{"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\/\">Di\u00adenst\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>Un\u00adte\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 be\u00adher\u00adber\u00adgen auch ein\u00adzi\u00adgar\u00adtige Spu\u00adren ih\u00adrer ver\u00adgan\u00adge\u00adnen Um\u00adwelt, de\u00adren In\u00adter\u00adpre\u00adta\u00adtion eng mit der Tem\u00adpe\u00adra\u00adtur verkn\u00fcpft ist.<\/p>\n<p>In den letz\u00adten Jah\u00adren ha\u00adben sich viele Stu\u00addien auf Spel\u00e4o\u00adtheme, se\u00adkund\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 In\u00adfor\u00adma\u00adtio\u00adnen zu ar\u00adchi\u00advie\u00adren, die ge\u00adnau auf die letz\u00adten 0,5 Ma da\u00adtiert wer\u00adden k\u00f6n\u00adnen. Meh\u00adrere Me\u00adcha\u00adnis\u00admen, da\u00adrun\u00adter die W\u00e4r\u00adme\u00addif\u00adfu\u00adsion im um\u00adge\u00adben\u00adden Ge\u00adstein und die Ad\u00advek\u00adtion durch Was\u00adser und Luft, \u00fcber\u00adtra\u00adgen W\u00e4rme von der Au\u00dfen\u00adfl\u00e4che in den Hohl\u00adraum. Je nach der re\u00adla\u00adti\u00adven Be\u00addeu\u00adtung die\u00adser ver\u00adschie\u00adde\u00adnen Fl\u00fcsse wird die un\u00adte\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 we\u00adni\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 da\u00adher grund\u00adle\u00adgend, um die Au\u00adfl\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 in\u00adter\u00adpre\u00adtie\u00adren und die Aus\u00adwir\u00adkun\u00adgen auf die le\u00adben\u00adden Or\u00adga\u00adnis\u00admen in den H\u00f6h\u00adlen zu be\u00adwer\u00adten.<\/p>\n<p><span class=\"more-text\"><br>\n<br>Aus\u00adge\u00adhend von der Li\u00adte\u00adra\u00adtur ha\u00adben wir drei Hy\u00adpo\u00adthe\u00adsen for\u00admu\u00adliert, die wir im Pro\u00adjekt zu va\u00adli\u00addie\u00adren su\u00adchen:<\/span><\/p>\n<ol>\n<li>Die Bel\u00fcf\u00adtung von Karst\u00admas\u00adsi\u00adven stellt ei\u00adnen do\u00admi\u00adnie\u00adren\u00adden Me\u00adcha\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 ad\u00advek\u00adti\u00adven Str\u00f6\u00admun\u00adgen (Was\u00adser und Luft) ab, mehr als von der W\u00e4r\u00adme\u00adlei\u00adtung im Ge\u00adstein.<\/li>\n<p><\/p>\n<li>Der W\u00e4r\u00admeaus\u00adtausch reicht aus, um zu\u00admin\u00addest un\u00adter bes\u00adtimm\u00adten Be\u00addin\u00adgun\u00adgen eine si\u00adgni\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 un\u00adte\u00adrir\u00addische Um\u00adwelt cha\u00adrak\u00adte\u00adri\u00adsie\u00adren und die ther\u00admische Reak\u00adtion ei\u00adner H\u00f6hle auf ver\u00adschie\u00adde\u00adnen r\u00e4um\u00adli\u00adchen und zeit\u00adli\u00adchen Ska\u00adlen bes\u00adtim\u00admen. Wir wer\u00adden ein ve\u00adrein\u00adfachtes glo\u00adbales Mo\u00addell der Karst\u00admas\u00adsive ent\u00adwi\u00adckeln, das aus meh\u00adre\u00adren Sub\u00adsys\u00adte\u00admen (Ge\u00adstein, Lei\u00adtung, Epi\u00adkarst...) bes\u00adteht. Die W\u00e4r\u00adme\u00fc\u00adber\u00adtra\u00adgung durch Lei\u00adtung und Ad\u00advek\u00adtion (Was\u00adser und Luft) im Ge\u00adstein und in den Lei\u00adtun\u00adgen wird voll\u00adst\u00e4n\u00addig ge\u00adkop\u00adpelt sein. Al\u00adler\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 Mo\u00addel\u00adlie\u00adrung ris\u00adkant macht. Da\u00adher wer\u00adden pa\u00adral\u00adlel zu den Si\u00admu\u00adla\u00adtio\u00adnen Feld\u00admes\u00adsun\u00adgen durch\u00adgef\u00fchrt.