{"id":2818,"date":"2025-01-27T15:23:06","date_gmt":"2025-01-27T14:23:06","guid":{"rendered":"https:\/\/devw.isska.ch\/?page_id=2818"},"modified":"2025-01-29T09:17:07","modified_gmt":"2025-01-29T08:17:07","slug":"thermokarst","status":"publish","type":"page","link":"https:\/\/devw.isska.ch\/de\/thermokarst\/","title":{"rendered":"Ther\u00admo\u00adKarst"},"content":{"rendered":"<ul>\n<li>\n        <a href=\"https:\/\/devw.isska.ch\/de\/wer-sind-wir\/\">\u00dcber uns<\/a>\n    <\/li>\n<li>\n        <a href=\"https:\/\/devw.isska.ch\/de\/kompetenzen\/\">Kom\u00adpe\u00adten\u00adzen<\/a>\n    <\/li>\n<li>\n        <a href=\"https:\/\/devw.isska.ch\/de\/leistungen\/\">Dienst\u00adleis\u00adtun\u00adgen<\/a>\n    <\/li>\n<\/ul>\n<h1>ThermoKarst<\/h1>\n<div>\n<div class=\"show-more-wrapper\">\n<div class=\"text-content\">\n<p>Unte\u00adrir\u00addische Hohlr\u00e4ume sind ein emp\u00adfind\u00adliches \u00d6ko\u00adsys\u00adtem, in dem bio\u00adgeo\u00adche\u00admische Pro\u00adzesse stark von der Tem\u00adpe\u00adra\u00adtur abh\u00e4n\u00adgen. Sie beher\u00adber\u00adgen auch ein\u00adzi\u00adgar\u00adtige Spu\u00adren ihrer ver\u00adgan\u00adge\u00adnen Umwelt, deren Inter\u00adpre\u00adta\u00adtion eng mit der Tem\u00adpe\u00adra\u00adtur verkn\u00fcpft ist.<\/p>\n<p>In den letz\u00adten Jah\u00adren haben sich viele Stu\u00addien auf Spel\u00e4o\u00adtheme, sekund\u00e4re Kar\u00adbo\u00adnat\u00adfor\u00adma\u00adtio\u00adnen wie Sta\u00adlag\u00admi\u00adten und Sta\u00adlag\u00admi\u00adtens\u00adtr\u00f6me, kon\u00adzen\u00adtriert, da sie in der Lage sind, pal\u00e4oen\u00advi\u00adron\u00admen\u00adtale Infor\u00adma\u00adtio\u00adnen zu archi\u00advie\u00adren, die genau auf die letz\u00adten 0,5 Ma datiert wer\u00adden k\u00f6n\u00adnen. Meh\u00adrere Mecha\u00adnis\u00admen, darun\u00adter die W\u00e4r\u00adme\u00addif\u00adfu\u00adsion im umge\u00adben\u00adden Gestein und die Advek\u00adtion durch Was\u00adser und Luft, \u00fcber\u00adtra\u00adgen W\u00e4rme von der Au\u00dfen\u00adfl\u00e4che in den Hohl\u00adraum. Je nach der rela\u00adti\u00adven Bedeu\u00adtung die\u00adser ver\u00adschie\u00adde\u00adnen Fl\u00fcsse wird die unte\u00adrir\u00addische Tem\u00adpe\u00adra\u00adtur als Reak\u00adtion auf die zeit\u00adli\u00adchen Schwan\u00adkun\u00adgen der Au\u00dfen\u00adtem\u00adpe\u00adra\u00adtur mehr oder weni\u00adger stark ged\u00e4mpft und pha\u00adsen\u00adver\u00adscho\u00adben.<\/p>\n<p>Ein gutes Verst\u00e4nd\u00adnis der ther\u00admi\u00adschen Reak\u00adtion des Karstes auf den Kli\u00adma\u00adwan\u00addel ist daher grund\u00adle\u00adgend, um die Aufl\u00f6\u00adsungs-\/Nie\u00adder\u00adschlag\u00adsra\u00adten zu quan\u00adti\u00adfi\u00adzie\u00adren und die in den Kon\u00adkre\u00admen\u00adten beo\u00adbach\u00adte\u00adten geo\u00adche\u00admi\u00adschen Ver\u00e4n\u00adde\u00adrun\u00adgen zu inter\u00adpre\u00adtie\u00adren und die Aus\u00adwir\u00adkun\u00adgen auf die leben\u00adden Orga\u00adnis\u00admen in den H\u00f6h\u00adlen zu bewer\u00adten.<\/p>\n<p><span class=\"more-text\"><br>\n<br>Aus\u00adge\u00adhend von der Lite\u00adra\u00adtur haben wir drei Hypo\u00adthe\u00adsen for\u00admu\u00adliert, die wir im Pro\u00adjekt zu vali\u00addie\u00adren suchen&nbsp;:<\/span><\/p>\n<ol>\n<li>Die Bel\u00fcf\u00adtung von Karst\u00admas\u00adsi\u00adven stellt einen domi\u00adnie\u00adren\u00adden Mecha\u00adnis\u00admus f\u00fcr die W\u00e4r\u00adme\u00fc\u00adber\u00adtra\u00adgung dar<\/li>\n<p><\/p>\n<li>Die Reak\u00adtions\u00adzeit von Mas\u00adsi\u00adven und H\u00f6h\u00adlen h\u00e4ngt haupts\u00e4\u00adchlich von advek\u00adti\u00adven Str\u00f6\u00admun\u00adgen (Was\u00adser und Luft) ab, mehr als von der W\u00e4r\u00adme\u00adlei\u00adtung im Gestein.<\/li>\n<p><\/p>\n<li>Der W\u00e4r\u00admeaus\u00adtausch reicht aus, um zumin\u00addest unter bes\u00adtimm\u00adten Bedin\u00adgun\u00adgen eine signi\u00adfi\u00adkante Menge an Kon\u00addens\u00adwas\u00adser zur Auff\u00fcl\u00adlung von Karst\u00adsys\u00adte\u00admen zu pro\u00addu\u00adzie\u00adren.