HETEROGENEOUS REACTIONS OF HNO3(G)-]HCL(G)+NANO3(S) AND N2O5(G)+NACL(S)-]CLNO2(G)+NANO3(S)(NACL(S))

Citation
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
Citations number
43
Categorie Soggetti
Chemistry Physical
ISSN journal
00223654
Volume
99
Issue
35
Year of publication
1995
Pages
13203 - 13212
Database
ISI
SICI code
0022-3654(1995)99:35<13203:HROHAN>2.0.ZU;2-S
Abstract
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.