<\/p>\n<p>Um dieses Ziel zu er\u00adrei\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 Mo\u00adni\u00adto\u00adring und die Kon\u00adzep\u00adtua\u00adli\u00adsie\u00adrung von Karst\u00adsys\u00adte\u00admen (ISSKA), das an\u00addere auf W\u00e4rme- und Stoff\u00fc\u00adber\u00adtra\u00adgung (FAST). Diese bei\u00adden Teil\u00adbe\u00adreiche wer\u00adden da\u00adher pa\u00adral\u00adlel bear\u00adbei\u00adtet. Zu Be\u00adginn wird eine pa\u00adra\u00adme\u00adtrische Stu\u00addie (Aus\u00adgang\u00adsmo\u00addell) mit ve\u00adrein\u00adfach\u00adten ana\u00adly\u00adti\u00adschen Mo\u00addel\u00adlen durch\u00adgef\u00fchrt, um die Gr\u00f6\u00dfe der je\u00adwei\u00adli\u00adgen Pro\u00adzesse un\u00adter ver\u00adschie\u00adde\u00adnen Be\u00addin\u00adgun\u00adgen ab\u00adzu\u00adsch\u00e4t\u00adzen. Dies wird es erm\u00f6\u00adgli\u00adchen, den In\u00adhalt des<br>\ners\u00adten nu\u00adme\u00adri\u00adschen Mo\u00addells (Teil 1) und der Da\u00adte\u00adner\u00adfas\u00adsung im Feld (Teil 2). Die bei\u00adden Teile wer\u00adden im Laufe des For\u00adschung\u00adspro\u00adgramms ite\u00adra\u00adtiv zu\u00adsam\u00admen\u00adge\u00adfasst, so\u00addass am Ende alle drei Hy\u00adpo\u00adthe\u00adsen dis\u00adku\u00adtiert wer\u00adden k\u00f6n\u00adnen. Zwei Haupts\u00adtan\u00addorte wer\u00adden ins\u00adtru\u00admen\u00adtiert, da\u00adrun\u00adter das un\u00adte\u00adrir\u00addische La\u00adbor von Mi\u00adlandre, wo be\u00adreits zahl\u00adreiche Da\u00adten vor\u00adlie\u00adgen. Die Stan\u00addorte wer\u00adden hin\u00adsicht\u00adlich der Tem\u00adpe\u00adra\u00adtur so\u00adwie der wich\u00adtig\u00adsten Pa\u00adra\u00adme\u00adter, die den Mas\u00adsen\u00adtrans\u00adfer kon\u00adtrol\u00adlie\u00adren, \u00fcber\u00adwacht: Luft- und Was\u00adser\u00adfluss durch di\u00adrekte (Dur\u00adch\u00adfluss\u00adra\u00adten) und in\u00addi\u00adrekte (CO2 und Ra\u00addon) Mes\u00adsun\u00adgen.<\/p>\n<p>Ein Team von zwei Dok\u00adto\u00adran\u00adden soll das Mo\u00adni\u00adto\u00adring vor Ort ein\u00adset\u00adzen und die f\u00fcr das Pro\u00adjekt er\u00adfor\u00adder\u00adli\u00adchen Kom\u00adpe\u00adten\u00adzen und Si\u00admu\u00adla\u00adtions\u00adwerk\u00adzeuge ent\u00adwi\u00adckeln. Er\u00adfah\u00adrene For\u00adscher des SISKA und des FAST wer\u00adden die Dok\u00adto\u00adran\u00adden ak\u00adtiv un\u00adterst\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\u00f6\u00adsung der ans\u00adte\u00adhen\u00adden He\u00adraus\u00adfor\u00adde\u00adrun\u00adgen er\u00adfor\u00adder\u00adlich sind.<\/p>\n<p>Dieses Pro\u00adjekt wird zwei\u00adfel\u00adlos neue Er\u00adkennt\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 Be\u00addeu\u00adtung der Kon\u00adden\u00adsa\u00adtion f\u00fcr die Auff\u00fcl\u00adlung von Grund\u00adwas\u00adser\u00adlei\u00adtern lie\u00adfern.<\/p>\n<p>Die Er\u00adgeb\u00adnisse des Pro\u00adjekts wer\u00adden auch wich\u00adtige Da\u00adten f\u00fcr an\u00addere Be\u00adreiche lie\u00adfern: Trink\u00adwas\u00adser\u00adver\u00adsor\u00adgung (Tem\u00adpe\u00adra\u00adtur\u00adsch\u00adwan\u00adkun\u00adgen von Karst\u00adquel\u00adlen), \u00f6f\u00adfent\u00adliche Ge\u00adsund\u00adheit (aus\u00adgeat\u00admetes Ra\u00addon in Wohnh\u00e4u\u00adsern), Spel\u00e4o\u00adge\u00adnese (Kor\u00adro\u00adsion durch Kon\u00adden\u00adsa\u00adtion), Per\u00adma\u00adfrost (nat\u00fcr\u00adliche Ei\u00adsh\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 Mi\u00adnen\u00adbau (Vo\u00adrher\u00adsage von Hohlr\u00e4u\u00admen und mas\u00adsi\u00adven Was\u00adse\u00adrin\u00adtru\u00adsio\u00adnen), Fer\u00adner\u00adkun\u00addung (In\u00adter\u00adpre\u00adta\u00adtion ther\u00admi\u00adscher Ano\u00adma\u00adlien), H\u00f6h\u00adle\u00adne\u00adrhal\u00adtung (Schutz ar\u00adch\u00e4o\u00adlo\u00adgi\u00adscher und tou\u00adris\u00adti\u00adscher H\u00f6h\u00adlen), Koh\u00adlens\u00adtoff\u00adkreis\u00adlauf (Au\u00adfl\u00f6\u00adsung und Ausf\u00e4l\u00adlung von Kar\u00adbo\u00adna\u00adten wer\u00adden durch den pCO2-Wert, al\u00adso durch die Ven\u00adti\u00adla\u00adtion, ges\u00adteuert), un\u00adte\u00adrir\u00addische Bio\u00adlo\u00adgie (Bio\u00adtope<br>\nun\u00adte\u00adrir\u00addisch)...<\/p>\n<p>Die Er\u00adgeb\u00adnisse dieses Pro\u00adjekts wer\u00adden zu ei\u00adnem 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 Se\u00adda\u00adghat\u00adkish<br><a href=\"mailto:amir.sedaghatkish@isska.ch\">E-Mail 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-Mail 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\">Se\u00adda\u00adghat\u00adkish A., Dou\u00admenc F., Jean\u00adnin PY.,<span>&nbsp;<\/span><span>Luet\u00adscher M.<\/span>, 2024. Mo\u00adde\u00adling the ef\u00adfect 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, 4547-4565,<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-18-4547-2024<\/a><\/span><\/p>\n<p class><span lang=\"EN-US\">Pas\u00adtore C., Se\u00adda\u00adghat\u00adkish A., Schmid N., We\u00adber E.,<span>&nbsp;<\/span><span>Luet\u00adscher M.<\/span>, 2024. Mo\u00adni\u00adto\u00adring air fluxes in caves using di\u00adgi\u00adtal flow me\u00adters.<span>&nbsp;<\/span><i>In\u00adter\u00adna\u00adtio\u00adnal Jour\u00adnal of Spe\u00adleo\u00adlo\u00adgy, 53, 63-73.<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\/1827-806X.53.1.2500<\/a><\/span><\/p>\n<p class><span lang=\"EN-US\">Se\u00adda\u00adghat\u00adkish A., Pas\u00adtore C., Dou\u00admenc F., Jean\u00adnin PY.,<span>&nbsp;<\/span><span>Luet\u00adscher M.<\/span>, 2024. Mo\u00addel\u00adling heat trans\u00adfer for as\u00adses\u00adsing the convec\u00adtion length in ven\u00adti\u00adla\u00adted caves.<span>&nbsp;<\/span><i>Jour\u00adnal of Geo\u00adphy\u00adsi\u00adcal Re\u00adsearch: Earth Sur\u00adface (Jour\u00adnal f\u00fcr geo\u00adphy\u00adsi\u00adka\u00adlische For\u00adschung: Er\u00addo\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., We\u00adber 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>In\u00adter\u00adna\u00adtio\u00adnal Jour\u00adnal of Spe\u00adleo\u00adlo\u00adgy<\/i>, 53(1), 51-62.<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\/1827-806X.53.1.2497<\/a><\/span><\/p>\n<p class><span lang=\"EN-US\">Ga\u00adra\u00adgnon J,<span>&nbsp;<\/span><span>Luet\u00adscher M.<\/span>, We\u00adber E., 2022. Ven\u00adti\u00adla\u00adtion re\u00adgime in a kars\u00adtic sys\u00adtem (Mi\u00adlandre Cave, Swit\u00adzer\u00adland).<span>&nbsp;<\/span><i>Kars\u00adto\u00adlo\u00adgia Me\u00admoi\u00adren<\/i>, 23, 187-19<\/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? Kom\u00adpe\u00adten\u00adzen Leis\u00adtun\u00adgen Ther\u00admo\u00adKarst Un\u00adte\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 be\u00adher\u00adber\u00adgen auch ein\u00adzi\u00adgar\u00adtige Spu\u00adren ih\u00adrer ver\u00adgan\u00adge\u00adnen Um\u00adwelt, de\u00adren In\u00adter\u00adpre\u00adta\u00adtion eng mit der Tem\u00adpe\u00adra\u00adtur verkn\u00fcpft ist. In den letz\u00adten Jah\u00adren ha\u00adben sich viele Stu\u00addien auf Spel\u00e4o\u00adtheme kon\u00adzen\u00adtriert, se\u00adkund\u00e4re Kar\u00adbo\u00adnat\u00adfor\u00adma\u00adtio\u00adnen wie [...].<\/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}]}}