<\/li>\n<\/ol>\n<p>\nZiel des Pro\u00adjekts ist es, eine gr\u00fcnd\u00adliche Ana\u00adlyse der Mas\u00adsen- und W\u00e4r\u00adme\u00fc\u00adber\u00adtra\u00adgung in Karst\u00adsys\u00adte\u00admen dur\u00adch\u00adzuf\u00fch\u00adren, um diese Fra\u00adgen zu beant\u00adwor\u00adten. Ins\u00adbe\u00adson\u00addere m\u00f6ch\u00adten wir die Aus\u00adwir\u00adkun\u00adgen eines Kli\u00adma\u00adwan\u00addels auf die unte\u00adrir\u00addische Umwelt cha\u00adrak\u00adte\u00adri\u00adsie\u00adren und die ther\u00admische Reak\u00adtion einer H\u00f6hle auf ver\u00adschie\u00adde\u00adnen r\u00e4um\u00adli\u00adchen und zeit\u00adli\u00adchen Ska\u00adlen bes\u00adtim\u00admen. Wir wer\u00adden ein verein\u00adfachtes glo\u00adbales Modell der Karst\u00admas\u00adsive ent\u00adwi\u00adckeln, das aus meh\u00adre\u00adren Sub\u00adsys\u00adte\u00admen (Gestein, Lei\u00adtung, Epi\u00adkarst\u2026) bes\u00adteht. Die W\u00e4r\u00adme\u00fc\u00adber\u00adtra\u00adgung durch Lei\u00adtung und Advek\u00adtion (Was\u00adser und Luft) im Gestein und in den Lei\u00adtun\u00adgen wird voll\u00adst\u00e4n\u00addig gekop\u00adpelt sein. Aller\u00addings sind die Aus\u00adwir\u00adkun\u00adgen der nat\u00fcr\u00adli\u00adchen Bel\u00fcf\u00adtung der H\u00f6h\u00adlen und des Epi\u00adkarsts der\u00adzeit nicht gut quan\u00adti\u00adfi\u00adziert, was eine Model\u00adlie\u00adrung ris\u00adkant macht. Daher wer\u00adden paral\u00adlel zu den Simu\u00adla\u00adtio\u00adnen Feld\u00admes\u00adsun\u00adgen durch\u00adgef\u00fchrt.<\/p>\n<p>Um dieses Ziel zu errei\u00adchen, st\u00fctzt sich das Pro\u00adjekt auf zwei Teams mit kom\u00adple\u00adment\u00e4\u00adren Kom\u00adpe\u00adten\u00adzen, eines spe\u00adzia\u00adli\u00adsiert auf das Moni\u00adto\u00adring und die Kon\u00adzep\u00adtua\u00adli\u00adsie\u00adrung von Karst\u00adsys\u00adte\u00admen (ISSKA), das andere auf W\u00e4rme- und Stoff\u00fc\u00adber\u00adtra\u00adgung (FAST). Diese bei\u00adden Teil\u00adbe\u00adreiche wer\u00adden daher paral\u00adlel bear\u00adbei\u00adtet. Zu Beginn wird eine para\u00adme\u00adtrische Stu\u00addie (Aus\u00adgang\u00adsmo\u00addell) mit verein\u00adfach\u00adten ana\u00adly\u00adti\u00adschen Model\u00adlen durch\u00adgef\u00fchrt, um die Gr\u00f6\u00dfe der jewei\u00adli\u00adgen Pro\u00adzesse unter ver\u00adschie\u00adde\u00adnen Bedin\u00adgun\u00adgen abzu\u00adsch\u00e4t\u00adzen. Dies wird es erm\u00f6\u00adgli\u00adchen, den Inhalt des<br>\ners\u00adten nume\u00adri\u00adschen Modells (Teil 1) und der Date\u00adner\u00adfas\u00adsung im Feld (Teil 2). Die bei\u00adden Teile wer\u00adden im Laufe des For\u00adschung\u00adspro\u00adgramms ite\u00adra\u00adtiv zusam\u00admen\u00adge\u00adfasst, sodass am Ende alle drei Hypo\u00adthe\u00adsen dis\u00adku\u00adtiert wer\u00adden k\u00f6n\u00adnen. Zwei Haupts\u00adtan\u00addorte wer\u00adden ins\u00adtru\u00admen\u00adtiert, darun\u00adter das unte\u00adrir\u00addische Labor von Milandre, wo bereits zahl\u00adreiche Daten vor\u00adlie\u00adgen. Die Stan\u00addorte wer\u00adden hin\u00adsicht\u00adlich der Tem\u00adpe\u00adra\u00adtur sowie der wich\u00adtig\u00adsten Para\u00adme\u00adter, die den Mas\u00adsen\u00adtrans\u00adfer kon\u00adtrol\u00adlie\u00adren, \u00fcber\u00adwacht&nbsp;: Luft- und Was\u00adser\u00adfluss durch direkte (Dur\u00adch\u00adfluss\u00adra\u00adten) und indi\u00adrekte (CO2 und Radon) Mes\u00adsun\u00adgen.<\/p>\n<p>Ein Team von zwei Dok\u00adto\u00adran\u00adden soll das Moni\u00adto\u00adring vor Ort ein\u00adset\u00adzen und die f\u00fcr das Pro\u00adjekt erfor\u00adder\u00adli\u00adchen Kom\u00adpe\u00adten\u00adzen und Simu\u00adla\u00adtions\u00adwerk\u00adzeuge ent\u00adwi\u00adckeln. Erfah\u00adrene For\u00adscher des SISKA und des FAST wer\u00adden die Dok\u00adto\u00adran\u00adden aktiv unterst\u00fct\u00adzen, um<br>\nVer\u00adfah\u00adren fest\u00adle\u00adgen, Kom\u00adpe\u00adten\u00adzen ent\u00adwi\u00adckeln und Ent\u00adschei\u00addun\u00adgen tref\u00adfen, die zur L\u00f6sung der ans\u00adte\u00adhen\u00adden Heraus\u00adfor\u00adde\u00adrun\u00adgen erfor\u00adder\u00adlich sind.<\/p>\n<p>Dieses Pro\u00adjekt wird zwei\u00adfel\u00adlos neue Erkennt\u00adnisse \u00fcber die Reak\u00adtion von Karst\u00admas\u00adsi\u00adven auf den Kli\u00adma\u00adwan\u00addel, die Bel\u00fcf\u00adtung von Karst\u00admas\u00adsi\u00adven und die Bedeu\u00adtung der Kon\u00adden\u00adsa\u00adtion f\u00fcr die Auff\u00fcl\u00adlung von Grund\u00adwas\u00adser\u00adlei\u00adtern lie\u00adfern.