{"id":109743,"date":"2019-06-02T18:53:56","date_gmt":"2019-06-02T16:53:56","guid":{"rendered":"https:\/\/www.geostru.eu\/masw\/"},"modified":"2019-10-08T18:28:52","modified_gmt":"2019-10-08T16:28:52","slug":"masw","status":"publish","type":"post","link":"https:\/\/www.geostru.eu\/es\/blog\/2019\/06\/02\/masw\/","title":{"rendered":"MASW"},"content":{"rendered":"<p style=\"text-align: justify\"><strong>MASW<\/strong> (Multichannel Analysis of Surface Waves) es una t\u00e9cnica de investigaci\u00f3n no invasiva que permite definir el perfil de velocidad de las ondas de corte vertical Vs bas\u00e1ndose en la medida de las ondas superficiales, obtenida mediante sensores colocados en la superficie del suelo. La mayor contribuci\u00f3n viene de las <a href=\"https:\/\/es.wikipedia.org\/wiki\/Onda_s\u00edsmica\" target=\"_blank\" rel=\"noopener\"><strong>ondas de Rayleigh<\/strong><\/a>, las cuales se transmiten a una velocidad correlacionada con la rigidez de la porci\u00f3n de terreno afectada por la propagaci\u00f3n de las ondas. En un medio estratificado, las ondas de Rayleigh son dispersivas, o sea ondas con diferentes longitudes de onda se propagan con diferentes velocidades de fase y velocidad de grupo. En otras palabras, la velocidad de fase (o de grupo) aparente de las ondas de <strong>Rayleigh<\/strong> depende de la frecuencia de propagaci\u00f3n, o sea son ondas cuya velocidad depende de la frecuencia. Con <strong>MASW<\/strong> es posible determinar el perfil de velocidad de las odas de corte Vs y por lo tanto el tipo de suelo s\u00edsmico (A, B, C, D, E). A diferencia de la s\u00edsmica de refracci\u00f3n, se usan en cualquier situaci\u00f3n estratigr\u00e1fica, incluso en presencia de nivel fre\u00e1tico.<\/p>\n<p style=\"text-align: justify\"><strong>Elaboraci\u00f3n de datos\u00a0<\/strong><br \/>\nEl an\u00e1lisis <strong>MASW<\/strong> se puede efectuar en cuatro fases:<\/p>\n<p style=\"text-align: justify\">\u2022 la primera fase es la transformaci\u00f3n de las series temporales en el dominio frecuencia f \u2013 n\u00famero de onda K;<\/p>\n<p style=\"text-align: justify\">\u2022 la segunda fase consiste en la identificar las parejas f-k cuyos m\u00e1ximos espectrales de energ\u00eda (densidad espectral) permiten trazar la curva de dispersi\u00f3n de las ondas de Rayleigh en el plano V fase (m\/sec) \u2013 frecuencia (lentitud (s\/m) \u2013 frecuencia (Hz)<\/p>\n<p style=\"text-align: justify\">\u2022 la tercera fase consiste en calcular la curva de dispersi\u00f3n te\u00f3rica mediante la formulaci\u00f3n del perfil de velocidad de las ondas de corte verticali Vs, modificando oportunamente el espesor h, las velocidades de las ondas de corte Vs y de compresi\u00f3n Vp, la densidad de masa \u03c1 de las capas que forman el modelo del suelo;<\/p>\n<p style=\"text-align: justify\">\u2022 la cuarta y \u00faltima fase consiste en modificar la curva te\u00f3rica hasta alcanzar la superposici\u00f3n \u00f3ptima entre la velocidad de fase (o curva de dispersi\u00f3n) experimental y la velocidad de fase (o curva de dispersi\u00f3n) num\u00e9rica correspondiente al modelo de suolo.<\/p>\n<p style=\"text-align: justify\"><a href=\"http:\/\/www.darioflaccovio.it\/geofisica-applicata\/208-onde-di-superficie-in-geofisica-applicata.html\" target=\"_blank\" rel=\"noopener\">Onde di superficie in geofisica applicata<\/a>\u00a0 <a href=\"https:\/\/www.geostru.eu\/es\/shop\/software-es\/geofisica-es\/easy-masw-multi-channel-analysis-surface-waves\/\" target=\"_blank\" rel=\"noopener\">EasyMasw (Interpretaci\u00f3n autom\u00e1tica de estudios MASW)<\/a><\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<p style=\"text-align: center\"><strong><span style=\"font-size: 14pt\"><a href=\"https:\/\/www.geostru.eu\/es\/shop\/software-es\/geofisica-es\/easy-masw-multi-channel-analysis-surface-waves\/\">SOFTWARE EASY MASW<\/a><\/span><\/strong><\/p>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>MASW (Multichannel Analysis of Surface Waves) es una t\u00e9cnica de investigaci\u00f3n no invasiva que permite definir el perfil de velocidad de las ondas de corte vertical Vs bas\u00e1ndose en la medida de las ondas superficiales, obtenida mediante sensores colocados en la superficie del suelo. La mayor contribuci\u00f3n viene de las ondas de Rayleigh, las cuales&hellip;<\/p>\n","protected":false},"author":216,"featured_media":109907,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[584,581,583],"tags":[],"class_list":["post-109743","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-articulos-publicaciones-geotecnica","category-articulos-ingenieria-civil","category-articulos-para-la-geologia","category-584","category-581","category-583","description-off"],"yoast_head":"<!-- This site is optimized with the Yoast SEO Premium plugin v25.0 (Yoast SEO v25.0) - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>MASW<\/title>\n<meta name=\"description\" content=\"MASW ((Multichannel Analysis of Surface Waves) \u00e8 una tecnica di indagine non invasiva che consente la definizione del profilo di velocit\u00e0\" \/>\n<meta name=\"robots\" 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In 1999 he founded GeoStru, an international geotechnical software house whose catalogue he largely authored: slope stability and rockfall analysis, foundations and retaining structures, finite element analysis, geophysics and site investigation, hydrology and hydrogeology, and reinforced concrete design. Since 2016 he has run SC Engsoft S.r.l. in Cluj-Napoca, Romania, and he is technical and scientific consultant to GoMeeting. His most recent work is GeoStru.ai, a platform delivering geotechnical and civil calculation through natural-language conversation while keeping the analysis itself on deterministic, auditable algorithms. Between 2005 and 2013 he co-supervised degree theses at the University of Calabria and the Mediterranea University of Reggio Calabria. He teaches accredited professional-development courses for geologists and engineers under accreditation from the Italian Consiglio Nazionale dei Geologi. 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