The atom is the dominating species of mercury in the atmosphere. Its oxidat
ion processes are of great interest since it is mainly oxidised mercury tha
t undergoes deposition and thereby spreads into the ecosystems and becomes
bioaccumulated. The kinetics of the gas-phase reaction between atomic mercu
ry and hydroxyl radical has been determined at room temperature and atmosph
eric pressure of air by relative rate technique. OH radicals were produced
by photolysis employing methyl nitrite. By using cyclohexane as the referen
ce compound, the rate coefficient obtained was k(Hg-o + OH) = (8.7 +/- 2.8)
x 10(-14) cm(3) s(-1) leading to natural lifetimes of mercury at global me
an conditions of 4-7 month due to this reaction. (C) 2001 Elsevier Science
Ltd. All rights reserved.