{"id":1428,"date":"2015-06-29T22:05:42","date_gmt":"2015-06-29T22:05:42","guid":{"rendered":"http:\/\/elmontgomery.com\/?p=982"},"modified":"2022-12-07T14:54:54","modified_gmt":"2022-12-07T21:54:54","slug":"how-economic-brines-form-within-closed-basins","status":"publish","type":"post","link":"https:\/\/elmontgomery.com\/es\/hydro-notes\/how-economic-brines-form-within-closed-basins\/","title":{"rendered":"C\u00f3mo se forman salmueras econ\u00f3micas dentro de cuencas cerradas"},"content":{"rendered":"<div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-1 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"--awb-border-radius-top-left:0px;--awb-border-radius-top-right:0px;--awb-border-radius-bottom-right:0px;--awb-border-radius-bottom-left:0px;--awb-flex-wrap:wrap;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-flex-start fusion-flex-content-wrap\" style=\"max-width:1248px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-0 fusion_builder_column_1_1 1_1 fusion-flex-column\" style=\"--awb-bg-size:cover;--awb-width-large:100%;--awb-margin-top-large:0px;--awb-spacing-right-large:1.92%;--awb-margin-bottom-large:0px;--awb-spacing-left-large:1.92%;--awb-width-medium:100%;--awb-spacing-right-medium:1.92%;--awb-spacing-left-medium:1.92%;--awb-width-small:100%;--awb-spacing-right-small:1.92%;--awb-spacing-left-small:1.92%;\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\"><div class=\"fusion-text fusion-text-1\"><p>En ciertas cuencas cerradas en los Andes y otras partes del mundo, el agua subterr\u00e1nea puede llegar a estar tan concentrada en s\u00f3lidos disueltos totales (TDS) que supera la salinidad del agua de mar y forma salmuera. El agua subterr\u00e1nea generalmente se considera salina si su TDS supera los 1000 mg\/L, pero se clasifica como salobre cuando las concentraciones de TDS est\u00e1n en el rango de 1000 a 10 000 mg\/L. El agua de mar contiene alrededor de 35.000 mg\/L de TDS. Una vez que las concentraciones superan ese nivel, tenemos salmuera.<\/p>\n<p>Las cuencas cerradas, que no permiten la salida a cuerpos de agua externos, ofrecen condiciones ideales para la formaci\u00f3n de salmuera. (En Am\u00e9rica del Sur, tales cuencas se conocen como \u201csalares\u201d, un verbo espa\u00f1ol que significa \u201csalar\u201d). A medida que el agua fluye sobre y a trav\u00e9s de formaciones geol\u00f3gicas, varios elementos (sodio, calcio y potasio, entre otros) se disuelven de la roca; las fuentes hidrotermales tambi\u00e9n pueden liberar o movilizar dichos elementos. El agua fluye hacia la parte m\u00e1s baja de un recipiente cerrado, donde se evapora. Este proceso deja atr\u00e1s los elementos disueltos, aumentando las concentraciones de TDS y la densidad del agua. El agua subterr\u00e1nea m\u00e1s densa y salina se hunde. Durante miles de a\u00f1os, la cantidad de agua subterr\u00e1nea salina y densa aumenta, y el salar evolucionar\u00e1 de joven a viejo.<\/p>\n<p>Las salmueras pueden ser un recurso valioso si contienen elementos como litio, potasio y boro en concentraciones econ\u00f3micas. En particular, el inter\u00e9s por el litio se ha intensificado durante los \u00faltimos a\u00f1os a medida que ha aumentado la demanda de bater\u00edas; el USGS estima que el 58 por ciento del litio del mundo se encuentra en salmueras de cuencas cerradas (Bradley y Jaksula, 2014)<sup>1<\/sup>. El potasio, un ingrediente clave en los fertilizantes y parte de la potasa del mundo, proviene de los dep\u00f3sitos de salmuera. El boro, otro elemento importante, tiene muchos usos industriales.<\/p>\n<p>Vuelva a consultar la Parte 2, una discusi\u00f3n sobre c\u00f3mo evaluar y extraer este recurso.<\/p>\n<p><em>1 \u2014 Bradley, Dwight y Jaskula, Brian, 2014, Litio: para aprovechar la energ\u00eda renovable: hoja informativa del Servicio Geol\u00f3gico de EE. UU. 2014-3035, 2 p., http:\/\/pubs.usgs.gov\/fs\/2014\/3035\/<\/em><\/p>\n<\/div><\/div><\/div><\/div><\/div>","protected":false},"excerpt":{"rendered":"","protected":false},"author":4,"featured_media":9226,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[6],"tags":[],"class_list":["post-1428","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-hydro-notes"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.3 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>How do brines evolve within closed hydrologic basins?<\/title>\n<meta name=\"description\" content=\"Explanation of how lithium and other economic brines are formed in closed hydrologic basins or salars\" \/>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/elmontgomery.com\/es\/hydro-notes\/how-economic-brines-form-within-closed-basins\/\" \/>\n<meta property=\"og:locale\" content=\"es_ES\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"How do brines evolve within closed hydrologic basins?\" \/>\n<meta property=\"og:description\" content=\"Explanation of how lithium and other economic brines are formed in closed hydrologic basins or salars\" \/>\n<meta property=\"og:url\" content=\"https:\/\/elmontgomery.com\/es\/hydro-notes\/how-economic-brines-form-within-closed-basins\/\" \/>\n<meta property=\"og:site_name\" content=\"Montgomery &amp; 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