Zobrazeno 1 - 10
of 35
pro vyhledávání: '"Lake Vrana"'
Autor:
Lorena Selak, Helena Osterholz, Igor Stanković, Nikola Hanžek, Marija Gligora Udovič, Thorsten Dittmar, Sandi Orlić
In lake ecosystems, changes in eukaryotic and prokaryotic microbes and the concentration and availability of dissolved organic matter (DOM) produced within or supplied to the system by allochthonous sources are components that characterize complex pr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::75580aa5960aad58fc871db72d3f4a1c
https://www.bib.irb.hr/1177633
https://www.bib.irb.hr/1177633
Publikováno v:
Croatian Journal of Fisheries, Vol 67, Iss 3, Pp 101-112 (2009)
The Vrana Lake is a cryptodepression filled with water of about 76 m maximum depth, approximately 5 km long and 1.5 km large, having an area of 5.5 km2. It is situated in the central part of the Cres Island, spreading in the north–south direction.
Externí odkaz:
https://doaj.org/article/5bce4bbd2b454fd6b792657c79ec433e
Publikováno v:
Quaternary International. 494:5-18
The sediment core from Lake Vrana (between 1000 and 500 cm) on the eastern Adriatic coast was analyzed using palynological and geochemical approaches to detect environmental changes during the Holocene. The deepest sediments (between 1000 and 967 cm)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::398e19225b0280877580a6cc17ed158c
https://doi.org/10.1016/j.quaint.2018.06.010
https://doi.org/10.1016/j.quaint.2018.06.010
Autor:
Radanović, Sanja
U ovom diplomskom radu prikazan je hidraulički model funkcioniranja Vranskog jezera koji opisuje promjenu vodostaja u jezeru, uzimajući u obzir dotoke od oborina, podzemne gubitke prema moru, otjecanje kanalom Prosika, potrošnju vode za navodnjava
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______4003::6bff07055413361744efa246740211e8
https://urn.nsk.hr/urn:nbn:hr:123:526738
https://urn.nsk.hr/urn:nbn:hr:123:526738
Autor:
Radanović, Sanja
U ovom diplomskom radu prikazan je hidraulički model funkcioniranja Vranskog jezera koji opisuje promjenu vodostaja u jezeru, uzimajući u obzir dotoke od oborina, podzemne gubitke prema moru, otjecanje kanalom Prosika, potrošnju vode za navodnjava
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______4112::a3598c4203cbd7256a050317df633a07
https://repozitorij.svkst.unist.hr/islandora/object/gradst:1675/datastream/PDF
https://repozitorij.svkst.unist.hr/islandora/object/gradst:1675/datastream/PDF
Publikováno v:
Quaternary International. 494:167-179
The 11 m sediment core of karstic Lake Vrana located at the Dalmatian coast of Eastern Adriatic (Croatia) was investigated through the analyses of diatoms. The diatoms exhibited six marked changes in Diatom Zones (DZ) with included water/sediment int
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1ea22554011b92756a2794deeac9d5f3
https://doi.org/10.1016/j.quaint.2017.09.010
https://doi.org/10.1016/j.quaint.2017.09.010
Publikováno v:
Hydrology and Earth System Sciences, Vol 19, Iss 8, Pp 3653-3666 (2015)
The bathymetric survey of Lake Vrana included a wide range of activities that were performed in several different stages, in accordance with the standards set by the International Hydrographic Organization. The survey was conducted using an integrate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::49eb3fd36102477abac5b6e2d53b4321
https://www.hydrol-earth-syst-sci.net/19/3653/2015/
https://www.hydrol-earth-syst-sci.net/19/3653/2015/
Autor:
Ognjen Bonacci, Tanja Roje-Bonacci
Publikováno v:
Hrvatske vode
Volume 26
Issue 103
Volume 26
Issue 103
U radu je analizirano ponašanje dnevnih razina podzemne vode mjerenih u tri duboka piezometra locirana u slivu Vranskog jezera na otoku Cresu. Obuhvaćeno je razdoblje od 10. rujna 1997. do 31. prosinca 2000., dakle ukupno 1209 dana. Ponašanje razi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______951::709a6c8f1f25033dbb18c21a7694e1cc
https://hrcak.srce.hr/file/290336
https://hrcak.srce.hr/file/290336
Rock relief is an important trace of the formation and development of karst phenomena on various carbonate rock. The existing current state is usually in a rich and diverse stage of homogeneous or heterogeneous development. The various forms of rock
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::06f9d5e9e113279e928fc9d0093b113f
https://www.bib.irb.hr/794869
https://www.bib.irb.hr/794869
The information obtained from all the analysed data (ostracods, pollen, sedimentology and geochemistry) reflects three major periods of changes in the environmental evolution of the lake. According to the composition of the assemblages, five ostracod
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::16fe3090b773ca676402f4a93735e39e
https://www.bib.irb.hr/772263
https://www.bib.irb.hr/772263