{"id":1481,"date":"2021-08-08T11:26:05","date_gmt":"2021-08-08T11:26:05","guid":{"rendered":"https:\/\/geo-webonline.com\/?page_id=1481"},"modified":"2025-04-07T01:16:10","modified_gmt":"2025-04-07T01:16:10","slug":"el-efecto-del-agua-en-los-taludes","status":"publish","type":"page","link":"https:\/\/geo-webonline.com\/en\/el-efecto-del-agua-en-los-taludes\/","title":{"rendered":"The effect of water in slopes"},"content":{"rendered":"\t\t<div data-elementor-type=\"wp-page\" data-elementor-id=\"1481\" class=\"elementor elementor-1481\" data-elementor-post-type=\"page\">\n\t\t\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-a53acd5 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"a53acd5\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 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elementor-section-height-min-height elementor-hidden-desktop elementor-section-height-default elementor-section-items-middle\" data-id=\"b61b062\" data-element_type=\"section\" data-e-type=\"section\" data-settings=\"{&quot;background_background&quot;:&quot;gradient&quot;}\">\n\t\t\t\t\t\t\t<div class=\"elementor-background-overlay\"><\/div>\n\t\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-50 elementor-top-column elementor-element elementor-element-f282456\" data-id=\"f282456\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-0497d08 elementor-widget__width-initial elementor-absolute elementor-widget-mobile__width-initial elementor-hidden-desktop elementor-widget elementor-widget-image\" data-id=\"0497d08\" data-element_type=\"widget\" data-e-type=\"widget\" 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data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap\">\n\t\t\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-bc3b770 elementor-hidden-desktop elementor-hidden-tablet elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"bc3b770\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-5a4fec3\" data-id=\"5a4fec3\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-814f4ac elementor-nav-menu__align-center elementor-nav-menu--dropdown-tablet elementor-nav-menu__text-align-aside 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tabindex=\"-1\">geo-info<\/a>\n<ul class=\"sub-menu elementor-nav-menu--dropdown\">\n\t<li class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-1169\"><a href=\"https:\/\/geo-webonline.com\/en\/fundaciones-2\/\" class=\"elementor-sub-item\" tabindex=\"-1\">Fundaciones<\/a><\/li>\n\t<li class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-386\"><a href=\"https:\/\/geo-webonline.com\/en\/mecanica-de-suelos\/\" class=\"elementor-sub-item\" tabindex=\"-1\">Mec\u00e1nica de Suelos<\/a><\/li>\n\t<li class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-387\"><a href=\"https:\/\/geo-webonline.com\/en\/muros\/\" class=\"elementor-sub-item\" tabindex=\"-1\">Muros<\/a><\/li>\n\t<li class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-383\"><a href=\"https:\/\/geo-webonline.com\/en\/estabilidad-de-talues\/\" class=\"elementor-sub-item\" tabindex=\"-1\">Estabilidad de Taludes<\/a><\/li>\n\t<li class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-381\"><a href=\"https:\/\/geo-webonline.com\/en\/aguas-subterraneas\/\" class=\"elementor-sub-item\" tabindex=\"-1\">Aguas Subterraneas<\/a><\/li>\n\t<li class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-388\"><a href=\"https:\/\/geo-webonline.com\/en\/topicos-especiales\/\" class=\"elementor-sub-item\" tabindex=\"-1\">T\u00f3picos Especiales<\/a><\/li>\n\t<li class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-4247\"><a href=\"https:\/\/geo-webonline.com\/en\/terremoto-en-venezuela\/\" class=\"elementor-sub-item\" tabindex=\"-1\">Terremoto en Venezuela<\/a><\/li>\n<\/ul>\n<\/li>\n<li class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-1166\"><a href=\"https:\/\/geo-webonline.com\/en\/e-learning\/\" class=\"elementor-item\" tabindex=\"-1\">E-learning<\/a><\/li>\n<li class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-2318\"><a href=\"https:\/\/geo-webonline.com\/en\/servicios-de-consultoria\/\" class=\"elementor-item\" tabindex=\"-1\">Servicios de consultor\u00eda<\/a><\/li>\n<li