{"version":"1.0","provider_name":"HydroSciences Montpellier","provider_url":"https:\/\/www.hydrosciences.org\/en","title":"Equipe HYTAKE : HYdrog\u00e9ologie et Transferts  dans  les  Aquif\u00e8res Karstiques et h\u00e9t\u00e9rog\u00e8nEs - HydroSciences Montpellier","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"rtANdU5OoQ\"><a href=\"https:\/\/www.hydrosciences.org\/en\/hytake\/\">Equipe HYTAKE : HYdrog\u00e9ologie et Transferts   dans   les   Aquif\u00e8res Karstiques et h\u00e9t\u00e9rog\u00e8nEs<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/www.hydrosciences.org\/en\/hytake\/embed\/#?secret=rtANdU5OoQ\" width=\"600\" height=\"338\" title=\"&#8220;Equipe HYTAKE : HYdrog\u00e9ologie et Transferts   dans   les   Aquif\u00e8res Karstiques et h\u00e9t\u00e9rog\u00e8nEs&#8221; &#8212; HydroSciences Montpellier\" data-secret=\"rtANdU5OoQ\" 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:\/\/www.hydrosciences.org\/wp-includes\/js\/wp-embed.min.js\n<\/script>","description":"Responsable&nbsp; C. Batiot-Guilhe Mots cl\u00e9s Hydrog\u00e9ologie, Karst, Aquif\u00e8res h\u00e9t\u00e9rog\u00e8nes, Hydrodynamique, Hydrog\u00e9ochimie, Mod\u00e9lisation, Approche multi-\u00e9chelles, Interactions surface\/souterrain, Ressource en eau souterraine Pr\u00e9sentation L\u2019\u00e9quipe HYTAKE est compos\u00e9e de 15 membres permanents (\u224810 ETP), majoritairement enseignants-chercheurs, rattach\u00e9s \u00e0 l\u2019Universit\u00e9 de Montpellier et l\u2019IMT Mines Al\u00e8s, ainsi que des chercheurs CNRS et IRD et deux chercheurs associ\u00e9s du l\u2019\u00e9quipe [&hellip;]"}