<\/p>\n<p>Die Ergeb\u00adnisse des Pro\u00adjekts wer\u00adden auch wich\u00adtige Daten f\u00fcr andere Bereiche lie\u00adfern&nbsp;: Trink\u00adwas\u00adser\u00adver\u00adsor\u00adgung (Tem\u00adpe\u00adra\u00adtur\u00adsch\u00adwan\u00adkun\u00adgen von Karst\u00adquel\u00adlen), \u00f6ffent\u00adliche Gesund\u00adheit (aus\u00adgeat\u00admetes Radon in Wohnh\u00e4u\u00adsern), Spel\u00e4o\u00adge\u00adnese (Kor\u00adro\u00adsion durch Kon\u00adden\u00adsa\u00adtion), Per\u00adma\u00adfrost (nat\u00fcr\u00adliche Eish\u00f6h\u00adlen), Nie\u00adder\u00adtem\u00adpe\u00adra\u00adtur-Geo\u00adther\u00admie (Aus\u00adwir\u00adkun\u00adgen von Lei\u00adtun\u00adgen auf den W\u00e4r\u00admeaus\u00adtausch), Tun\u00adnel- und Minen\u00adbau (Vorher\u00adsage von Hohlr\u00e4u\u00admen und mas\u00adsi\u00adven Was\u00adse\u00adrin\u00adtru\u00adsio\u00adnen), Fer\u00adner\u00adkun\u00addung (Inter\u00adpre\u00adta\u00adtion ther\u00admi\u00adscher Ano\u00adma\u00adlien), H\u00f6h\u00adle\u00adne\u00adrhal\u00adtung (Schutz arch\u00e4o\u00adlo\u00adgi\u00adscher und tou\u00adris\u00adti\u00adscher H\u00f6h\u00adlen), Koh\u00adlens\u00adtoff\u00adkreis\u00adlauf (Aufl\u00f6\u00adsung und Ausf\u00e4l\u00adlung von Kar\u00adbo\u00adna\u00adten wer\u00adden durch den pCO2-Wert, also durch die Ven\u00adti\u00adla\u00adtion, ges\u00adteuert), unte\u00adrir\u00addische Bio\u00adlo\u00adgie (Bio\u00adtope<br>\nunte\u00adrir\u00addisch)\u2026<\/p>\n<p>Die Ergeb\u00adnisse dieses Pro\u00adjekts wer\u00adden zu einem Schl\u00fcs\u00adsel\u00adschritt im Verst\u00e4nd\u00adnis der W\u00e4r\u00adme\u00fc\u00adber\u00adtra\u00adgung in Kar\u00adbo\u00adnat\u00adge\u00adstein wer\u00adden.<\/p>\n<p><span><a href=\"https:\/\/data.snf.ch\/grants\/grant\/188636\" data-wplink-url-error=\"true\" target=\"_blank\" rel=\"noopener\">Link zur SNF-Seite Ther\u00admo\u00adkarst<\/a><\/span><br>\n<br>\n     \t\n    <\/p><\/div>\n<p>    <button class=\"show-more-button\">Show more<\/button><\/p>\n<\/div>\n<p><img decoding=\"async\" src=\"\/wp-content\/uploads\/2024\/12\/domain_3-scaled.jpeg\" alt><br>\n<img decoding=\"async\" src=\"\/wp-content\/uploads\/2024\/12\/m0-scaled.jpg\" alt><\/p>\n<h1>PHD-Studierende<\/h1>\n<div>\n<div>\n<h3 style=\"text-align: center;\">Kontakt<\/h3>\n<p style=\"text-align: center;\"><a href=\"https:\/\/devw.isska.ch\/wp-admin\/admin-ajax.php?action=kernel&amp;p=customizer&amp;site=https%3A%2F%2Fdevw.isska.ch%2Ffr%2Fcompetences%2Fformation-et-mediation%2F\" aria-label=\"Select Image\" class=\"uk-position-cover\"><\/a><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/devw.isska.ch\/wp-content\/uploads\/2024\/01\/Amir_nb-225x300.jpg\" alt width=\"225\" height=\"300\" class=\"alignnone wp-image-611 size-medium\" srcset=\"https:\/\/devw.isska.ch\/wp-content\/uploads\/2024\/01\/Amir_nb-225x300.jpg 225w, https:\/\/devw.isska.ch\/wp-content\/uploads\/2024\/01\/Amir_nb-768x1024.jpg 768w, https:\/\/devw.isska.ch\/wp-content\/uploads\/2024\/01\/Amir_nb-1152x1536.jpg 1152w, https:\/\/devw.isska.ch\/wp-content\/uploads\/2024\/01\/Amir_nb-1536x2048.jpg 1536w, https:\/\/devw.isska.ch\/wp-content\/uploads\/2024\/01\/Amir_nb-scaled.jpg 1920w\" sizes=\"auto, (max-width: 225px) 100vw, 225px\"><\/p>\n<p style=\"text-align: center;\">Amir Seda\u00adghat\u00adkish<br><a href=\"mailto:amir.sedaghatkish@isska.ch\">E\u2011Mail sen\u00adden<\/a><\/p>\n\n<\/div>\n<\/div>\n<div>\n<div>\n<h3 style=\"text-align: center;\">Kontakt<\/h3>\n<p style=\"text-align: center;\"><a href=\"https:\/\/devw.isska.ch\/wp-admin\/admin-ajax.php?action=kernel&amp;p=customizer&amp;site=https%3A%2F%2Fdevw.isska.ch%2Ffr%2Fcompetences%2Fformation-et-mediation%2F\" aria-label=\"Select Image\" class=\"uk-position-cover\"><\/a><img loading=\"lazy\" decoding=\"async\" src=\"https:\/\/devw.isska.ch\/wp-content\/uploads\/2024\/01\/Claudio_nb-225x300.jpg\" alt width=\"225\" height=\"300\" class=\"alignnone wp-image-612 size-medium\" srcset=\"https:\/\/devw.isska.ch\/wp-content\/uploads\/2024\/01\/Claudio_nb-225x300.jpg 225w, https:\/\/devw.isska.ch\/wp-content\/uploads\/2024\/01\/Claudio_nb.jpg 532w\" sizes=\"auto, (max-width: 225px) 100vw, 225px\"><\/p>\n<p style=\"text-align: center;\">Clau\u00addio Pas\u00adtore<br><a href=\"mailto:claudio.pastore@isska.ch\">E\u2011Mail sen\u00adden<\/a><\/p>\n\n<\/div>\n<\/div>\n<h1>PIs<\/h1>\n<div>\n<p><span>Pierre-Yves Jean\u00adnin (ISSKA), Fr\u00e9\u00add\u00e9\u00adric Dou\u00admenc (Sor\u00adbonne), Marc Luet\u00adscher (ISSKA).<\/span><\/p>\n<\/div>\n<h1>Ver\u00f6ffentlichungen<\/h1>\n<div>\n<p class><span lang=\"EN-US\">Seda\u00adghat\u00adkish A., Dou\u00admenc F., Jean\u00adnin PY.,<span>&nbsp;<\/span><span>Luet\u00adscher M.<\/span>, 2024. Mode\u00adling the effect of free convec\u00adtion on per\u00adma\u00adfrost mel\u00adting rates in fro\u00adzen rock-clefts.<span>&nbsp;<\/span><i>The Cryos\u00adpher<\/i>e, 18, 4547\u20134565,<span>&nbsp;<\/span><a class=\"defaultMailLink defaultMailLink\" href=\"http:\/\/doi.org\/10.5194\/tc-18-4547-2024\" target=\"_blank\" rel=\"noopener noreferrer\" data-ik=\"ik-secure\">doi.org\/10.5194\/tc-18\u20134547-2024<\/a><\/span><\/p>\n<p class><span lang=\"EN-US\">Pas\u00adtore C., Seda\u00adghat\u00adkish A., Schmid N., Weber E.,<span>&nbsp;<\/span><span>Luet\u00adscher M.