FTIR studies of annealing processes and irradiation effects at 266 nm in ozone-amorphous ice-mixtures

Fourier transform infrared (FTIR) spectroscopy is used to study the vibrational spectrum of ozone trapped in amorphous ice (a situation observed on icy satellites in the solar system). Evaporation of ozone from ice is investigated from 30 to 150 K under a static pressure of 10⁻⁷ Torr. Condensed and...

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Veröffentlicht in:Физика низких температур
Datum:2000
Hauptverfasser: Chaabouni, H., Schriver-Mazzuoli, L., Schriver, A.
Format: Artikel
Sprache:Englisch
Veröffentlicht: Фізико-технічний інститут низьких температур ім. Б.І. Вєркіна НАН України 2000
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Online Zugang:https://nasplib.isofts.kiev.ua/handle/123456789/129218
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Zitieren:FTIR studies of annealing processes and irradiation effects at 266 nm in ozone-amorphous ice-mixtures / H. Chaabouni, L. Schriver-Mazzuoli, A. Schriver // Физика низких температур. — 2000. — Т. 26, № 9-10. — С. 963-971. — Бібліогр.: 33 назв. — англ.

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Digital Library of Periodicals of National Academy of Sciences of Ukraine
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author Chaabouni, H.
Schriver-Mazzuoli, L.
Schriver, A.
author_facet Chaabouni, H.
Schriver-Mazzuoli, L.
Schriver, A.
citation_txt FTIR studies of annealing processes and irradiation effects at 266 nm in ozone-amorphous ice-mixtures / H. Chaabouni, L. Schriver-Mazzuoli, A. Schriver // Физика низких температур. — 2000. — Т. 26, № 9-10. — С. 963-971. — Бібліогр.: 33 назв. — англ.
collection DSpace DC
container_title Физика низких температур
description Fourier transform infrared (FTIR) spectroscopy is used to study the vibrational spectrum of ozone trapped in amorphous ice (a situation observed on icy satellites in the solar system). Evaporation of ozone from ice is investigated from 30 to 150 K under a static pressure of 10⁻⁷ Torr. Condensed and chemisorbed ozone on the surface of micropores is released at a temperature between 40 and 80 K, and ozone in water lattice evaporates starting from 120 K. The release of ozone probes the gradual transformation of water ice. The photochemistry of ozone in excess ice is also investigated using 266 nm laser irradiation. At low temperature, condensation of H₂O/O₃ mixtures leads to ozone trapped in pores and cavities, and H₂O₂ is produced through the hydrogen-bonded complex between ozone and free OH bonds. At higher temperature, when a solid solution of ozone in water is observed, H₂O₂ is formed by the reaction of the excited oxygen atom O(¹D) with the nearest water molecules. Kinetic studies suggest that recombination of the dioxygen molecule with ground-state atomic oxygen O(³P) is a minor channel.
first_indexed 2025-12-07T19:24:28Z
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language English
last_indexed 2025-12-07T19:24:28Z
publishDate 2000
publisher Фізико-технічний інститут низьких температур ім. Б.І. Вєркіна НАН України
record_format dspace
spelling Chaabouni, H.
Schriver-Mazzuoli, L.
Schriver, A.
2018-01-17T19:53:47Z
2018-01-17T19:53:47Z
2000
FTIR studies of annealing processes and irradiation effects at 266 nm in ozone-amorphous ice-mixtures / H. Chaabouni, L. Schriver-Mazzuoli, A. Schriver // Физика низких температур. — 2000. — Т. 26, № 9-10. — С. 963-971. — Бібліогр.: 33 назв. — англ.
0132-6414
PACS: 78.30.Hv, 71.55.Ht
https://nasplib.isofts.kiev.ua/handle/123456789/129218
Fourier transform infrared (FTIR) spectroscopy is used to study the vibrational spectrum of ozone trapped in amorphous ice (a situation observed on icy satellites in the solar system). Evaporation of ozone from ice is investigated from 30 to 150 K under a static pressure of 10⁻⁷ Torr. Condensed and chemisorbed ozone on the surface of micropores is released at a temperature between 40 and 80 K, and ozone in water lattice evaporates starting from 120 K. The release of ozone probes the gradual transformation of water ice. The photochemistry of ozone in excess ice is also investigated using 266 nm laser irradiation. At low temperature, condensation of H₂O/O₃ mixtures leads to ozone trapped in pores and cavities, and H₂O₂ is produced through the hydrogen-bonded complex between ozone and free OH bonds. At higher temperature, when a solid solution of ozone in water is observed, H₂O₂ is formed by the reaction of the excited oxygen atom O(¹D) with the nearest water molecules. Kinetic studies suggest that recombination of the dioxygen molecule with ground-state atomic oxygen O(³P) is a minor channel.
en
Фізико-технічний інститут низьких температур ім. Б.І. Вєркіна НАН України
Физика низких температур
Low-Temperature Physics and Chemistry in Cryomatrice
FTIR studies of annealing processes and irradiation effects at 266 nm in ozone-amorphous ice-mixtures
Article
published earlier
spellingShingle FTIR studies of annealing processes and irradiation effects at 266 nm in ozone-amorphous ice-mixtures
Chaabouni, H.
Schriver-Mazzuoli, L.
Schriver, A.
Low-Temperature Physics and Chemistry in Cryomatrice
title FTIR studies of annealing processes and irradiation effects at 266 nm in ozone-amorphous ice-mixtures
title_full FTIR studies of annealing processes and irradiation effects at 266 nm in ozone-amorphous ice-mixtures
title_fullStr FTIR studies of annealing processes and irradiation effects at 266 nm in ozone-amorphous ice-mixtures
title_full_unstemmed FTIR studies of annealing processes and irradiation effects at 266 nm in ozone-amorphous ice-mixtures
title_short FTIR studies of annealing processes and irradiation effects at 266 nm in ozone-amorphous ice-mixtures
title_sort ftir studies of annealing processes and irradiation effects at 266 nm in ozone-amorphous ice-mixtures
topic Low-Temperature Physics and Chemistry in Cryomatrice
topic_facet Low-Temperature Physics and Chemistry in Cryomatrice
url https://nasplib.isofts.kiev.ua/handle/123456789/129218
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