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.
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页码:4157 / 4169
页数:13
相关论文
共 68 条
[42]   HETEROGENEOUS REACTIONS OF CHLORINE NITRATE AND HYDROGEN-CHLORIDE ON TYPE-I POLAR STRATOSPHERIC CLOUDS [J].
LEU, MT ;
MOORE, SB ;
KEYSER, LF .
JOURNAL OF PHYSICAL CHEMISTRY, 1991, 95 (20) :7763-7771
[43]  
LISTER D.H., 1999, Aviation and the Global Atmosphere: A Special Report of the Intergovernmental Panel on Climate Change
[44]   Diffusion kinetics of HC1 hydrates in ice measured using infrared laser resonant desorption depth-profiling [J].
Livingston, FE ;
George, SM .
JOURNAL OF PHYSICAL CHEMISTRY A, 2001, 105 (21) :5155-5164
[45]   Depth-profiling and diffusion measurements in ice films using infrared laser resonant desorption [J].
Livingston, FE ;
Smith, JA ;
George, SM .
ANALYTICAL CHEMISTRY, 2000, 72 (22) :5590-5599
[46]   REDUCTIONS OF ANTARCTIC OZONE DUE TO SYNERGISTIC INTERACTIONS OF CHLORINE AND BROMINE [J].
MCELROY, MB ;
SALAWITCH, RJ ;
WOFSY, SC ;
LOGAN, JA .
NATURE, 1986, 321 (6072) :759-762
[47]   Exploration of the mechanism of the activation of ClONO2 by HCl in small water clusters using electronic structure methods [J].
McNamara, JP ;
Tresadern, G ;
Hillier, IH .
JOURNAL OF PHYSICAL CHEMISTRY A, 2000, 104 (17) :4030-4044
[48]   AN UPPER LIMIT TO THE RATE OF THE HCL + CLONO2 REACTION [J].
MOLINA, LT ;
MOLINA, MJ ;
STACHNIK, RA ;
TOM, RD .
JOURNAL OF PHYSICAL CHEMISTRY, 1985, 89 (18) :3779-3781
[49]   ANTARCTIC STRATOSPHERIC CHEMISTRY OF CHLORINE NITRATE, HYDROGEN-CHLORIDE AND ICE - RELEASE OF ACTIVE CHLORINE [J].
MOLINA, MJ ;
TSO, TL ;
MOLINA, LT ;
WANG, FCY .
SCIENCE, 1987, 238 (4831) :1253-1257
[50]   Real-time kinetics of the uptake of ClONO2 on ice and in the presence of HCl in the temperature range 160K<=T<=200K [J].
Oppliger, R ;
Allanic, A ;
Rossi, MJ .
JOURNAL OF PHYSICAL CHEMISTRY A, 1997, 101 (10) :1903-1911