<\/span>, 2024. Moni\u00adto\u00adring air fluxes in caves using digi\u00adtal flow meters.<span>&nbsp;<\/span><i>Inter\u00adna\u00adtio\u00adnal Jour\u00adnal of Spe\u00adleo\u00adlo\u00adgy, 53, 63\u201373.<span>&nbsp;<\/span><\/i><a class=\"defaultMailLink defaultMailLink\" href=\"http:\/\/doi.org\/10.5038\/1827-806X.53.1.2500\" target=\"_blank\" rel=\"noopener noreferrer\" data-ik=\"ik-secure\">doi.org\/10.5038\/1827\u2013806X.53.1.2500<\/a><\/span><\/p>\n<p class><span lang=\"EN-US\">Seda\u00adghat\u00adkish A., Pas\u00adtore C., Dou\u00admenc F., Jean\u00adnin PY.,<span>&nbsp;<\/span><span>Luet\u00adscher M.<\/span>, 2024. Model\u00adling heat trans\u00adfer for asses\u00adsing the convec\u00adtion length in ven\u00adti\u00adla\u00adted caves.<span>&nbsp;<\/span><i>Jour\u00adnal of Geo\u00adphy\u00adsi\u00adcal Research&nbsp;: Earth Sur\u00adface (Jour\u00adnal f\u00fcr geo\u00adphy\u00adsi\u00adka\u00adlische For\u00adschung&nbsp;: Erdo\u00adber\u00adfl\u00e4che)<\/i>, 129, e2024JF007646.<\/span><span lang=\"EN-US\"><span>&nbsp;<\/span><\/span><span lang=\"FR\"><a class=\"defaultMailLink\" href=\"https:\/\/doi.org\/10.1029\/2024JF007646\" target=\"_blank\" rel=\"noopener noreferrer\" data-ik=\"ik-secure\"><span lang=\"EN-US\">doi.org\/10.1029\/2024JF007646<\/span><\/a><\/span><span lang=\"EN-US\"><\/span><\/p>\n<p class><span lang=\"EN-US\">Pas\u00adtore C., Weber E., Dou\u00admenc F., Jean\u00adnin PY.,<span>&nbsp;<\/span><span>Luet\u00adscher M.<\/span>, 2024. Dis\u00adper\u00adsion von k\u00fcnst\u00adli\u00adchen Tra\u00adcern in bel\u00fcf\u00adte\u00adten H\u00f6h\u00adlen.<span>&nbsp;<\/span><i>Inter\u00adna\u00adtio\u00adnal Jour\u00adnal of Spe\u00adleo\u00adlo\u00adgy<\/i>, 53(1), 51\u201362.<span>&nbsp;<\/span><a class=\"defaultMailLink defaultMailLink\" href=\"http:\/\/doi.org\/10.5038\/1827-806X.53.1.2497\" target=\"_blank\" rel=\"noopener noreferrer\" data-ik=\"ik-secure\">doi.org\/10.5038\/1827\u2013806X.53.1.2497<\/a><\/span><\/p>\n<p class><span lang=\"EN-US\">Gara\u00adgnon J,<span>&nbsp;<\/span><span>Luet\u00adscher M.<\/span>, Weber E., 2022. Ven\u00adti\u00adla\u00adtion regime in a kars\u00adtic sys\u00adtem (Milandre Cave, Swit\u00adzer\u00adland).<span>&nbsp;<\/span><i>Kars\u00adto\u00adlo\u00adgia Memoi\u00adren<\/i>, 23, 187\u201319<\/span><\/p>\n<\/div>\n<p><!--more--><br>\n<!-- {\"type\":\"layout\",\"children\":[{\"type\":\"section\",\"props\":{\"css\":\"@media (max-width:759px) {\\n  .el-section {\\n      height: 370px;\\n    }\\n}\\n@media (min-width:760px) {\\n    .el-section {\\n        height: 275px;\\n    }\\n}\\n@media (min-width:1200px) {\\n    .el-section {\\n        height: 340px;\\n    }\\n}\\n@media (min-width:1600px) {\\n    .el-section {\\n        height: 580px;\\n    }\\n}\\n@media (min-width:1600px) and (max-height:1100px) {\\n    .el-section {\\n        height: 460px;\\n    }\\n}\",\"image\":\"wp-content\\\/uploads\\\/2024\\\/01\\\/CreteVaas_2023_RW_5-scaled.jpg\",\"image_position\":\"center-center\",\"image_size\":\"cover\",\"padding\":\"large\",\"style\":\"default\",\"title_breakpoint\":\"xl\",\"title_position\":\"top-left\",\"title_rotation\":\"left\",\"vertical_align\":\"middle\",\"width\":\"default\"},\"children\":[{\"type\":\"row\",\"children\":[{\"type\":\"column\",\"props\":{\"image_position\":\"center-center\",\"position_sticky_breakpoint\":\"m\"},\"children\":[{\"type\":\"button\",\"props\":{\"css\":\".el-content {\\n    font-family: \\\"Century Gothic\\\", Verdana, sans-serif;\\n    }\\n@media (max-width:759px) {\\n  .el-content {\\n    margin: 10px 50px; \\n    width: 250px;\\n    position: relative;\\n    top: 180px;\\n  }\\n}\\n@media (min-width:760px) {\\n  .el-content {\\n    margin: 10px 6px; \\n    width: 217px;\\n    position: relative;\\n    top: 104px;\\n  }\\n}\\n@media (min-width:1200px) {\\n  .el-content {\\n    width: 260px;\\n    margin: 0px 40px;\\n    position: relative;\\n    top: 165px;\\n  }\\n}\\n@media (min-width:1600px) {\\n  .el-content {\\n    margin-top: 250px;\\n }\\n} \\n@media (min-width:1600px) and (max-height:1100px) {\\n  .el-content {\\n    margin-top: 130px;\\n }\\n} \",\"fullwidth\":false,\"grid_column_gap\":\"collapse\",\"grid_row_gap\":\"small\",\"margin\":\"default\",\"position_bottom\":\"-93\",\"position_z_index\":\"2\",\"text_align\":\"center\"},\"children\":[{\"type\":\"button_item\",\"props\":{\"button_style\":\"primary\",\"content\":\"Qui sommes-nous?