Measurements of peroxide concentrations in fog water were conducted near th
e summit of Mt. Norikura (altitude, 2770m) in central Japan, and at the mid
slope of Mt. Oyama (altitude, 680m), southwest of the Kanto Plain. The conc
entrations of peroxide at Mt. Norikura, far from industrial regions, ranged
from 3 to 120 muM during the summer and early autumn in 1993. The potentia
l capacity for SO, oxidation appears to be very high near the summit of Mt.
Norikura. Analysis of the chemical composition of three-stage size-fractio
nated fog water samples collected at Mt. Norikura showed that the concentra
tions of peroxide were apparently independent of droplet size, whereas the
concentrations of chemical constituents mainly derived from secondary aeros
ols and the acidity were higher in smaller droplets. Peroxide concentration
s in fog water were low (< 5 muM) at Mt. Oyama, located near heavy industri
al areas, and lower than those in rain water sampled simultaneously (0.2-33
mu M). Especially, peroxide was scarcely detected in strongly acidic fogs
(< 0.2 mu M). Peroxide might have been decomposed by SO2 (S(IV)) oxidation
in the aqueous-phase.