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Detailed Reference Information |
Jeffers, P.M. and Wolfe, N.L. (1996). On the degradation of methyl bromide in sea water. Geophysical Research Letters 23: doi: 10.1029/96GL01670. issn: 0094-8276. |
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Methyl bromide degradation in sea water can be described by a summation of the hydrolysis and chloride ion exchange reactions. Laboratory experiments covered chloride concentrations of 0.1 to 1.0 mol/l, and temperatures from 20 to 60 ¿C. The first-order hydrolysis rate constant is k(H2O)=(5.7¿0.6)¿1011 e-(12455¿240)/T sec-1 and the second-order chloride ion exchange rate constant deduced from the experiment is k(Cl-)=(1.09¿0.21)¿1013 e-(12724¿560)/T l/mol.sec. At a sea water surface temperature of 21.9 ¿C and a chloride concentration of 0.56 mol/l, the calculated degradation half-life of methyl bromide in sea water is 4 days. At 35 ¿C, &tgr;1/2=22 hr. |
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Abstract |
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Keywords
Atmospheric Composition and Structure, Biosphere/atmosphere interactions, Atmospheric Composition and Structure, Chemical kinetic and photochemical properties, Atmospheric Composition and Structure, Troposphere—constituent transport and chemistry |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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