\",\"icon_align\":\"left\",\"link\":\"https:\\\/\\\/devw.isska.ch\\\/qui-sommes-nous\"}},{\"type\":\"button_item\",\"props\":{\"button_style\":\"primary\",\"content\":\"Comp\\u00e9tences\",\"icon_align\":\"left\",\"link\":\"https:\\\/\\\/devw.isska.ch\\\/competences\\\/\"}},{\"type\":\"button_item\",\"props\":{\"button_style\":\"primary\",\"content\":\"Prestations\",\"icon_align\":\"left\",\"link\":\"https:\\\/\\\/devw.isska.ch\\\/prestations\\\/\"}}]}]}]}],\"name\":\"Header_fr\"},{\"type\":\"section\",\"props\":{\"css\":\"@media (max-width: 759px) {\\n    .el-row {\\n        padding-top: 135px;\\n    }\\n}\\n@media (max-width: 759px) and (orientation:landscape) {\\n    .el-row {\\n        padding-top: 140px;\\n    }\\n}\",\"image_position\":\"center-center\",\"style\":\"default\",\"title_breakpoint\":\"xl\",\"title_position\":\"top-left\",\"title_rotation\":\"left\",\"vertical_align\":\"middle\",\"width\":\"default\"},\"children\":[{\"type\":\"row\",\"children\":[{\"type\":\"column\",\"props\":{\"image_position\":\"center-center\",\"position_sticky_breakpoint\":\"m\"},\"children\":[{\"type\":\"breadcrumbs\",\"props\":{\"show_current\":true,\"show_home\":true,\"visibility\":\"s\"},\"name\":\"Breadcrumbs\"},{\"type\":\"headline\",\"props\":{\"content\":\"ThermoKarst\",\"title_element\":\"h1\"},\"name\":\"Titre\"},{\"type\":\"html\",\"props\":{\"content\":\"\n\n<div class=\\\"show-more-wrapper\\\">\\n    \n\n<div class=\\\"text-content\\\">\\n        \n\n<p>Les cavit\\u00e9s souterraines constituent un \\u00e9cosyst\\u00e8me fragile dans lequel les processus biog\\u00e9ochimiques d\\u00e9pendent fortement de la temp\\u00e9rature. Elles abritent \\u00e9galement des traces uniques de leur environnement pass\\u00e9 dont l\\u2019interpr\\u00e9tation d\\u00e9pend \\u00e9troitement de la temp\\u00e9rature.<br \/>\\n<br \/>Au cours des derni\\u00e8res ann\\u00e9es, beaucoup d\\u2019\\u00e9tudes ont port\\u00e9 sur les sp\\u00e9l\\u00e9oth\\u00e8mes, formations carbonat\\u00e9es secondaires telles que stalagmites et coul\\u00e9es stalagmitiques, en raison de leur capacit\\u00e9 \\u00e0 archiver des informations pal\\u00e9oenvironnementales que l\\u2019on peut dater avec pr\\u00e9cision, sur les derniers 0.5 Ma environ. Plusieurs m\\u00e9canismes, dont la diffusion thermique dans l\\u2019encaissant rocheux et l\\u2019advection par l\\u2019eau et l\\u2019air, transf\\u00e8rent de la chaleur de la surface ext\\u00e9rieure vers la cavit\\u00e9. En fonction de l\\u2019importance relative de ces diff\\u00e9rents flux, la temp\\u00e9rature souterraine sera plus ou moins att\\u00e9nu\\u00e9e et d\\u00e9phas\\u00e9e en r\\u00e9ponse aux variations temporelles de la temp\\u00e9rature ext\\u00e9rieure.<br \/>\\n<br \/>Bien comprendre la r\\u00e9ponse thermique du karst au changement climatique est donc fondamental pour quantifier les taux de dissolution\\\/pr\\u00e9cipitation et interpr\\u00e9ter les variations g\\u00e9ochimiques observ\\u00e9es dans les concr\\u00e9tions, et pour \\u00e9valuer les impacts sur les organismes vivants dans les grottes.<br \/><\\\/p>\\n<span class=\\\"more-text\\\">\\n<br \/>A partir de la litt\\u00e9rature, nous avons formul\\u00e9 trois hypoth\\u00e8ses que nous chercherons \\u00e0 valider dans le projet :\\n\n\n<ol>   \\n\n\n<li>La ventilation des massifs karstiques repr\\u00e9sente un m\\u00e9canisme dominant pour le transfert de chaleur<\\\/li><br \/>\\n\n\n<li>Le temps de r\\u00e9action des massifs et des grottes d\\u00e9pend principalement des flux advectifs (eau et air), plus que de la conduction de chaleur dans la roche<\\\/li><br \/>\\n\n\n<li>Les \\u00e9changes thermiques sont suffisants pour produire une quantit\\u00e9 significative d\\u2019eau de condensation pour recharger les syst\\u00e8mes karstiques, au-moins dans certaines conditions.<\\\/li>\\n<\\\/ol><br \/>\\nL\\u2019objectif du projet est d\\u2019effectuer une analyse approfondie des transferts de masse et de chaleur dans les syst\\u00e8mes karstiques pour r\\u00e9pondre \\u00e0 ces questions. En particulier nous souhaitons caract\\u00e9riser les cons\\u00e9quences d\\u2019un changement climatique sur le milieu souterrain et d\\u00e9terminer la r\\u00e9ponse thermique d\\u2019une cavit\\u00e9 \\u00e0 diff\\u00e9rentes \\u00e9chelles spatiales et temporelles. Nous d\\u00e9velopperons un mod\\u00e8le global simplifi\\u00e9 des massifs karstiques constitu\\u00e9 de plusieurs sous-syst\\u00e8mes (roche, conduit, \\u00e9pikarst\\u2026). Les transferts de chaleur par conduction et advection (eau et air) dans la roche et les conduits seront enti\\u00e8rement coupl\\u00e9s. Cependant, les effets de la ventilation naturelle des grottes, et de l\\u2019\\u00e9pikarst ne sont actuellement pas bien quantifi\\u00e9s, rendant leur mod\\u00e9lisation hasardeuse. Des mesures de terrain seront donc men\\u00e9es parall\\u00e8lement aux simulations.