class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-3224\"><a href=\"https:\/\/geo-webonline.com\/en\/proyecto-geotecnico\/\" class=\"elementor-item\" tabindex=\"-1\">Proyectos geot\u00e9cnicos<\/a><\/li>\n<li class=\"menu-item menu-item-type-post_type menu-item-object-page menu-item-1168\"><a href=\"https:\/\/geo-webonline.com\/en\/contacto\/\" class=\"elementor-item\" tabindex=\"-1\">Contacto<\/a><\/li>\n<\/ul>\t\t\t<\/nav>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-06ca7a3 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"06ca7a3\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-3149c7e\" data-id=\"3149c7e\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-603670a elementor-widget elementor-widget-heading\" data-id=\"603670a\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<h2 class=\"elementor-heading-title elementor-size-default\">El efecto del agua en los taludes<\/h2>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-1edb722 elementor-section-full_width elementor-section-height-default elementor-section-height-default\" data-id=\"1edb722\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-8943746\" data-id=\"8943746\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-e3c126e elementor-widget elementor-widget-text-editor\" data-id=\"e3c126e\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p><em>El agua est\u00e1 normalmente asociada a la mayor\u00eda de los mecanismos de falla que puede experimentar un talud. Desde varios tipos de carga que incrementan los esfuerzos actuantes en el talud, hasta la disminuci\u00f3n de la resistencia al corte del terreno, el agua aparece como un factor fundamental a considerar en cualquier an\u00e1lisis de estabilidad.<\/em><\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-655aa9f elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"655aa9f\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-782ff24\" data-id=\"782ff24\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-c64ac1b elementor-toc--minimized-on-tablet elementor-widget elementor-widget-table-of-contents\" data-id=\"c64ac1b\" data-element_type=\"widget\" data-e-type=\"widget\" data-settings=\"{&quot;headings_by_tags&quot;:[&quot;h3&quot;],&quot;exclude_headings_by_selector&quot;:[],&quot;no_headings_message&quot;:&quot;No headings were found on this page.&quot;,&quot;marker_view&quot;:&quot;numbers&quot;,&quot;minimize_box&quot;:&quot;yes&quot;,&quot;minimized_on&quot;:&quot;tablet&quot;,&quot;hierarchical_view&quot;:&quot;yes&quot;,&quot;min_height&quot;:{&quot;unit&quot;:&quot;px&quot;,&quot;size&quot;:&quot;&quot;,&quot;sizes&quot;:[]},&quot;min_height_tablet&quot;:{&quot;unit&quot;:&quot;px&quot;,&quot;size&quot;:&quot;&quot;,&quot;sizes&quot;:[]},&quot;min_height_mobile&quot;:{&quot;unit&quot;:&quot;px&quot;,&quot;size&quot;:&quot;&quot;,&quot;sizes&quot;:[]}}\" data-widget_type=\"table-of-contents.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<div class=\"elementor-toc__header\">\n\t\t\t\t\t\t<h4 class=\"elementor-toc__header-title\">\n\t\t\t\tContenidos\t\t\t<\/h4>\n\t\t\t\t\t\t\t\t\t\t<div class=\"elementor-toc__toggle-button elementor-toc__toggle-button--expand\" role=\"button\" tabindex=\"0\" aria-controls=\"elementor-toc__c64ac1b\" aria-expanded=\"true\" aria-label=\"Open table of contents\"><i aria-hidden=\"true\" class=\"fas fa-chevron-down\"><\/i><\/div>\n\t\t\t\t<div class=\"elementor-toc__toggle-button elementor-toc__toggle-button--collapse\" role=\"button\" tabindex=\"0\" aria-controls=\"elementor-toc__c64ac1b\" aria-expanded=\"true\" aria-label=\"Close table of contents\"><i aria-hidden=\"true\" class=\"fas fa-chevron-up\"><\/i><\/div>\n\t\t\t\t\t<\/div>\n\t\t\t\t<div id=\"elementor-toc__c64ac1b\" class=\"elementor-toc__body\">\n\t\t\t<div class=\"elementor-toc__spinner-container\">\n\t\t\t\t<i class=\"elementor-toc__spinner eicon-animation-spin eicon-loading\" aria-hidden=\"true\"><\/i>\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-6f43947 elementor-section-full_width elementor-section-height-default elementor-section-height-default\" data-id=\"6f43947\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-4ef3c4c\" data-id=\"4ef3c4c\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-ee92cf9 