br />

(8).<br />

⎝<br />

t ⎠ k4<br />

⎝ 3 t ⎠<br />

A plot of ln([GEM]0/[GEM]t against ln([O3]0/[O3]t should give a straight line with intercept 0 and a<br />

slope equal to k5/k4. Fig. 4 shows such a plot using the data from Station Nord. Data were selected<br />

for periods where the initial concentration of GEM was above 0.4 ng/m 3 in order to ensure good<br />

signal to noise ratio and where three consecutive measurements of both ozone and GEM are<br />

decreasing. All measurement included were in periods with 24 hour daylight. There is a strong<br />

linear correlation (

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