HENRYS LAW CONSTANT DETERMINATIONS FOR HYDROGEN-PEROXIDE, METHYL HYDROPEROXIDE, HYDROXYMETHYL HYDROPEROXIDE, ETHYL HYDROPEROXIDE, AND PEROXYACETIC ACID
Dw. Osullivan et al., HENRYS LAW CONSTANT DETERMINATIONS FOR HYDROGEN-PEROXIDE, METHYL HYDROPEROXIDE, HYDROXYMETHYL HYDROPEROXIDE, ETHYL HYDROPEROXIDE, AND PEROXYACETIC ACID, Journal of physical chemistry, 100(8), 1996, pp. 3241-3247
The temperature-dependent solubilities of hydrogen peroxide (H2O2), hy
droxymethyl hydroperoxide (HOCH2O2H), methyl hydroperoxide (CH3O2H), p
eroxyacetic acid (CH3C(O)O2H), and ethyl hydroperoxide (C2H5O2H) were
determined under conditions used in the aqueous collection and analysi
s oi atmospheric hydroperoxides. Henry's law was obeyed over the sourc
e concentration range employed, nominally 10(-6)-10(-2) M. Measurement
s were made using either pH = 3 or pH = 6 source and collection soluti
ons. The temperatures investigated ranged from 4 to 28 degrees C. A so
lution pH 3 was used for experiments with H2O2, HOCH2O2H, and CH3C(O)O
2H since these compounds decompose in less acidic solution. The solubi
lity of HOC2H4O2H could not be accurately determined because of its ra
pid decomposition in solutions with pH > 3. The Henry's law solubility
of H2O2, HOCH2O2H, CH3O2H, and CH3C(O)O2H are in agreement with prior
determinations. The solubility measurement of C2H5O2H is the first of
its kind. Dimensional Henry's law constants (M/atm) can be expressed
by In(K-h) = A/T - B, where Tis in degrees kelvin. K-h at 25 degrees C
and the A and B coefficients are [GRAPHICS] The high solubility of HO
CH2O2H implies it will be efficiently removed from the atmosphere by p
recipitation or surface deposition. Its decomposition and that of HOC2
H4O2H and CH3C(O)O2H forming H2O2 near neutral pH suggest these hydrop
eroxides may constitute a heterogeneous source of H2O2 in atmospheric
water if they are formed in the troposphere. The solubility of the lis
ted organic hydroperoxides and the propensity of three of them to deco
mpose at neutral pH further underscores the potential for interference
's and artifacts in the aqueous collection and nonspecific analysis of
H2O2 in the atmosphere.