Measurements of Ultrasonic Wave Velocities in Ice Cores from Greenland and Antarctica.

Detailed ultrasonic velocity measurements were made on snow and ice cores from Greenland and Antarctica in order to study velocity anisotropy and its relationship to the petrofabric analysis of these cores. In addition, ultrasonic velocities were measured in the near-surface snow layers at Byrd Stat...

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Bibliographic Details
Main Author: Bennett,Hugh F.
Other Authors: MICHIGAN STATE UNIV EAST LANSING DEPT OF GEOLOGY
Format: Text
Language:English
Published: 1972
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/AD0745904
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0745904
id ftdtic:AD0745904
record_format openpolar
spelling ftdtic:AD0745904 2023-05-15T14:03:11+02:00 Measurements of Ultrasonic Wave Velocities in Ice Cores from Greenland and Antarctica. Bennett,Hugh F. MICHIGAN STATE UNIV EAST LANSING DEPT OF GEOLOGY 1972-06 text/html http://www.dtic.mil/docs/citations/AD0745904 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0745904 en eng http://www.dtic.mil/docs/citations/AD0745904 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost (*ICE ULTRASONIC RADIATION) SEISMIC WAVES GREENLAND ANTARCTIC REGIONS ANISOTROPY STRUCTURAL GEOLOGY PACK ICE ACOUSTIC VELOCITY LAND ICE Text 1972 ftdtic 2016-02-19T01:52:05Z Detailed ultrasonic velocity measurements were made on snow and ice cores from Greenland and Antarctica in order to study velocity anisotropy and its relationship to the petrofabric analysis of these cores. In addition, ultrasonic velocities were measured in the near-surface snow layers at Byrd Station and South Pole Station, Antarctica, to provide a detailed velocity profile in the region of the ice sheet where the velocity is greatly influenced by the snow structure. The experimental arrangement, including the design of equipment, measurement errors, techniques, and problems encountered in the study, is discussed. The theory of wave propagation in a general anisotropic medium is reviewed and a detailed presentation of this theory, concerning transversely isotropic media, is given. A method is developed for calculating a theoretical velocity model from the petrofabric analysis of the ice cores, thus providing a means of testing the theory with field and laboratory observations. (Author) Text Antarc* Antarctic Antarctica Greenland Ice Ice Sheet permafrost South pole South pole Defense Technical Information Center: DTIC Technical Reports database Antarctic Byrd Byrd Station ENVELOPE(-119.533,-119.533,-80.017,-80.017) Greenland South Pole
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Snow
Ice and Permafrost
(*ICE
ULTRASONIC RADIATION)
SEISMIC WAVES
GREENLAND
ANTARCTIC REGIONS
ANISOTROPY
STRUCTURAL GEOLOGY
PACK ICE
ACOUSTIC VELOCITY
LAND ICE
spellingShingle Snow
Ice and Permafrost
(*ICE
ULTRASONIC RADIATION)
SEISMIC WAVES
GREENLAND
ANTARCTIC REGIONS
ANISOTROPY
STRUCTURAL GEOLOGY
PACK ICE
ACOUSTIC VELOCITY
LAND ICE
Bennett,Hugh F.
Measurements of Ultrasonic Wave Velocities in Ice Cores from Greenland and Antarctica.
topic_facet Snow
Ice and Permafrost
(*ICE
ULTRASONIC RADIATION)
SEISMIC WAVES
GREENLAND
ANTARCTIC REGIONS
ANISOTROPY
STRUCTURAL GEOLOGY
PACK ICE
ACOUSTIC VELOCITY
LAND ICE
description Detailed ultrasonic velocity measurements were made on snow and ice cores from Greenland and Antarctica in order to study velocity anisotropy and its relationship to the petrofabric analysis of these cores. In addition, ultrasonic velocities were measured in the near-surface snow layers at Byrd Station and South Pole Station, Antarctica, to provide a detailed velocity profile in the region of the ice sheet where the velocity is greatly influenced by the snow structure. The experimental arrangement, including the design of equipment, measurement errors, techniques, and problems encountered in the study, is discussed. The theory of wave propagation in a general anisotropic medium is reviewed and a detailed presentation of this theory, concerning transversely isotropic media, is given. A method is developed for calculating a theoretical velocity model from the petrofabric analysis of the ice cores, thus providing a means of testing the theory with field and laboratory observations. (Author)
author2 MICHIGAN STATE UNIV EAST LANSING DEPT OF GEOLOGY
format Text
author Bennett,Hugh F.
author_facet Bennett,Hugh F.
author_sort Bennett,Hugh F.
title Measurements of Ultrasonic Wave Velocities in Ice Cores from Greenland and Antarctica.
title_short Measurements of Ultrasonic Wave Velocities in Ice Cores from Greenland and Antarctica.
title_full Measurements of Ultrasonic Wave Velocities in Ice Cores from Greenland and Antarctica.
title_fullStr Measurements of Ultrasonic Wave Velocities in Ice Cores from Greenland and Antarctica.
title_full_unstemmed Measurements of Ultrasonic Wave Velocities in Ice Cores from Greenland and Antarctica.
title_sort measurements of ultrasonic wave velocities in ice cores from greenland and antarctica.
publishDate 1972
url http://www.dtic.mil/docs/citations/AD0745904
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0745904
long_lat ENVELOPE(-119.533,-119.533,-80.017,-80.017)
geographic Antarctic
Byrd
Byrd Station
Greenland
South Pole
geographic_facet Antarctic
Byrd
Byrd Station
Greenland
South Pole
genre Antarc*
Antarctic
Antarctica
Greenland
Ice
Ice Sheet
permafrost
South pole
South pole
genre_facet Antarc*
Antarctic
Antarctica
Greenland
Ice
Ice Sheet
permafrost
South pole
South pole
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0745904
op_rights APPROVED FOR PUBLIC RELEASE
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