<br \/>\\n\\n <br \/>Pour atteindre cet objectif, le projet s\\u2019appuie sur deux \\u00e9quipes aux comp\\u00e9tences compl\\u00e9mentaires, l\\u2019une sp\\u00e9cialiste du monitoring et de la conceptualisation des syst\\u00e8mes karstiques (ISSKA), l\\u2019autre des transferts de chaleur et de masse (FAST). Ces deux volets seront donc trait\\u00e9s en parall\\u00e8le. Au d\\u00e9but, une \\u00e9tude param\\u00e9trique (mod\\u00e8le initial) sera men\\u00e9e avec des mod\\u00e8les analytiques simplifi\\u00e9s afin d\\u2019estimer la magnitude des processus respectifs sous diff\\u00e9rentes conditions. Ceci permettra de pr\\u00e9ciser le contenu du\\npremier mod\\u00e8le num\\u00e9rique (volet 1) et de l\\u2019acquisition des donn\\u00e9es sur le terrain (volet 2). Les deux volets seront synth\\u00e9tis\\u00e9s it\\u00e9rativement tout au long du programme de recherche, ce qui permettra de discuter les trois hypoth\\u00e8ses \\u00e0 la fin. Deux sites principaux seront instrument\\u00e9s incluant le laboratoire souterrain de Milandre o\\u00f9 de nombreuses donn\\u00e9es sont d\\u00e9j\\u00e0 disponibles. Les sites seront monitor\\u00e9s en temp\\u00e9rature ainsi que pour les principaux param\\u00e8tres contr\\u00f4lant le transfert de masse : flux d\\u2019air et d\\u2019eau en utilisant des mesures directes (d\\u00e9bits) et indirectes (CO2 et radon).<br \/>\\n\\n<br \/>Une \\u00e9quipe de deux doctorants est pr\\u00e9vue pour d\\u00e9ployer le monitoring sur le terrain et d\\u00e9velopper les comp\\u00e9tence et outils de simulation n\\u00e9cessaires au projet. Les chercheurs exp\\u00e9riment\\u00e9s de l\\u2019ISSKA et du FAST soutiendront activement les doctorants pour\\n\\u00e9tablir les proc\\u00e9dures, d\\u00e9velopper les comp\\u00e9tences et prendre les d\\u00e9cisions n\\u00e9cessaires \\u00e0 r\\u00e9soudre les d\\u00e9fis qui se pr\\u00e9senteront.<br \/>\\n\\n<br \/>Ce projet apportera incontestablement des informations nouvelles sur la r\\u00e9ponse des massifs karstiques aux changements climatiques, sur la ventilation des massifs et sur l\\u2019importance de la condensation pour la recharge des aquif\\u00e8res.<br \/>\\n\\n <br \/>Les r\\u00e9sultats du projet apporteront aussi des donn\\u00e9es essentielles pour d\\u2019autres domaines : l\\u2019alimentation en eau potable (variations de temp\\u00e9rature des sources karstiques), sant\\u00e9 publique (radon exhal\\u00e9 dans les habitations), la sp\\u00e9l\\u00e9ogen\\u00e8se (corrosion par condensation), le permafrost (glaci\\u00e8res naturelles), la g\\u00e9othermie basse temp\\u00e9rature (effet des conduits sur les \\u00e9changes thermiques), le percement de tunnels et de mines (pr\\u00e9diction de vides et d\\u2019intrusions massives d\\u2019eau), la t\\u00e9l\\u00e9d\\u00e9tection (interpr\\u00e9tation d\\u2019anomalies thermiques), la conservation des grottes (protection des grottes arch\\u00e9ologiques et touristiques), le cycle du carbone (la dissolution et la pr\\u00e9cipitation des carbonates sont contr\\u00f4l\\u00e9es par la pCO2, donc par la ventilation), la biologie souterraine (biotopes\\nsouterrains)\\u2026<br \/>\\n\\n<br \/>Les r\\u00e9sultats de ce projet deviendront une \\u00e9tape-cl\\u00e9 dans la compr\\u00e9hension des transferts de chaleur dans les roches carbonat\\u00e9es.\\n<br \/>\\n<br \/>\\n<span><a href=\\\"https:\\\/\\\/data.snf.ch\\\/grants\\\/grant\\\/188636\\\" data-wplink-url-error=\\\"true\\\" target=\\\"_blank\\\" rel=\\\"noopener\\\">Lien vers la page FNS Thermokarst<\\\/a><\\\/span>\\n<\\\/span>\\n     \\t<\\\/span>\\n    <\\\/div>\\n    <button class=\\\"show-more-button\\\">Show more<\\\/button>\\n\\n\"}},{\"type\":\"image\",\"props\":{\"image\":\"wp-content\\\/uploads\\\/2024\\\/12\\\/domain_3-scaled.jpeg\",\"image_svg_color\":\"emphasis\",\"margin\":\"default\"}},{\"type\":\"image\",\"props\":{\"image\":\"wp-content\\\/uploads\\\/2024\\\/12\\\/m0-scaled.jpg\",\"image_svg_color\":\"emphasis\",\"margin\":\"default\"}}]}]},{\"type\":\"row\",\"children\":[{\"type\":\"column\",\"props\":{\"image_position\":\"center-center\",\"position_sticky_breakpoint\":\"m\"},\"children\":[{\"type\":\"headline\",\"props\":{\"content\":\"PHD