elementor-widget elementor-widget-heading\" data-id=\"ee92cf9\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<h3 class=\"elementor-heading-title elementor-size-default\">El agua <\/h3>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-295da21 elementor-section-full_width elementor-section-height-default elementor-section-height-default\" data-id=\"295da21\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-4eaea31\" data-id=\"4eaea31\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-08ae90d elementor-widget elementor-widget-text-editor\" data-id=\"08ae90d\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p>Cuando tratamos problemas relacionados con el suelo en general, constantemente mencionamos al agua. Pero, \u00bfqu\u00e9 es el agua? \u00bfcu\u00e1les son sus propiedades?<\/p><p>\u00a0<\/p><p>El agua es, ante todo, un <em>compuesto qu\u00edmico<\/em>, el cual tiene una estructura at\u00f3mica tal, que los \u00e1tomos de hidr\u00f3geno forman un \u00e1ngulo aproximado de 105\u00b0 entre las rectas que unen sus centros con el \u00e1tomo de ox\u00edgeno, lo cual le confiere la propiedad de <em>bipolaridad<\/em>. La Figura 1 muestra un esquema de la mol\u00e9cula de este compuesto.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-89040b9 elementor-section-full_width elementor-section-height-default elementor-section-height-default\" data-id=\"89040b9\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-a063ce4\" data-id=\"a063ce4\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-f73437b elementor-widget elementor-widget-image\" data-id=\"f73437b\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<img decoding=\"async\" width=\"1209\" height=\"627\" src=\"https:\/\/geo-webonline.com\/wp-content\/uploads\/2021\/08\/Figura-1-2.jpg\" class=\"attachment-full size-full wp-image-1483\" alt=\"\" srcset=\"https:\/\/geo-webonline.com\/wp-content\/uploads\/2021\/08\/Figura-1-2.jpg 1209w, https:\/\/geo-webonline.com\/wp-content\/uploads\/2021\/08\/Figura-1-2-300x156.jpg 300w, https:\/\/geo-webonline.com\/wp-content\/uploads\/2021\/08\/Figura-1-2-1024x531.jpg 1024w, https:\/\/geo-webonline.com\/wp-content\/uploads\/2021\/08\/Figura-1-2-768x398.jpg 768w\" sizes=\"(max-width: 1209px) 100vw, 1209px\" \/>\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-c81c9eb elementor-section-full_width elementor-section-height-default elementor-section-height-default\" data-id=\"c81c9eb\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-366237e\" data-id=\"366237e\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-2bcab5a elementor-widget elementor-widget-text-editor\" data-id=\"2bcab5a\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p><a href=\"https:\/\/www.renovablesverdes.com\/molecula-de-agua\/\"><strong>Figura 1 <\/strong>Mol\u00e9cula de agua\u00a0<\/a><\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-bb508ba elementor-section-full_width elementor-section-height-default elementor-section-height-default\" data-id=\"bb508ba\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-787d0f7\" data-id=\"787d0f7\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-0308db8 elementor-widget elementor-widget-text-editor\" data-id=\"0308db8\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p>El hecho de que el agua sea una mol\u00e9cula bipolar, implica que la misma sea similar a un peque\u00f1o im\u00e1n que puede orientarse de acuerdo al campo magn\u00e9tico; y por lo tanto es la que permite que reaccione junto a otros elementos qu\u00edmicos, generando, por ejemplo, la expansi\u00f3n de las arcillas.<\/p><p>\u00a0<\/p><p>Adicionalmente, dadas sus propiedades f\u00edsicas, el agua es un disolvente de amplio espectro, adem\u00e1s de ser la sustancia m\u00e1s abundante de la corteza terrestre, y la \u00fanica que se encuentra en los estados s\u00f3lido, l\u00edquido y gaseoso. El ciclo del agua (<a href=\"https:\/\/geo-webonline.com\/el-ciclo-hidrologico\/\">que hemos descrito en el post \u201c\u00bfDe d\u00f3nde viene el agua? El ciclo hidrol\u00f3gico\u201d<\/a>) describe la presencia y el movimiento del agua en la Tierra. Puede ser de utilidad echarle un vistazo.