Frequencies and predominant periods of earthquakes registered in the city of Tacna, by means of analysis and Fourier spectrum

Descripción del Articulo

The city of Tacna is in seismic silence, waiting for a large earthquake and the environmental effects that this causes. The objective of the investigation was to determine the prevailing frequencies and periods of some earthquakes registered in the city of Tacna, using the Fourier analysis and spect...

Descripción completa

Detalles Bibliográficos
Autores: Mendoza Ramirez, Wilber, Cotrado Flores, Dina Marlene, Ticahuanca Mamani, Joel, Mendoza Chura, Arleth
Formato: artículo
Fecha de Publicación:2020
Institución:Universidad Privada de Tacna
Repositorio:Revistas - Universidad Privada de Tacna
Lenguaje:español
OAI Identifier:oai:revistas.upt.edu.pe:article/288
Enlace del recurso:https://revistas.upt.edu.pe/ojs/index.php/ingenieria/article/view/288
Nivel de acceso:acceso abierto
Materia:Dominio de la frecuencia
frecuencia predominante
fuentes sismogénicas
resonancia
Frequency domain
predominant frequency
seismogenic sources
resonance
Descripción
Sumario:The city of Tacna is in seismic silence, waiting for a large earthquake and the environmental effects that this causes. The objective of the investigation was to determine the prevailing frequencies and periods of some earthquakes registered in the city of Tacna, using the Fourier analysis and spectrum. Earthquakes of the present century, of a magnitude greater than 5.0 Mw and from different near, intermediate and distant seismogenic sources were selected. The research used the Fourier mathematical model to process seismic signals, from the time domain to the frequency domain, then, the prevailing frequencies and periods of the different signals were analyzed and learned. For better signal processing, a code was created in Matlab to perform the calculations, which were then verified using the Seismosignal software. The predominant frequencies of earthquakes from close sources vary from 2.12 to 11.43 Hz (predominant periods from 0.09 to 0.47 s); earthquakes of intermediate source, vary from 5.15 to 11.29 Hz (predominant periods from 0.09 to 0.19 s); and earthquakes from distant sources, vary from 0.43 to 6.06 Hz (predominant periods from 0.17 to 2.34 s). As most of the earthquakes had predominantly short periods, these could generate resonance phenomena to structures with periods of vibration less than 0.5 s.
Nota importante:
La información contenida en este registro es de entera responsabilidad de la institución que gestiona el repositorio institucional donde esta contenido este documento o set de datos. El CONCYTEC no se hace responsable por los contenidos (publicaciones y/o datos) accesibles a través del Repositorio Nacional Digital de Ciencia, Tecnología e Innovación de Acceso Abierto (ALICIA).