Reaction of Chlorine Nitrate with Hydrogen Chloride and Water at Antarctic Stratospheric Temperatures
Laboratory studies of heterogeneous reactions important for ozone depletion over Antarctica are reported. The reaction of chlorine nitrate (ClONO 2 ) with H 2 O and hydrogen chloride (HCl) on surfaces that simulate polar stratospheric clouds [ice and nitric acid (HNO 3 )—ice and sulfuric acid] are s...
Published in: | Science |
---|---|
Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Association for the Advancement of Science (AAAS)
1987
|
Subjects: | |
Online Access: | http://dx.doi.org/10.1126/science.238.4831.1258 https://www.science.org/doi/pdf/10.1126/science.238.4831.1258 |
id |
craaas:10.1126/science.238.4831.1258 |
---|---|
record_format |
openpolar |
spelling |
craaas:10.1126/science.238.4831.1258 2024-09-30T14:24:52+00:00 Reaction of Chlorine Nitrate with Hydrogen Chloride and Water at Antarctic Stratospheric Temperatures Tolbert, Margaret A. Rossi, Michel J. Malhotra, Ripudaman Golden, David M. 1987 http://dx.doi.org/10.1126/science.238.4831.1258 https://www.science.org/doi/pdf/10.1126/science.238.4831.1258 en eng American Association for the Advancement of Science (AAAS) Science volume 238, issue 4831, page 1258-1260 ISSN 0036-8075 1095-9203 journal-article 1987 craaas https://doi.org/10.1126/science.238.4831.1258 2024-09-12T04:01:38Z Laboratory studies of heterogeneous reactions important for ozone depletion over Antarctica are reported. The reaction of chlorine nitrate (ClONO 2 ) with H 2 O and hydrogen chloride (HCl) on surfaces that simulate polar stratospheric clouds [ice and nitric acid (HNO 3 )—ice and sulfuric acid] are studied at temperatures relevant to the Antarctic stratosphere. The reaction of ClONO 2 on ice and certain mixtures of HNO 3 and ice proceeded readily. The sticking coefficient of ClONO 2 on ice of 0.009 ± 0.002 was observed. A reaction produced gas-phase hypochlorous acid (HOCl) and condensed-phase HNO 3 HOCl underwent a secondary reaction on ice producing dichlorine monoxide (Cl 2 O). In addition to the reaction with H 2 O, ClONO 2 reacted with HCl on ice to form gas-phase chlorine (Cl 2 ) and condensed-phase HNO 3. Essentially all of the HCl in the bulk of the ice can react with ClONO 2 on the ice surface. The gaseous products of the above reactions, HOCl, Cl 2 O, and Cl 2 , could readily photolyze in the Antarctic spring to produce active chlorine for ozone depletion. Furthermore, the formation of condensed-phase HNO 3 could serve as a sink for odd nitrogen species that would otherwise scavenge the active chlorine. Article in Journal/Newspaper Antarc* Antarctic Antarctica AAAS Resource Center (American Association for the Advancement of Science) Antarctic The Antarctic Science 238 4831 1258 1260 |
institution |
Open Polar |
collection |
AAAS Resource Center (American Association for the Advancement of Science) |
op_collection_id |
craaas |
language |
English |
description |
Laboratory studies of heterogeneous reactions important for ozone depletion over Antarctica are reported. The reaction of chlorine nitrate (ClONO 2 ) with H 2 O and hydrogen chloride (HCl) on surfaces that simulate polar stratospheric clouds [ice and nitric acid (HNO 3 )—ice and sulfuric acid] are studied at temperatures relevant to the Antarctic stratosphere. The reaction of ClONO 2 on ice and certain mixtures of HNO 3 and ice proceeded readily. The sticking coefficient of ClONO 2 on ice of 0.009 ± 0.002 was observed. A reaction produced gas-phase hypochlorous acid (HOCl) and condensed-phase HNO 3 HOCl underwent a secondary reaction on ice producing dichlorine monoxide (Cl 2 O). In addition to the reaction with H 2 O, ClONO 2 reacted with HCl on ice to form gas-phase chlorine (Cl 2 ) and condensed-phase HNO 3. Essentially all of the HCl in the bulk of the ice can react with ClONO 2 on the ice surface. The gaseous products of the above reactions, HOCl, Cl 2 O, and Cl 2 , could readily photolyze in the Antarctic spring to produce active chlorine for ozone depletion. Furthermore, the formation of condensed-phase HNO 3 could serve as a sink for odd nitrogen species that would otherwise scavenge the active chlorine. |
format |
Article in Journal/Newspaper |
author |
Tolbert, Margaret A. Rossi, Michel J. Malhotra, Ripudaman Golden, David M. |
spellingShingle |
Tolbert, Margaret A. Rossi, Michel J. Malhotra, Ripudaman Golden, David M. Reaction of Chlorine Nitrate with Hydrogen Chloride and Water at Antarctic Stratospheric Temperatures |
author_facet |
Tolbert, Margaret A. Rossi, Michel J. Malhotra, Ripudaman Golden, David M. |
author_sort |
Tolbert, Margaret A. |
title |
Reaction of Chlorine Nitrate with Hydrogen Chloride and Water at Antarctic Stratospheric Temperatures |
title_short |
Reaction of Chlorine Nitrate with Hydrogen Chloride and Water at Antarctic Stratospheric Temperatures |
title_full |
Reaction of Chlorine Nitrate with Hydrogen Chloride and Water at Antarctic Stratospheric Temperatures |
title_fullStr |
Reaction of Chlorine Nitrate with Hydrogen Chloride and Water at Antarctic Stratospheric Temperatures |
title_full_unstemmed |
Reaction of Chlorine Nitrate with Hydrogen Chloride and Water at Antarctic Stratospheric Temperatures |
title_sort |
reaction of chlorine nitrate with hydrogen chloride and water at antarctic stratospheric temperatures |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
1987 |
url |
http://dx.doi.org/10.1126/science.238.4831.1258 https://www.science.org/doi/pdf/10.1126/science.238.4831.1258 |
geographic |
Antarctic The Antarctic |
geographic_facet |
Antarctic The Antarctic |
genre |
Antarc* Antarctic Antarctica |
genre_facet |
Antarc* Antarctic Antarctica |
op_source |
Science volume 238, issue 4831, page 1258-1260 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.238.4831.1258 |
container_title |
Science |
container_volume |
238 |
container_issue |
4831 |
container_start_page |
1258 |
op_container_end_page |
1260 |
_version_ |
1811642582415966208 |