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-0a4d3d6 elementor-section-full_width elementor-section-height-default elementor-section-height-default\" data-id=\"0a4d3d6\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-0211384\" data-id=\"0211384\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-a40f075 elementor-widget elementor-widget-heading\" data-id=\"a40f075\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<h3 class=\"elementor-heading-title elementor-size-default\">El s\u00f3lido como medio poroso<\/h3>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-06e15c2 elementor-section-full_width elementor-section-height-default elementor-section-height-default\" data-id=\"06e15c2\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-125de8e\" data-id=\"125de8e\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-49212cb elementor-widget elementor-widget-text-editor\" data-id=\"49212cb\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p>\u00bfQu\u00e9 condici\u00f3n debe cumplir el suelo para poder interactuar con el agua? Para que un s\u00f3lido contenga agua debe ser necesariamente <em>poroso<\/em>, es decir, que debe contener espacios que puedan ser ocupados por agua.<\/p><p>\u00a0<\/p><p>La porosidad se define usualmente como la relaci\u00f3n entre los espacios \u201cvac\u00edos\u201d (o sea, no s\u00f3lidos) y el volumen total. Sin embargo, este concepto puede ser enga\u00f1oso, tal como se desprende del an\u00e1lisis de la Figura 2.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-3a077ac elementor-section-full_width elementor-section-height-default elementor-section-height-default\" data-id=\"3a077ac\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-2abcb8b\" data-id=\"2abcb8b\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-6abb50f elementor-widget elementor-widget-image\" data-id=\"6abb50f\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<img decoding=\"async\" width=\"1209\" height=\"627\" src=\"https:\/\/geo-webonline.com\/wp-content\/uploads\/2021\/08\/Figura-2-1.jpg\" class=\"attachment-full size-full wp-image-1488\" alt=\"\" srcset=\"https:\/\/geo-webonline.com\/wp-content\/uploads\/2021\/08\/Figura-2-1.jpg 1209w, https:\/\/geo-webonline.com\/wp-content\/uploads\/2021\/08\/Figura-2-1-300x156.jpg 300w, https:\/\/geo-webonline.com\/wp-content\/uploads\/2021\/08\/Figura-2-1-1024x531.jpg 1024w, https:\/\/geo-webonline.com\/wp-content\/uploads\/2021\/08\/Figura-2-1-768x398.jpg 768w\" sizes=\"(max-width: 1209px) 100vw, 1209px\" \/>\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-c7f42da elementor-section-full_width elementor-section-height-default elementor-section-height-default\" data-id=\"c7f42da\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-3ee8124\" data-id=\"3ee8124\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-cad76d3 elementor-widget elementor-widget-text-editor\" data-id=\"cad76d3\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p><strong>Figura 2 <\/strong>Diferentes tipos de porosidad<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-c767a2a elementor-section-full_width elementor-section-height-default elementor-section-height-default\" data-id=\"c767a2a\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-84750ae\" data-id=\"84750ae\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-cd60e51 elementor-widget elementor-widget-text-editor\" data-id=\"cd60e51\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p>En la mencionada figura se presentan cinco (5) materiales con porosidad similar. En el caso de la roca vacuolar (en la cual cada poro es independiente de otro), si \u00e9sta contiene alg\u00fan fluido, dicho fluido debe haberse formado al mismo tiempo que la roca. Para el caso de suelos granulares, los poros est\u00e1n interconectados, y por ende se deduce que se formaron al mismo tiempo que la fase s\u00f3lida. La roca fracturada, por su parte, puede mostrar fracturas interconectadas entre s\u00ed, o bien poros que no est\u00e1n conectados, dado que se formaron posteriormente a la roca. Finalmente, las arcillas francas no poseen poros propiamente dichos, aun cuando se porosidad se mide por la cantidad de agua que absorbe por unidad de volumen. En este caso, el agua, mediante un proceso f\u00edsico-qu\u00edmico y por ser un diel\u00e9ctrico, se abre espacio para penetrar entre los cristales laminados de arcilla, raz\u00f3n por la cual toda arcilla es expansiva ante la presencia de agua.