ABSORPTIVITY OF ICE I IN THE RANGE 4000-30/cm

The absorbance of several samples of ice Ih has been measured in the range 4000-30/cm, and scaled to that of a particular film of unknown thickness. The thickness of the film has been calculated by two methods, first from the known absorptivity at 4940/cm, and second by equating the appropriate Kram...

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Main Authors: Bertie,J. E., Labbe,H. J., Whalley,E.
Other Authors: ALBERTA UNIV EDMONTON DEPT OF CHEMISTRY
Format: Text
Language:English
Published: 1968
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/AD0697594
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0697594
id ftdtic:AD0697594
record_format openpolar
spelling ftdtic:AD0697594 2023-05-15T16:37:31+02:00 ABSORPTIVITY OF ICE I IN THE RANGE 4000-30/cm Bertie,J. E. Labbe,H. J. Whalley,E. ALBERTA UNIV EDMONTON DEPT OF CHEMISTRY 1968-12-13 text/html http://www.dtic.mil/docs/citations/AD0697594 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0697594 en eng http://www.dtic.mil/docs/citations/AD0697594 Availability: Pub. in Jnl. of Chemical Physics, v50 n10 p4501-4520, 15 May 69. No copies furnished. DTIC AND NTIS Snow Ice and Permafrost Atomic and Molecular Physics and Spectroscopy (*ICE *INFRARED SPECTRA) WATER INFRARED SPECTROSCOPY DEUTERIUM COMPOUNDS VIBRATIONAL ENERGY LEVELS Text 1968 ftdtic 2016-02-18T22:39:51Z The absorbance of several samples of ice Ih has been measured in the range 4000-30/cm, and scaled to that of a particular film of unknown thickness. The thickness of the film has been calculated by two methods, first from the known absorptivity at 4940/cm, and second by equating the appropriate Kramers-Kronig integral to the known infrared contribution to the microwave refractive index. The two thicknesses agreed well and allowed the absorptivity to be obtained in the range 4000-30/cm. The complex refractive index and permittivity and the normal incidence reflectivity have been calculated from the absorptivity. About three-quarters of the infrared contribution to the microwave refractive index is caused by the translational lattice vibrations and about 15% by the rotational vibrations; the O-H stretching bands which absorb very strongly contribute relatively little. The maximum of the density of states in the transverse acoustic branch is at 65/cm rather than below 50/cm as reported earlier. A theory of the contribution of the translational lattice vibrations to the microwave permittivity is given based on the theory of the absorption by orientationally disordered crystals given in an earlier paper. From the theory and the experimental measurements reported in this paper the dipole-moment derivative for the relative displacement of two water molecules in ice along their line of centers (or equivalently the effective charge of a water molecule) is about 0.3 electronic charges. (Author) Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Snow
Ice and Permafrost
Atomic and Molecular Physics and Spectroscopy
(*ICE
*INFRARED SPECTRA)
WATER
INFRARED SPECTROSCOPY
DEUTERIUM COMPOUNDS
VIBRATIONAL ENERGY LEVELS
spellingShingle Snow
Ice and Permafrost
Atomic and Molecular Physics and Spectroscopy
(*ICE
*INFRARED SPECTRA)
WATER
INFRARED SPECTROSCOPY
DEUTERIUM COMPOUNDS
VIBRATIONAL ENERGY LEVELS
Bertie,J. E.
Labbe,H. J.
Whalley,E.
ABSORPTIVITY OF ICE I IN THE RANGE 4000-30/cm
topic_facet Snow
Ice and Permafrost
Atomic and Molecular Physics and Spectroscopy
(*ICE
*INFRARED SPECTRA)
WATER
INFRARED SPECTROSCOPY
DEUTERIUM COMPOUNDS
VIBRATIONAL ENERGY LEVELS
description The absorbance of several samples of ice Ih has been measured in the range 4000-30/cm, and scaled to that of a particular film of unknown thickness. The thickness of the film has been calculated by two methods, first from the known absorptivity at 4940/cm, and second by equating the appropriate Kramers-Kronig integral to the known infrared contribution to the microwave refractive index. The two thicknesses agreed well and allowed the absorptivity to be obtained in the range 4000-30/cm. The complex refractive index and permittivity and the normal incidence reflectivity have been calculated from the absorptivity. About three-quarters of the infrared contribution to the microwave refractive index is caused by the translational lattice vibrations and about 15% by the rotational vibrations; the O-H stretching bands which absorb very strongly contribute relatively little. The maximum of the density of states in the transverse acoustic branch is at 65/cm rather than below 50/cm as reported earlier. A theory of the contribution of the translational lattice vibrations to the microwave permittivity is given based on the theory of the absorption by orientationally disordered crystals given in an earlier paper. From the theory and the experimental measurements reported in this paper the dipole-moment derivative for the relative displacement of two water molecules in ice along their line of centers (or equivalently the effective charge of a water molecule) is about 0.3 electronic charges. (Author)
author2 ALBERTA UNIV EDMONTON DEPT OF CHEMISTRY
format Text
author Bertie,J. E.
Labbe,H. J.
Whalley,E.
author_facet Bertie,J. E.
Labbe,H. J.
Whalley,E.
author_sort Bertie,J. E.
title ABSORPTIVITY OF ICE I IN THE RANGE 4000-30/cm
title_short ABSORPTIVITY OF ICE I IN THE RANGE 4000-30/cm
title_full ABSORPTIVITY OF ICE I IN THE RANGE 4000-30/cm
title_fullStr ABSORPTIVITY OF ICE I IN THE RANGE 4000-30/cm
title_full_unstemmed ABSORPTIVITY OF ICE I IN THE RANGE 4000-30/cm
title_sort absorptivity of ice i in the range 4000-30/cm
publishDate 1968
url http://www.dtic.mil/docs/citations/AD0697594
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0697594
genre Ice
permafrost
genre_facet Ice
permafrost
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0697594
op_rights Availability: Pub. in Jnl. of Chemical Physics, v50 n10 p4501-4520, 15 May 69. No copies furnished.
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