Students\",\"title_element\":\"h1\"}},{\"type\":\"fragment\",\"props\":{\"margin\":\"default\"},\"children\":[{\"type\":\"row\",\"props\":{\"layout\":\"1-2,1-2\"},\"children\":[{\"type\":\"column\",\"props\":{\"image_position\":\"center-center\",\"position_sticky_breakpoint\":\"m\",\"width_medium\":\"1-2\"},\"children\":[{\"type\":\"panel\",\"props\":{\"content\":\"\n\n<h3 style=\\\"text-align: center;\\\"><br \\\/>Contact<\\\/h3>\\n\n\n<p style=\\\"text-align: center;\\\"><a href=\\\"https:\\\/\\\/devw.isska.ch\\\/wp-admin\\\/admin-ajax.php?action=kernel&amp;p=customizer&amp;site=https%3A%2F%2Fdevw.isska.ch%2Ffr%2Fcompetences%2Fformation-et-mediation%2F\\\" aria-label=\\\"Select Image\\\" class=\\\"uk-position-cover\\\"><\\\/a><img src=\\\"https:\\\/\\\/devw.isska.ch\\\/wp-content\\\/uploads\\\/2024\\\/01\\\/Amir_nb-225x300.jpg\\\" alt=\\\"\\\" width=\\\"225\\\" height=\\\"300\\\" class=\\\"alignnone wp-image-611 size-medium\\\" \\\/><\\\/p>\\n\n\n<p style=\\\"text-align: center;\\\">Amir Sedaghatkish<br \\\/><a href=\\\"mailto:amir.sedaghatkish@isska.ch\\\">Envoyer e-mail<\\\/a><\\\/p>\\n\n\n<p><\\\/p>\",\"content_column_breakpoint\":\"m\",\"css\":\".el-element {\\n    text-align: justify;\\n    font-family: 'Century Gothic', Verdana, sans-serif;\\n\\n}\",\"icon_width\":80,\"image\":\"\",\"image_align\":\"top\",\"image_grid_breakpoint\":\"m\",\"image_grid_width\":\"1-2\",\"image_svg_color\":\"emphasis\",\"image_width\":200,\"link_style\":\"default\",\"link_text\":\"Read more\",\"margin\":\"default\",\"meta_align\":\"below-title\",\"meta_element\":\"div\",\"meta_style\":\"text-meta\",\"panel_style\":\"card-default\",\"title_align\":\"top\",\"title_element\":\"h3\",\"title_grid_breakpoint\":\"m\",\"title_grid_width\":\"1-2\",\"title_hover_style\":\"reset\"},\"name\":\"Contact_Comp\"}]},{\"type\":\"column\",\"props\":{\"image_position\":\"center-center\",\"position_sticky_breakpoint\":\"m\",\"width_medium\":\"1-2\"},\"children\":[{\"type\":\"panel\",\"props\":{\"content\":\"\n\n<h3 style=\\\"text-align: center;\\\"><br \\\/>Contact<\\\/h3>\\n\n\n<p style=\\\"text-align: center;\\\"><a href=\\\"https:\\\/\\\/devw.isska.ch\\\/wp-admin\\\/admin-ajax.php?action=kernel&amp;p=customizer&amp;site=https%3A%2F%2Fdevw.isska.ch%2Ffr%2Fcompetences%2Fformation-et-mediation%2F\\\" aria-label=\\\"Select Image\\\" class=\\\"uk-position-cover\\\"><\\\/a><img src=\\\"https:\\\/\\\/devw.isska.ch\\\/wp-content\\\/uploads\\\/2024\\\/01\\\/Claudio_nb-225x300.jpg\\\" alt=\\\"\\\" width=\\\"225\\\" height=\\\"300\\\" class=\\\"alignnone wp-image-612 size-medium\\\" \\\/><\\\/p>\\n\n\n<p style=\\\"text-align: center;\\\">Claudio Pastore<br \\\/><a href=\\\"mailto:claudio.pastore@isska.ch\\\">Envoyer e-mail<\\\/a><\\\/p>\\n\n\n<p><\\\/p>\",\"content_column_breakpoint\":\"m\",\"css\":\".el-element {\\n    text-align: justify;\\n    font-family: 'Century Gothic', Verdana, sans-serif;\\n\\n}\",\"icon_width\":80,\"image\":\"\",\"image_align\":\"top\",\"image_grid_breakpoint\":\"m\",\"image_grid_width\":\"1-2\",\"image_svg_color\":\"emphasis\",\"image_width\":200,\"link_style\":\"default\",\"link_text\":\"Read more\",\"margin\":\"default\",\"meta_align\":\"below-title\",\"meta_element\":\"div\",\"meta_style\":\"text-meta\",\"panel_style\":\"card-default\",\"title_align\":\"top\",\"title_element\":\"h3\",\"title_grid_breakpoint\":\"m\",\"title_grid_width\":\"1-2\",\"title_hover_style\":\"reset\"},\"name\":\"Contact_Comp\"}]}]}]}]}]},{\"type\":\"row\",\"children\":[{\"type\":\"column\",\"props\":{\"image_position\":\"center-center\",\"position_sticky_breakpoint\":\"m\"},\"children\":[{\"type\":\"headline\",\"props\":{\"content\":\"PIs\",\"title_element\":\"h1\"}},{\"type\":\"text\",\"props\":{\"column_breakpoint\":\"m\",\"content\":\"\n\n<p><span>Pierre-Yves Jeannin (ISSKA), Fr\\u00e9d\\u00e9ric Doumenc (Sorbonne), Marc Luetscher (ISSKA).<\\\/span><\\\/p>\",\"margin\":\"default\"}}]}]},{\"type\":\"row\",\"children\":[{\"type\":\"column\",\"props\":{\"image_position\":\"center-center\",\"position_sticky_breakpoint\":\"m\"},\"children\":[{\"type\":\"headline\",\"props\":{\"content\":\"Publications\",\"title_element\":\"h1\"}},{\"type\":\"text\",\"props\":{\"column_breakpoint\":\"m\",\"content\":\"\n\n<p class=\\\"\\\"><span lang=\\\"EN-US\\\">Sedaghatkish A., Doumenc F., Jeannin PY.,<span>\\u00a0<\\\/span><span>Luetscher M.<\\\/span>, 2024. Modeling the effect of free convection on permafrost melting rates in frozen rock-clefts.