Determination of seismograph constants from the calibration curve

Autores
Gershanik, Simón; Gershanik, Carlota
Año de publicación
1981
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The explicit expression of the long-period WWSSN calibration curve can be obtained solving the differential equations of the seismograph system in terms of ew and identifying the characteristic equation to a product of polynomials of the second degree. The coefficients of these polynomials are the equivalent constants. These and a scale factor can be obtained from the calibration curve. The frequency response of the seismograph system is fully determined by these elements provided that the reduced motor constant and the calibration current are known. The explicit knowledge of the seismograph partial constants is not necessary. Newton-Raphson's method is generally efficient to obtain the elements from the calibration curve, but it may fail some times. Levenberg's method (slightly modified) and also simple step reduction can be helpful in such cases. The unknowns can be obtained either freely or under the constraint that some of the partial constants have the values assigned to them. The latter may be convenient when the behavior of parts of the system is affected by some trouble.
Facultad de Ciencias Astronómicas y Geofísicas
Materia
Geofísica
Calibration
Instruments
Mathematical models
Seismographs
Seismology
Theoretical studies
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/licenses/by-nc-sa/4.0/
Repositorio
SEDICI (UNLP)
Institución
Universidad Nacional de La Plata
OAI Identificador
oai:sedici.unlp.edu.ar:10915/131382

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network_name_str SEDICI (UNLP)
spelling Determination of seismograph constants from the calibration curveGershanik, SimónGershanik, CarlotaGeofísicaCalibrationInstrumentsMathematical modelsSeismographsSeismologyTheoretical studiesThe explicit expression of the long-period WWSSN calibration curve can be obtained solving the differential equations of the seismograph system in terms of ew and identifying the characteristic equation to a product of polynomials of the second degree. The coefficients of these polynomials are the equivalent constants. These and a scale factor can be obtained from the calibration curve. The frequency response of the seismograph system is fully determined by these elements provided that the reduced motor constant and the calibration current are known. The explicit knowledge of the seismograph partial constants is not necessary. Newton-Raphson's method is generally efficient to obtain the elements from the calibration curve, but it may fail some times. Levenberg's method (slightly modified) and also simple step reduction can be helpful in such cases. The unknowns can be obtained either freely or under the constraint that some of the partial constants have the values assigned to them. The latter may be convenient when the behavior of parts of the system is affected by some trouble.Facultad de Ciencias Astronómicas y Geofísicas1981info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionArticulohttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdf531-540http://sedici.unlp.edu.ar/handle/10915/131382enginfo:eu-repo/semantics/altIdentifier/issn/0037-1106info:eu-repo/semantics/altIdentifier/issn/1943-3573info:eu-repo/semantics/altIdentifier/doi/10.1785/bssa0710020531info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc-sa/4.0/Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2025-09-29T11:31:48Zoai:sedici.unlp.edu.ar:10915/131382Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-09-29 11:31:48.336SEDICI (UNLP) - Universidad Nacional de La Platafalse
dc.title.none.fl_str_mv Determination of seismograph constants from the calibration curve
title Determination of seismograph constants from the calibration curve
spellingShingle Determination of seismograph constants from the calibration curve
Gershanik, Simón
Geofísica
Calibration
Instruments
Mathematical models
Seismographs
Seismology
Theoretical studies
title_short Determination of seismograph constants from the calibration curve
title_full Determination of seismograph constants from the calibration curve
title_fullStr Determination of seismograph constants from the calibration curve
title_full_unstemmed Determination of seismograph constants from the calibration curve
title_sort Determination of seismograph constants from the calibration curve
dc.creator.none.fl_str_mv Gershanik, Simón
Gershanik, Carlota
author Gershanik, Simón
author_facet Gershanik, Simón
Gershanik, Carlota
author_role author
author2 Gershanik, Carlota
author2_role author
dc.subject.none.fl_str_mv Geofísica
Calibration
Instruments
Mathematical models
Seismographs
Seismology
Theoretical studies
topic Geofísica
Calibration
Instruments
Mathematical models
Seismographs
Seismology
Theoretical studies
dc.description.none.fl_txt_mv The explicit expression of the long-period WWSSN calibration curve can be obtained solving the differential equations of the seismograph system in terms of ew and identifying the characteristic equation to a product of polynomials of the second degree. The coefficients of these polynomials are the equivalent constants. These and a scale factor can be obtained from the calibration curve. The frequency response of the seismograph system is fully determined by these elements provided that the reduced motor constant and the calibration current are known. The explicit knowledge of the seismograph partial constants is not necessary. Newton-Raphson's method is generally efficient to obtain the elements from the calibration curve, but it may fail some times. Levenberg's method (slightly modified) and also simple step reduction can be helpful in such cases. The unknowns can be obtained either freely or under the constraint that some of the partial constants have the values assigned to them. The latter may be convenient when the behavior of parts of the system is affected by some trouble.
Facultad de Ciencias Astronómicas y Geofísicas
description The explicit expression of the long-period WWSSN calibration curve can be obtained solving the differential equations of the seismograph system in terms of ew and identifying the characteristic equation to a product of polynomials of the second degree. The coefficients of these polynomials are the equivalent constants. These and a scale factor can be obtained from the calibration curve. The frequency response of the seismograph system is fully determined by these elements provided that the reduced motor constant and the calibration current are known. The explicit knowledge of the seismograph partial constants is not necessary. Newton-Raphson's method is generally efficient to obtain the elements from the calibration curve, but it may fail some times. Levenberg's method (slightly modified) and also simple step reduction can be helpful in such cases. The unknowns can be obtained either freely or under the constraint that some of the partial constants have the values assigned to them. The latter may be convenient when the behavior of parts of the system is affected by some trouble.
publishDate 1981
dc.date.none.fl_str_mv 1981
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info:eu-repo/semantics/publishedVersion
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format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://sedici.unlp.edu.ar/handle/10915/131382
url http://sedici.unlp.edu.ar/handle/10915/131382
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/issn/0037-1106
info:eu-repo/semantics/altIdentifier/issn/1943-3573
info:eu-repo/semantics/altIdentifier/doi/10.1785/bssa0710020531
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by-nc-sa/4.0/
Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)
eu_rights_str_mv openAccess
rights_invalid_str_mv http://creativecommons.org/licenses/by-nc-sa/4.0/
Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)
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531-540
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repository.name.fl_str_mv SEDICI (UNLP) - Universidad Nacional de La Plata
repository.mail.fl_str_mv alira@sedici.unlp.edu.ar
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