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
- Institución
- Universidad Nacional de La Plata
- OAI Identificador
- oai:sedici.unlp.edu.ar:10915/131382
Ver los metadatos del registro completo
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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 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Articulo http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
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 |
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http://creativecommons.org/licenses/by-nc-sa/4.0/ Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0) |
dc.format.none.fl_str_mv |
application/pdf 531-540 |
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SEDICI (UNLP) - Universidad Nacional de La Plata |
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