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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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 |
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Open Polar |
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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 |
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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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1766027811268591616 |