<\/p><p>\u00a0<\/p><p>De acuerdo a lo anterior, es evidente la existencia de varios tipos de porosidad, siendo la m\u00e1s importante para la interacci\u00f3n terreno-agua aquella relacionada con la circulaci\u00f3n de agua entre el material, es decir, la llamada <em>porosidad efectiva<\/em>.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-4322d84 elementor-section-full_width elementor-section-height-default elementor-section-height-default\" data-id=\"4322d84\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-fe99bb7\" data-id=\"fe99bb7\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-129a2f5 elementor-widget elementor-widget-heading\" data-id=\"129a2f5\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<h3 class=\"elementor-heading-title elementor-size-default\">Principales efectos del agua en taludes<\/h3>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-e833a95 elementor-section-full_width elementor-section-height-default elementor-section-height-default\" data-id=\"e833a95\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-16c5479\" data-id=\"16c5479\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-3042459 elementor-widget elementor-widget-text-editor\" data-id=\"3042459\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p>La mayor\u00eda de las fallas de los taludes est\u00e1n relacionadas, de una forma u otra, con el agua, ya que \u00e9sta juega un papel muy importante en la mayor\u00eda de los procesos que generan, o bien una disminuci\u00f3n de la resistencia al corte del terreno, o bien un incremento en solicitaciones que afectan el estado de esfuerzos en la masa del mismo.<\/p><p>\u00a0<\/p><p>Es por eso que la interacci\u00f3n terreno-agua debe ser comprendida de manera adecuada, ya que es uno de los factores m\u00e1s importantes a considerar en an\u00e1lisis de estabilidad de taludes. En la Figura 3 se presentan los principales efectos del agua como detonante de una falla en un talud.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-a333990 elementor-section-full_width elementor-section-height-default elementor-section-height-default\" data-id=\"a333990\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-765bfbc\" data-id=\"765bfbc\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-08404bb elementor-widget elementor-widget-image\" data-id=\"08404bb\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<img loading=\"lazy\" decoding=\"async\" width=\"1209\" height=\"627\" src=\"https:\/\/geo-webonline.com\/wp-content\/uploads\/2021\/08\/Figura-3-1.jpg\" class=\"attachment-full size-full wp-image-1489\" alt=\"\" srcset=\"https:\/\/geo-webonline.com\/wp-content\/uploads\/2021\/08\/Figura-3-1.jpg 1209w, https:\/\/geo-webonline.com\/wp-content\/uploads\/2021\/08\/Figura-3-1-300x156.jpg 300w, https:\/\/geo-webonline.com\/wp-content\/uploads\/2021\/08\/Figura-3-1-1024x531.jpg 1024w, https:\/\/geo-webonline.com\/wp-content\/uploads\/2021\/08\/Figura-3-1-768x398.jpg 768w\" sizes=\"(max-width: 1209px) 100vw, 1209px\" \/>\t\t\t\t\t\t\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-b7f22df elementor-section-full_width elementor-section-height-default elementor-section-height-default\" data-id=\"b7f22df\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-dcaa0c7\" data-id=\"dcaa0c7\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-7e7c202 elementor-widget elementor-widget-text-editor\" data-id=\"7e7c202\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p><strong>Figura 3 <\/strong>Principales efectos del agua como detonante de una falla en un talud.