{"version":"1.0","provider_name":"matforge.org","provider_url":"https:\/\/matforge.org","author_name":"Elena Markovska","author_url":"https:\/\/matforge.org\/author\/elena-markovska\/","title":"Aplicaciones Geof\u00edsicas: Modelado PDE para Sistemas de Tierra - matforge.org","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"0s8t1ONXTF\"><a href=\"https:\/\/matforge.org\/es\/geophysics-applications-pde-modeling-for-earth-systems\/\">Aplicaciones Geof\u00edsicas: Modelado PDE para Sistemas de Tierra<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/matforge.org\/es\/geophysics-applications-pde-modeling-for-earth-systems\/embed\/#?secret=0s8t1ONXTF\" width=\"600\" height=\"338\" title=\"\u00abAplicaciones Geof\u00edsicas: Modelado PDE para Sistemas de Tierra\u00bb \u2014 matforge.org\" data-secret=\"0s8t1ONXTF\" frameborder=\"0\" marginwidth=\"0\" marginheight=\"0\" scrolling=\"no\" class=\"wp-embedded-content\"><\/iframe><script>\n\/*! This file is auto-generated *\/\n!function(d,l){\"use strict\";l.querySelector&&d.addEventListener&&\"undefined\"!=typeof URL&&(d.wp=d.wp||{},d.wp.receiveEmbedMessage||(d.wp.receiveEmbedMessage=function(e){var t=e.data;if((t||t.secret||t.message||t.value)&&!\/[^a-zA-Z0-9]\/.test(t.secret)){for(var s,r,n,a=l.querySelectorAll('iframe[data-secret=\"'+t.secret+'\"]'),o=l.querySelectorAll('blockquote[data-secret=\"'+t.secret+'\"]'),c=new RegExp(\"^https?:$\",\"i\"),i=0;i<o.length;i++)o[i].style.display=\"none\";for(i=0;i<a.length;i++)s=a[i],e.source===s.contentWindow&&(s.removeAttribute(\"style\"),\"height\"===t.message?(1e3<(r=parseInt(t.value,10))?r=1e3:~~r<200&&(r=200),s.height=r):\"link\"===t.message&&(r=new URL(s.getAttribute(\"src\")),n=new URL(t.value),c.test(n.protocol))&&n.host===r.host&&l.activeElement===s&&(d.top.location.href=t.value))}},d.addEventListener(\"message\",d.wp.receiveEmbedMessage,!1),l.addEventListener(\"DOMContentLoaded\",function(){for(var e,t,s=l.querySelectorAll(\"iframe.wp-embedded-content\"),r=0;r<s.length;r++)(t=(e=s[r]).getAttribute(\"data-secret\"))||(t=Math.random().toString(36).substring(2,12),e.src+=\"#?secret=\"+t,e.setAttribute(\"data-secret\",t)),e.contentWindow.postMessage({message:\"ready\",secret:t},\"*\")},!1)))}(window,document);\n\/\/# sourceURL=https:\/\/matforge.org\/wp-includes\/js\/wp-embed.min.js\n<\/script>\n","description":"Los fen\u00f3menos geof\u00edsicos, desde el flujo de agua subterr\u00e1nea hasta la convecci\u00f3n del manto, se rigen por ecuaciones diferenciales parciales (PDE). Los m\u00e9todos de volumen finito (FVM) resuelven estas PDE haciendo cumplir las leyes de conservaci\u00f3n sobre los vol\u00famenes de control, haci\u00e9ndolos ideales para sistemas de tierra complejos y no lineales. Las herramientas de Python [&hellip;]"}