The uptake of gas-phase methanol by liquid sulfuric acid has been investiga
ted over the composition range of 40-85 wt % H2SO4 and the temperature rang
e of 210-235 K. Laboratory studies were performed with a flow-tube reactor
coupled to an electron-impact ionization mass spectrometer to detect trace
gases. While reversible uptake was the primary mechanism at low acid concen
trations, an irreversible reaction between methanol and sulfuric acid at lo
w temperatures, forming methyl hydrogen sulfate and dimethyl sulfate, was o
bserved at all concentrations. At compositions >65 wt % H2SO4, more than 90
% of uptake was found to be reactive. On the basis of the uptake data and t
he calculated liquid-phase diffusion coefficients, the product of the effec
tive Henry's law constant (H*) and the square root of the overall liquid-ph
ase reaction rate (k(1)) was calculated as a function of acid concentration
and temperature. The results suggest that the reaction with sulfuric acid
forming methyl hydrogen sulfate and dimethyl sulfate is the dominant loss m
echanism of methanol and that the oxidation of methanol is only a minor sou
rce of hydroxyl radicals in the upper troposphere.