<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-920e836 elementor-section-full_width elementor-section-height-default elementor-section-height-default\" data-id=\"920e836\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-68d74b4\" data-id=\"68d74b4\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-3989458 elementor-widget elementor-widget-text-editor\" data-id=\"3989458\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<p>Echemos un vistazo a cada factor:<\/p><p>\u00a0<\/p><ol><li>En relaci\u00f3n al <em>aumento del peso del suelo<\/em>, al ser \u00e9ste un medio poroso, el mismo puede eventualmente saturarse (debido a la acci\u00f3n de lluvias muy intensas, por ejemplo, o por infiltraci\u00f3n de agua asociada a efectos antr\u00f3picos), y as\u00ed aumentar considerablemente el peso unitario del mismo, lo que favorece el movimiento de la masa del terreno.<\/li><\/ol><p>\u00a0<\/p><ol start=\"2\"><li>La <em>disminuci\u00f3n de la resistencia por agua adsorbida<\/em> es particularmente importante para el caso de materiales arcillosos, en los cuales el agua es absorbida f\u00e1cilmente, adhiri\u00e9ndose a los bordes y las caras de las part\u00edculas s\u00f3lidas, generando as\u00ed una disminuci\u00f3n de la resistencia al corte entre las mismas.<\/li><\/ol><p>\u00a0<\/p><ol start=\"3\"><li>En ciertos materiales (como por ejemplo algunos suelos residuales, o suelos potencialmente colapsables), el flujo de agua a trav\u00e9s de los poros del suelo genera la <em>disoluci\u00f3n<\/em> de las part\u00edculas minerales de menor tama\u00f1o, que fungen como uniones entre las de mayor tama\u00f1o, lo cual ocasiona el colapso de la estructura de suelo.<\/li><\/ol><p>\u00a0<\/p><ol start=\"4\"><li>La <em>erosi\u00f3n interna<\/em>, por su parte, est\u00e1 asociada al flujo de agua entre los poros del terreno, que puede generar cavernas, induciendo as\u00ed la falla del talud.<\/li><\/ol><p>\u00a0<\/p><ol start=\"5\"><li>La saturaci\u00f3n del terreno genera que los poros se llenen de agua, y si por alguna raz\u00f3n externa se genera un <em>incremento de la<\/em> <em>presi\u00f3n de poros<\/em> (como puede ocurrir debido a fuertes lluvias, o a infiltraci\u00f3n de agua proveniente de procesos antr\u00f3picos), la resistencia al corte del terreno disminuye, seg\u00fan la conocida Ley de Esfuerzos Efectivos desarrollada por Terzaghi.<\/li><\/ol><p>\u00a0<\/p><p>Por supuesto, todos los suelos se ven afectados por estos procesos. Sin embargo, la naturaleza de los materiales afectar\u00e1 la <em>rapidez<\/em> con la que ocurren estos fen\u00f3menos. En general, puede decirse que en materiales de elevada permeabilidad, estos efectos pueden ocurrir r\u00e1pidamente, en cuesti\u00f3n de minutos, mientras que en el caso de terrenos poco permeables, los cambios son m\u00e1s lentos.<\/p><p>\u00a0<\/p><p>\u00a1A tener cuidado con los efectos del agua! \u00a1Y a considerarlos de manera apropiada en los an\u00e1lisis de estabilidad de taludes!<\/p>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-4d28d92 elementor-section-full_width elementor-section-height-default elementor-section-height-default\" data-id=\"4d28d92\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-4a45198\" data-id=\"4a45198\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-0f01cc1 elementor-widget elementor-widget-heading\" data-id=\"0f01cc1\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<h3 class=\"elementor-heading-title elementor-size-default\">Referencias<\/h3>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-3daf53b elementor-section-full_width elementor-section-height-default elementor-section-height-default\" data-id=\"3daf53b\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-4cb2365\" data-id=\"4cb2365\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-d49c614 elementor-widget elementor-widget-text-editor\" data-id=\"d49c614\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<ul><li>Abramson, L; Lee, T; Sharma, S. &amp; Boyce, G. (1996) <strong>\u201cSlope Stabilization and Stabilization Methods\u201d<\/strong>. John Wiley &amp; Sons, INC. USA.<\/li><li>Sancio, R. (1995) <strong>\u201cElementos de Hidrolog\u00eda e Hidrogeolog\u00eda\u201d<\/strong>. I Curso Panamericano de Movimientos de Masas. Barquisimeto, Venezuela.