The nature of the interface and the diffusion coefficient of HCl/ice and HBr/ice in the temperature range 190-205 K

被引:8
作者
Aguzzi, A [1 ]
Flückiger, B [1 ]
Rossi, MJ [1 ]
机构
[1] Ecole Polytech Fed Lausanne, Lab Pollut Atmospher, Inst Sci & Technol Environm, CH-1015 Lausanne, Switzerland
关键词
D O I
10.1039/b308422c
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
We have investigated the structural properties of the near-surface region of various types of HX (X=Cl, Br)-doped H2O ice from a kinetic point of view by monitoring the time dependent [HX] in the interface region using the fast titration reaction XONO2 + HX --> X-2 + HNO3. These "dope and probe" experiments reveal that HX is located throughout a well-defined region of thickness I readily available for titration. At 190 K and a dose of 10(16) molecules corresponding to one HCl monolayer condensed onto a typically 1 mum thick ice sample, we measured I-HCl = 90 +/- 9, 120 +/- 15 and 90 +/- 30 nm for single crystalline (SC), condensed (C) and frozen liquid water or bulk (B) ices, respectively, with I-HCl increasing by up to a factor of two with a tenfold increase in HCl dose. The corresponding values for HBr at the same temperature are I-HBr = 20 +/- 2, 30 +/- 4 and 30 +/- 4 nm. In addition. we have determined the bulk diffusion coefficient in bulk ice for HX, D-HX, by applying Fick's second law of diffusion that results in values for D-HCl and D-HBr in the range 5.1.10(-14) -4.3. 10(-13) cm(2) s(-1) and 2.5. 10(-15) -7.0. 10(-14) cm(2) s(-1). respectively, depending on the type of ice in the temperature range 190-205 K. The consequences of these results for heterogeneous reactions on ice particles such as Cirrus clouds, contrails and PSC's type II are discussed.
引用
收藏
页码:4157 / 4169
页数:13
相关论文
共 68 条
[21]   Properties of the HCl/ice, HBr/ice, and H2O/ice interface at stratospheric temperatures (200 K) and its importance for atmospheric heterogeneous reactions [J].
Fluckiger, B ;
Chaix, L ;
Rossi, MJ .
JOURNAL OF PHYSICAL CHEMISTRY A, 2000, 104 (50) :11739-11750
[22]  
Fluckiger B, 1998, BER BUNSEN PHYS CHEM, V102, P915, DOI 10.1002/bbpc.19981020704
[23]   Second harmonic generation studies of ozone depletion reactions on ice surfaces under stratospheric conditions [J].
Geiger, FM ;
Tridico, AC ;
Hicks, JM .
JOURNAL OF PHYSICAL CHEMISTRY B, 1999, 103 (39) :8205-8215
[24]  
Gertner BJ, 1999, ISR J CHEM, V39, P273
[25]   HCL/H2O SOLID-PHASE VAPOR-PRESSURES AND HCL SOLUBILITY IN ICE [J].
HANSON, DR ;
MAUERSBERGER, K .
JOURNAL OF PHYSICAL CHEMISTRY, 1990, 94 (11) :4700-4705
[26]   HETEROGENEOUS CHEMISTRY OF BROMINE SPECIES IN SULFURIC-ACID UNDER STRATOSPHERIC CONDITIONS [J].
HANSON, DR ;
RAVISHANKARA, AR .
GEOPHYSICAL RESEARCH LETTERS, 1995, 22 (04) :385-388
[27]   REACTIVE UPTAKE OF CLONO2 ONTO SULFURIC-ACID DUE TO REACTION WITH HCL AND H2O [J].
HANSON, DR ;
RAVISHANKARA, AR .
JOURNAL OF PHYSICAL CHEMISTRY, 1994, 98 (22) :5728-5735
[28]   INVESTIGATION OF THE REACTIVE AND NONREACTIVE PROCESSES INVOLVING CLONO2 AND HCL ON WATER AND NITRIC-ACID DOPED ICE [J].
HANSON, DR ;
RAVISHANKARA, AR .
JOURNAL OF PHYSICAL CHEMISTRY, 1992, 96 (06) :2682-2691
[29]  
HANSON DR, 1993, NATO ASI SERIES, V17
[30]   EFFECTS OF INITIAL ACTIVE CHLORINE CONCENTRATIONS ON THE ANTARCTIC OZONE SPRING DEPLETION [J].
HENDERSON, GS ;
EVANS, WFJ ;
MCCONNELL, JC .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1990, 95 (D2) :1899-1908