<span>\\u00a0<\\\/span><i>The Cryospher<\\\/i>e, 18, 4547\\u20134565,<span>\\u00a0<\\\/span><a class=\\\"defaultMailLink defaultMailLink\\\" href=\\\"http:\\\/\\\/doi.org\\\/10.5194\\\/tc-18-4547-2024\\\" target=\\\"_blank\\\" rel=\\\"noopener noreferrer\\\" data-ik=\\\"ik-secure\\\">doi.org\\\/10.5194\\\/tc-18-4547-2024<\\\/a><\\\/span><\\\/p>\\n\n\n<p class=\\\"\\\"><span lang=\\\"EN-US\\\">Pastore C., Sedaghatkish A., Schmid N., Weber E.,<span>\\u00a0<\\\/span><span>Luetscher M.<\\\/span>, 2024. Monitoring air fluxes in caves using digital flow meters.<span>\\u00a0<\\\/span><i>International Journal of Speleology, 53, 63-73.<span>\\u00a0<\\\/span><\\\/i><a class=\\\"defaultMailLink defaultMailLink\\\" href=\\\"http:\\\/\\\/doi.org\\\/10.5038\\\/1827-806X.53.1.2500\\\" target=\\\"_blank\\\" rel=\\\"noopener noreferrer\\\" data-ik=\\\"ik-secure\\\">doi.org\\\/10.5038\\\/1827-806X.53.1.2500<\\\/a><\\\/span><\\\/p>\\n\n\n<p class=\\\"\\\"><span lang=\\\"EN-US\\\">Sedaghatkish A., Pastore C., Doumenc F., Jeannin PY.,<span>\\u00a0<\\\/span><span>Luetscher M.<\\\/span>, 2024. Modelling heat transfer for assessing the convection length in ventilated caves.<span>\\u00a0<\\\/span><i>Journal of Geophysical Research: Earth Surface<\\\/i>, 129, e2024JF007646.<\\\/span><span lang=\\\"EN-US\\\"><span>\\u00a0<\\\/span><\\\/span><span lang=\\\"FR\\\"><a class=\\\"defaultMailLink\\\" href=\\\"https:\\\/\\\/doi.org\\\/10.1029\\\/2024JF007646\\\" target=\\\"_blank\\\" rel=\\\"noopener noreferrer\\\" data-ik=\\\"ik-secure\\\"><span lang=\\\"EN-US\\\">doi.org\\\/10.1029\\\/2024JF007646<\\\/span><\\\/a><\\\/span><span lang=\\\"EN-US\\\"><\\\/span><\\\/p>\\n\n\n<p class=\\\"\\\"><span lang=\\\"EN-US\\\">Pastore C., Weber E., Doumenc F., Jeannin PY.,<span>\\u00a0<\\\/span><span>Luetscher M.<\\\/span>, 2024. Dispersion of artificial tracers in ventilated caves.<span>\\u00a0<\\\/span><i>International Journal of Speleology<\\\/i>, 53(1), 51-62.<span>\\u00a0<\\\/span><a class=\\\"defaultMailLink defaultMailLink\\\" href=\\\"http:\\\/\\\/doi.org\\\/10.5038\\\/1827-806X.53.1.2497\\\" target=\\\"_blank\\\" rel=\\\"noopener noreferrer\\\" data-ik=\\\"ik-secure\\\">doi.org\\\/10.5038\\\/1827-806X.53.1.2497<\\\/a><\\\/span><\\\/p>\\n\n\n<p class=\\\"\\\"><span lang=\\\"EN-US\\\">Garagnon J.,<span>\\u00a0<\\\/span><span>Luetscher M.<\\\/span>, Weber E., 2022. Ventilation regime in a karstic system (Milandre Cave, Switzerland).<span>\\u00a0<\\\/span><i>Karstologia M\\u00e9moires<\\\/i>, 23, 187-19<\\\/span><\\\/p>\",\"margin\":\"default\"}}]}]}]}],\"version\":\"4.3.5\"} --><\/p><\/div>","protected":false},"excerpt":{"rendered":"<p>Wer sind wir&nbsp;? Kom\u00adpe\u00adten\u00adzen Leis\u00adtun\u00adgen Ther\u00admo\u00adKarst Unte\u00adrir\u00addische Hohlr\u00e4ume sind ein emp\u00adfind\u00adliches \u00d6ko\u00adsys\u00adtem, in dem bio\u00adgeo\u00adche\u00admische Pro\u00adzesse stark von der Tem\u00adpe\u00adra\u00adtur abh\u00e4n\u00adgen. Sie beher\u00adber\u00adgen auch ein\u00adzi\u00adgar\u00adtige Spu\u00adren ihrer ver\u00adgan\u00adge\u00adnen Umwelt, deren Inter\u00adpre\u00adta\u00adtion eng mit der Tem\u00adpe\u00adra\u00adtur verkn\u00fcpft ist. In den letz\u00adten Jah\u00adren haben sich viele Stu\u00addien auf Spel\u00e4o\u00adtheme kon\u00adzen\u00adtriert, sekund\u00e4re Kar\u00adbo\u00adnat\u00adfor\u00adma\u00adtio\u00adnen wie [\u2026].<\/p>","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"wp_typography_post_enhancements_disabled":false,"footnotes":""},"categories":[],"tags":[],"class_list":["post-2818","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/devw.isska.ch\/de\/wp-json\/wp\/v2\/pages\/2818","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/devw.isska.ch\/de\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/devw.isska.ch\/de\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/devw.isska.ch\/de\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/devw.isska.ch\/de\/wp-json\/wp\/v2\/comments?post=2818"}],"version-history":[{"count":22,"href":"https:\/\/devw.isska.ch\/de\/wp-json\/wp\/v2\/pages\/2818\/revisions"}],"predecessor-version":[{"id":2982,"href":"https:\/\/devw.isska.ch\/de\/wp-json\/wp\/v2\/pages\/2818\/revisions\/2982"}],"wp:attachment":[{"href":"https:\/\/devw.isska.ch\/de\/wp-json\/wp\/v2\/media?parent=2818"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/devw.isska.ch\/de\/wp-json\/wp\/v2\/categories?post=2818"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/devw.isska.ch\/de\/wp-json\/wp\/v2\/tags?post=2818"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}