{"id":3708,"date":"2020-02-18T02:48:15","date_gmt":"2020-02-18T02:48:15","guid":{"rendered":"http:\/\/crodestinations.com\/hr\/?p=3708"},"modified":"2020-02-26T03:03:00","modified_gmt":"2020-02-26T03:03:00","slug":"voda-rijeke-krke-prirodni-fenomen-u-bezvodnom-dalmatinskom-krsu-foto","status":"publish","type":"post","link":"https:\/\/crodestinations.com\/hr\/voda-rijeke-krke-prirodni-fenomen-u-bezvodnom-dalmatinskom-krsu-foto\/","title":{"rendered":"VODA RIJEKE KRKE: Prirodni fenomen u bezvodnom dalmatinskom kr\u0161u [FOTO]"},"content":{"rendered":"
\"Nacionalni<\/a>
Foto: Pixabay<\/figcaption><\/figure>\n

Vode koje teku i poniru i podzemni putovi kojima se ispreple\u0107u, me\u0111usobno napajaju pa opet izviru posebnost su kr\u0161a. Ni podru\u010dje rijeke Krke nije iznimka, dapa\u010de, 72,5 km rijeke kroz bezvodni kr\u0161 prirodni su fenomen.<\/strong> <\/p>\n

Slatkovodni dio toka rijeke Krke dug je 49 km, a na preostalih 23,5 km osje\u0107a se utjecaj mora. Sa svojim pritocima Krka \u010dini nadzemni slijev povr\u0161ine 2.450 km\u00b2, a s hidrogeolo\u0161kim slijevom zauzima podru\u010dje od 2.650 km\u00b2. Ukupni pad toka iznosi 224 m. <\/p>\n

\"Nacionalni<\/a>
Visovac | Foto: NP Krka<\/figcaption><\/figure>\n

Kr\u0161ka podru\u010dja odlikuje bezvodnost, a prevlast karbonatnih stijena i njihova tektonska razlomljenost pospje\u0161uju poniranje atmosferskih voda u unutra\u0161njost. Rijeka Krka povr\u0161inski te\u010de iznad razina kolebanja temeljnih kr\u0161kih podzemnih voda kao vise\u0107a teku\u0107ica koja na takvoj podlozi ne gubi vodu. <\/p>\n

Za kr\u0161 je svojstvena dinami\u010dna i izravna veza povr\u0161inske i podzemne vode, koja stvara razli\u010dita stani\u0161ta i prenosi hranjive tvari te tako omogu\u0107uje \u017eivot i na povr\u0161ini i u podzemlju. Zato je o\u010duvanje osjetljiva kr\u0161kog ekosustava od najve\u0107e va\u017enosti.<\/p>\n

\"Nacionalni<\/a>
Foto: NP Krka<\/figcaption><\/figure>\n

Kompleksni geolo\u0161ki uvjeti razlog su kompliciranih hidrolo\u0161kih odnosa. Na podru\u010dju rijeke Krke susre\u0107u se dvije megastrukturne jedinice: Dinarik i Adrijatik. Dinarskoj karbonatnoj platformi pripada planinski dio slijeva rijeke Krke do tektonske zone Strmica \u2013 Knin \u2013 Petrovo polje, Jadranskoj karbonatnoj platformi za\u0161ti\u0107eni dio kanjona.<\/p>\n

Najve\u0107i dio karbonatnih naslaga je vodopropustan pa voda ponire u okr\u0161eni reljef, dok manji dio ima funkciju nepropusnih stijena, koje su barijera za podzemne vodene tokove. Zone nepropusnih stijena nalaze se u izvori\u0161nom dijelu, oko Knina i sjevernije od njega, gdje se nalaze izvori, nadzemni i podzemni tokovi koji “prihranjuju” kanjonski dio rijeke Krke. <\/p>\n

Najju\u017eniji kr\u0161ki izvor u toj zoni jest \u010cikola u Petrovu polju. Taj se izvor za su\u0161nih razdoblja ne prelijeva, a za ki\u0161nih formira rijeku. <\/p>\n

Zona vodonepropusnih naslaga ili fli\u0161 prote\u017ee se i na ju\u017enoj granici Parka, oko Skradinskoga buka pa do izvora Torak na u\u0161\u0107u \u010cikole u Krku, a obuhva\u0107a i donji dio Visova\u010dkog jezera. Krka se prihranjuje i podzemnim vodama. Dio tih voda potje\u010de iz dinarskog zale\u0111a (Grahova polja), a dio iz gornjeg porje\u010dja rijeke Zrmanje, s kojom Krka dijeli zajedni\u010dko podzemno vodno lice. Najizda\u0161niji izvori uzdu\u017e kanjona rijeke Krke jesu Miljacka i Jaruga, a u kanjonu rijeke \u010cikole izvor Torak. Nizvodno od Skradinskoga buka izvori\u0161te je Jaruga, a od prukljanskog dijela nizvodno bo\u010dati izvor Litno u Zatonu.<\/p>\n

Porje\u010dje Krke tijekom godine primi oko 1.250 mm oborina. Najvi\u0161e ki\u0161e padne u zimskom razdoblju, dok su ljeta vrlo suha. Vodostaj Krke najvi\u0161i je u studenome i o\u017eujku, a najni\u017ei u kolovozu. <\/p>\n

Srednja vrijednost protoka Krke na izvoru iznosi 12 m\u00b3\/s a na Skradinskom buku 55 m\u00b3\/s. Maksimalna vrijednost protoka, 481 m\u00b3\/s, zabilje\u017eena je 24. prosinca 1982., a minimalna, 4,99 m\u00b3\/s, 5. listopada 1961. Najvi\u0161a temperatura vode na Skradinskom buku, 27,5 \u00b0C, zabilje\u017eena je 25. kolovoza 2011., a najni\u017ea, 3,5 \u00b0C, 12. sije\u010dnja 1985. <\/p>\n

Najve\u0107a vrijednost vodostaja na Skradinskom buku, 223 cm, zabilje\u017eena je 7. prosinca 2005., a minimalna, samo 5 cm, 3. listopada 1990.<\/p>\n

\"Nacionalni<\/a>
Foto: Canva<\/figcaption><\/figure>\n
\"Nacionalni<\/a>
Foto: Canva<\/figcaption><\/figure>\n
\"Nacionalni<\/a>
Foto: Canva<\/figcaption><\/figure>\n","protected":false},"excerpt":{"rendered":"

Vode koje teku i poniru i podzemni putovi kojima se ispreple\u0107u, me\u0111usobno napajaju pa opet<\/p>\n","protected":false},"author":1,"featured_media":3713,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[135,6],"tags":[57,474,655],"class_list":["post-3708","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-nacionalni-parkovi","category-odredista","tag-krka","tag-nacionalni-park-krka","tag-np-krka"],"yoast_head":"\nVODA RIJEKE KRKE: Prirodni fenomen u bezvodnom dalmatinskom kr\u0161u [FOTO] - CROdestinations<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/crodestinations.com\/hr\/voda-rijeke-krke-prirodni-fenomen-u-bezvodnom-dalmatinskom-krsu-foto\/\" \/>\n<meta property=\"og:locale\" content=\"hr_HR\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"VODA RIJEKE KRKE: Prirodni fenomen u bezvodnom dalmatinskom kr\u0161u [FOTO] - 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