DISPERSION TABLES FOR RAYLEIGH WAVES ON A SINGLE SURFACE LAYER.

Tables are presented to show the dispersive characteristics for Rayleigh waves on a single elastic layer overlying a uniform elastic half-space. Two standard models are considered, each specified in terms of four parameters: Poisson's ratio in the layer and in the half-space, and the shear velo...

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Main Authors: Mooney, Harold M., Bolt, Bruce A.
Other Authors: MICHIGAN UNIV ANN ARBOR INST OF SCIENCE AND TECHNOLOGY
Format: Text
Language:English
Published: 1965
Subjects:
Online Access:http://www.dtic.mil/docs/citations/AD0473363
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0473363
id ftdtic:AD0473363
record_format openpolar
spelling ftdtic:AD0473363 2023-05-15T16:38:16+02:00 DISPERSION TABLES FOR RAYLEIGH WAVES ON A SINGLE SURFACE LAYER. Mooney, Harold M. Bolt, Bruce A. MICHIGAN UNIV ANN ARBOR INST OF SCIENCE AND TECHNOLOGY 1965-10 text/html http://www.dtic.mil/docs/citations/AD0473363 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0473363 en eng http://www.dtic.mil/docs/citations/AD0473363 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS (*SEISMIC WAVES TABLES(DATA)) SEISMOLOGY SCATTERING SURFACE PROPERTIES VELOCITY DETERMINANTS(MATHEMATICS) EARTH MODELS COMPRESSIVE PROPERTIES SHEAR STRESSES DENSITY DETECTION VELA UNIFORM Text 1965 ftdtic 2016-02-18T17:15:36Z Tables are presented to show the dispersive characteristics for Rayleigh waves on a single elastic layer overlying a uniform elastic half-space. Two standard models are considered, each specified in terms of four parameters: Poisson's ratio in the layer and in the half-space, and the shear velocity and density ratios. Each parameter is varied through eight values, holding the other three parameters constant. For each such structure, results are given for the fundamental Rayleigh mode and the first and second shear modes. The tables consist of 32 cases, for each of three modes, for each of the two standard models, or a total of 192 tables. A special computation procedure for group velocities is used which eliminates the errors associated with the usual finite-difference approximation. Auxiliary information includes a tabulation of long-period cutoff values as a function of structure parameters. To illustrate the results for specific geologic and laboratory models, 36 additional tables are given. These include results for a continental ice cap, a continental crust, a sedimentary basin, an alluvial overburden, various two-and three-dimensional seismic models, and a case selected from the literature. (Author) Text Ice cap 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 (*SEISMIC WAVES
TABLES(DATA))
SEISMOLOGY
SCATTERING
SURFACE PROPERTIES
VELOCITY
DETERMINANTS(MATHEMATICS)
EARTH MODELS
COMPRESSIVE PROPERTIES
SHEAR STRESSES
DENSITY
DETECTION
VELA UNIFORM
spellingShingle (*SEISMIC WAVES
TABLES(DATA))
SEISMOLOGY
SCATTERING
SURFACE PROPERTIES
VELOCITY
DETERMINANTS(MATHEMATICS)
EARTH MODELS
COMPRESSIVE PROPERTIES
SHEAR STRESSES
DENSITY
DETECTION
VELA UNIFORM
Mooney, Harold M.
Bolt, Bruce A.
DISPERSION TABLES FOR RAYLEIGH WAVES ON A SINGLE SURFACE LAYER.
topic_facet (*SEISMIC WAVES
TABLES(DATA))
SEISMOLOGY
SCATTERING
SURFACE PROPERTIES
VELOCITY
DETERMINANTS(MATHEMATICS)
EARTH MODELS
COMPRESSIVE PROPERTIES
SHEAR STRESSES
DENSITY
DETECTION
VELA UNIFORM
description Tables are presented to show the dispersive characteristics for Rayleigh waves on a single elastic layer overlying a uniform elastic half-space. Two standard models are considered, each specified in terms of four parameters: Poisson's ratio in the layer and in the half-space, and the shear velocity and density ratios. Each parameter is varied through eight values, holding the other three parameters constant. For each such structure, results are given for the fundamental Rayleigh mode and the first and second shear modes. The tables consist of 32 cases, for each of three modes, for each of the two standard models, or a total of 192 tables. A special computation procedure for group velocities is used which eliminates the errors associated with the usual finite-difference approximation. Auxiliary information includes a tabulation of long-period cutoff values as a function of structure parameters. To illustrate the results for specific geologic and laboratory models, 36 additional tables are given. These include results for a continental ice cap, a continental crust, a sedimentary basin, an alluvial overburden, various two-and three-dimensional seismic models, and a case selected from the literature. (Author)
author2 MICHIGAN UNIV ANN ARBOR INST OF SCIENCE AND TECHNOLOGY
format Text
author Mooney, Harold M.
Bolt, Bruce A.
author_facet Mooney, Harold M.
Bolt, Bruce A.
author_sort Mooney, Harold M.
title DISPERSION TABLES FOR RAYLEIGH WAVES ON A SINGLE SURFACE LAYER.
title_short DISPERSION TABLES FOR RAYLEIGH WAVES ON A SINGLE SURFACE LAYER.
title_full DISPERSION TABLES FOR RAYLEIGH WAVES ON A SINGLE SURFACE LAYER.
title_fullStr DISPERSION TABLES FOR RAYLEIGH WAVES ON A SINGLE SURFACE LAYER.
title_full_unstemmed DISPERSION TABLES FOR RAYLEIGH WAVES ON A SINGLE SURFACE LAYER.
title_sort dispersion tables for rayleigh waves on a single surface layer.
publishDate 1965
url http://www.dtic.mil/docs/citations/AD0473363
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0473363
genre Ice cap
genre_facet Ice cap
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0473363
op_rights APPROVED FOR PUBLIC RELEASE
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