{"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":"Applications de la g\u00e9ophysique : mod\u00e9lisation PDE pour les syst\u00e8mes terrestres - matforge.org","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"RBOGPehwk2\"><a href=\"https:\/\/matforge.org\/fr\/geophysics-applications-pde-modeling-for-earth-systems\/\">Applications de la g\u00e9ophysique : mod\u00e9lisation PDE pour les syst\u00e8mes terrestres<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/matforge.org\/fr\/geophysics-applications-pde-modeling-for-earth-systems\/embed\/#?secret=RBOGPehwk2\" width=\"600\" height=\"338\" title=\"\u00ab\u00a0Applications de la g\u00e9ophysique : mod\u00e9lisation PDE pour les syst\u00e8mes terrestres\u00a0\u00bb &#8212; matforge.org\" data-secret=\"RBOGPehwk2\" 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":"Les ph\u00e9nom\u00e8nes g\u00e9ophysiques, de l&rsquo;\u00e9coulement des eaux souterraines \u00e0 la convection du manteau, sont r\u00e9gis par des \u00e9quations aux d\u00e9riv\u00e9es partielles (EDP). Les m\u00e9thodes de volume fini (FVM) r\u00e9solvent ces PDE en appliquant les lois de conservation sur les volumes de contr\u00f4le, ce qui les rend id\u00e9ales pour les syst\u00e8mes terrestres complexes et non lin\u00e9aires. [&hellip;]"}