{"id":464,"date":"2017-06-02T17:38:53","date_gmt":"2017-06-02T17:38:53","guid":{"rendered":"https:\/\/www.zuloaga.online\/ignacio\/?p=464"},"modified":"2023-05-31T17:40:41","modified_gmt":"2023-05-31T17:40:41","slug":"geofisica-clasificar-el-terreno-para-diseno-sismico-remi-masw","status":"publish","type":"post","link":"https:\/\/www.zuloaga.online\/ignacio\/geofisica-clasificar-el-terreno-para-diseno-sismico-remi-masw\/","title":{"rendered":"Geofi\u0301sica &#8211; Clasificar el Terreno para Dise\u00f1o S\u00edsmico &#8211; ReMi &#8211; MASW"},"content":{"rendered":"<p>\u00bfc\u00f3mo clasificar el terreno, para el dise\u00f1o s\u00edsmico?<\/p>\n<p>El M\u00e9todo de Refracci\u00f3n Microtremor (ReMi) es un m\u00e9todo, relativamente nuevo, para mediciones in situ de perfiles de velocidad de ondas de corte Vs usando registros de ruido ambiental. Pudi\u00e9ndose generar un perfil del subsuelo 1-D bas\u00e1ndose en la velocidad con la profundidad.<\/p>\n<p>Para la adquisici\u00f3n de datos se usa un sism\u00f3grafo convencional y ge\u00f3fonos verticales equidistantes de onda P usados en estudios de refracci\u00f3n.<\/p>\n<p>Esta t\u00e9cnica esta basada en dos planteamientos. El primero es que el equipo de adquisici\u00f3n de refracci\u00f3n s\u00edsmica aporta una salida casi id\u00e9ntica a la s\u00edsmica de refracci\u00f3n de la onda P, adem\u00e1s puede efectivamente grabar ondas superficiales a frecuencias tan bajas como de 2 Hz.<\/p>\n<p>El segundo planteamiento es que se pueden separar las ondas Rayleigh de otras ondas registradas por el equipo, por lo que es posible reconocer la verdadera fase de velocidad de otras velocidades aparentes. Esto hace posible un an\u00e1lisis espectral de ondas de superficies (SASW) y una efectiva t\u00e9cnica de an\u00e1lisis multicanales de ondas de superficies (MASW).<\/p>\n<p style=\"text-align: center;\"><iframe src=\"https:\/\/drive.google.com\/file\/d\/16r_JE39psIrkr1NZo6oYoy-IhQNQik1P\/preview\" width=\"640\" height=\"480\"><\/iframe><\/p>\n","protected":false},"excerpt":{"rendered":"<p>\u00bfc\u00f3mo clasificar el terreno, para el dise\u00f1o s\u00edsmico? El M\u00e9todo de Refracci\u00f3n Microtremor (ReMi) es un m\u00e9todo, relativamente nuevo, para mediciones in situ de perfiles de velocidad de ondas de corte Vs usando registros de ruido ambiental. Pudi\u00e9ndose generar un perfil del subsuelo 1-D bas\u00e1ndose en la velocidad con la profundidad. Para la adquisici\u00f3n de [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"video","meta":{"site-sidebar-layout":"default","site-content-layout":"default","ast-site-content-layout":"default","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"default","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"footnotes":""},"categories":[46,7,10],"tags":[],"class_list":["post-464","post","type-post","status-publish","format-video","hentry","category-geofisica","category-geotecnia","category-geotecnia-online","post_format-post-format-video"],"_links":{"self":[{"href":"https:\/\/www.zuloaga.online\/ignacio\/wp-json\/wp\/v2\/posts\/464","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.zuloaga.online\/ignacio\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.zuloaga.online\/ignacio\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.zuloaga.online\/ignacio\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.zuloaga.online\/ignacio\/wp-json\/wp\/v2\/comments?post=464"}],"version-history":[{"count":2,"href":"https:\/\/www.zuloaga.online\/ignacio\/wp-json\/wp\/v2\/posts\/464\/revisions"}],"predecessor-version":[{"id":466,"href":"https:\/\/www.zuloaga.online\/ignacio\/wp-json\/wp\/v2\/posts\/464\/revisions\/466"}],"wp:attachment":[{"href":"https:\/\/www.zuloaga.online\/ignacio\/wp-json\/wp\/v2\/media?parent=464"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.zuloaga.online\/ignacio\/wp-json\/wp\/v2\/categories?post=464"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.zuloaga.online\/ignacio\/wp-json\/wp\/v2\/tags?post=464"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}