<\/li><\/ul>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-cd6a96c elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"cd6a96c\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-52174e5\" data-id=\"52174e5\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-10abc11 elementor-shape-circle elementor-grid-0 e-grid-align-center elementor-widget elementor-widget-social-icons\" data-id=\"10abc11\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"social-icons.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t<div class=\"elementor-social-icons-wrapper elementor-grid\" role=\"list\">\n\t\t\t\t\t\t\t<span class=\"elementor-grid-item\" role=\"listitem\">\n\t\t\t\t\t<a class=\"elementor-icon elementor-social-icon elementor-social-icon-facebook elementor-repeater-item-7da78dc\" href=\"https:\/\/www.facebook.com\/Geo-Web-100977118794652\" target=\"_blank\">\n\t\t\t\t\t\t<span class=\"elementor-screen-only\">Facebook<\/span>\n\t\t\t\t\t\t<i aria-hidden=\"true\" class=\"fab fa-facebook\"><\/i>\t\t\t\t\t<\/a>\n\t\t\t\t<\/span>\n\t\t\t\t\t\t\t<span class=\"elementor-grid-item\" role=\"listitem\">\n\t\t\t\t\t<a class=\"elementor-icon elementor-social-icon elementor-social-icon-twitter elementor-repeater-item-fe85f2d\" href=\"https:\/\/twitter.com\/geowebonline\" target=\"_blank\">\n\t\t\t\t\t\t<span class=\"elementor-screen-only\">Twitter<\/span>\n\t\t\t\t\t\t<i aria-hidden=\"true\" class=\"fab fa-twitter\"><\/i>\t\t\t\t\t<\/a>\n\t\t\t\t<\/span>\n\t\t\t\t\t\t\t<span class=\"elementor-grid-item\" role=\"listitem\">\n\t\t\t\t\t<a class=\"elementor-icon elementor-social-icon elementor-social-icon-instagram elementor-repeater-item-a21533a\" href=\"https:\/\/www.instagram.com\/geowebonline\/\" target=\"_blank\">\n\t\t\t\t\t\t<span class=\"elementor-screen-only\">Instagram<\/span>\n\t\t\t\t\t\t<i aria-hidden=\"true\" class=\"fab fa-instagram\"><\/i>\t\t\t\t\t<\/a>\n\t\t\t\t<\/span>\n\t\t\t\t\t\t\t<span class=\"elementor-grid-item\" role=\"listitem\">\n\t\t\t\t\t<a class=\"elementor-icon elementor-social-icon elementor-social-icon-linkedin elementor-repeater-item-8544528\" href=\"https:\/\/www.linkedin.com\/in\/alvaro-boiero-37bb4348\/\" target=\"_blank\">\n\t\t\t\t\t\t<span class=\"elementor-screen-only\">Linkedin<\/span>\n\t\t\t\t\t\t<i aria-hidden=\"true\" class=\"fab fa-linkedin\"><\/i>\t\t\t\t\t<\/a>\n\t\t\t\t<\/span>\n\t\t\t\t\t<\/div>\n\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-68b95fb elementor-section-full_width elementor-section-height-default elementor-section-height-default\" data-id=\"68b95fb\" data-element_type=\"section\" data-e-type=\"section\" data-settings=\"{&quot;background_background&quot;:&quot;gradient&quot;}\">\n\t\t\t\t\t\t\t<div class=\"elementor-background-overlay\"><\/div>\n\t\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-2e5522b\" data-id=\"2e5522b\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-5004c22 elementor-widget elementor-widget-heading\" data-id=\"5004c22\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"heading.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t<h2 class=\"elementor-heading-title elementor-size-default\">2024 - geo Todos los derechos reservados \/ Desarrollo web: lubercba<\/h2>\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<\/div>\n\t\t","protected":false},"excerpt":{"rendered":"<p>Facebook Twitter Instagram Linkedin El efecto del agua en los taludes El agua est\u00e1 normalmente asociada a la mayor\u00eda de los mecanismos de falla que puede experimentar un talud. Desde varios tipos de carga que incrementan los esfuerzos actuantes en el talud, hasta la disminuci\u00f3n de la resistencia al corte del terreno, el agua aparece [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-1481","page","type-page","status-publish","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v28.0 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>El efecto del agua en los taludes -<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/geo-webonline.com\/en\/el-efecto-del-agua-en-los-taludes\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"El efecto del agua en los taludes -\" \/>\n<meta property=\"og:description\" content=\"Facebook Twitter Instagram Linkedin El efecto del agua en los taludes El agua est\u00e1 normalmente asociada a la mayor\u00eda de los mecanismos de falla que puede experimentar un talud. 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