Mt. Leu et al., HETEROGENEOUS REACTIONS OF HNO3(G)-]HCL(G)+NANO3(S) AND N2O5(G)+NACL(S)-]CLNO2(G)+NANO3(S)(NACL(S)), Journal of physical chemistry, 99(35), 1995, pp. 13203-13212
The heterogeneous reactions of HNO3(g) + NaCl(s) --> HCl(g) + NaNO3(s)
(eq 1) and N2O5(g) + NaCl(s) --> CINO2(g) + NaNO3(s) (eq 2) were inve
stigated over the temperature range 223-296 K in a now-tube reactor co
upled to a quadrupole mass spectrometer. Either a chemical ionization
mass spectrometer (CIMS) or an electron-impact ionization mass spectro
meter (EIMS) was used to provide suitable detection sensitivity and se
lectivity. In order to mimic atmospheric conditions, partial pressures
of HNO3 and N2O5 in the range 6 x 10(-8) similar to 2 x 10(-6) Torr w
ere used. Granule sizes and surface roughness of the solid NaCl substr
ates were determined by using a scanning electron microscope. For dry
NaCl substrates, decay rates of HNO3 were used to obtain gamma(1) = 0.
013 +/- 0.004 (1 sigma) at 296 K and >0.008 at 223 K, respectively. Th
e error quoted is the statistical error. After all corrections were ma
de, the overall error, including systematic error, was estimated to be
about a factor of 2. HCl was found to be the sole gas-phase product o
f reaction 1. The mechanism changed from heterogeneous reaction to pre
dominantly physical adsorption when the reactor was cooled from 296 to
223 K. For reaction 2 using dry salts, gamma(2) was found to be less
than 1.0 x 10(-4) at both 223 and 296 K. The gas-phase reaction produc
t was identified as CINO2 in previous studies using an infrared spectr
ometer. An enhancement in reaction probability was observed if water w
as not completely removed from salt surfaces, probably due to the reac
tion of N2O5(g) + H2O(s) --> 2HNO(3)(g). Our results are compared with
previous literature values obtained using different experimental tech
niques and conditions. The implications of the present results for the
enhancement of the hydrogen chloride column density in the lower stra
tosphere after the El Chichon volcanic eruption and for the chemistry
of HC1 and HNO3 in the marine troposphere are discussed.