Pregled bibliografske jedinice broj: 680475
Seasonal variation of oxic-anoxic conditions in the small, seawater lake (Rogoznica Lake, East Adriatic Coast) related to the global climate changes
Seasonal variation of oxic-anoxic conditions in the small, seawater lake (Rogoznica Lake, East Adriatic Coast) related to the global climate changes // Water in the Mediterranean Basin / Gökçekus, Hüseyin ; Türker, Umut ; LaMoreaux, James W. (ur.).
Berlin : Heidelberg: Springer, 2011. str. 230-240
CROSBI ID: 680475 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Seasonal variation of oxic-anoxic conditions in the small, seawater lake (Rogoznica Lake, East Adriatic Coast) related to the global climate changes
Autori
Ciglenečki, Irena ; Bura-Nakić, Elvira ; Carić, Marina ; Kršinić, Frane ; Viličić, Damir ; Burić, Zrinka ; Ćosović, Božena
Vrsta, podvrsta i kategorija rada
Poglavlja u knjigama, ostalo
Knjiga
Water in the Mediterranean Basin
Urednik/ci
Gökçekus, Hüseyin ; Türker, Umut ; LaMoreaux, James W.
Izdavač
Springer
Grad
Berlin : Heidelberg
Godina
2011
Raspon stranica
230-240
ISBN
978-3-642-20335-0
Ključne riječi
karstic seawater lake, Rogoznica Lake, anoxia, reduced sulfur species, dissolved
Sažetak
Long term investigation of the Rogoznica Lake (since 1994 seasonal variations of temperature, salinity, dissolved oxygen, nutrients, dissolved organic carbon, surface-active substances, reduced sulfur species, phytoplankton and zoo-plankton have been investigated) showed that main physical- chemical characteristic of the Lake is occurrence of well-defined seasonal stratification of water column as well as occurrence of anoxic conditions in deeper water layers (>10 m). During spring and summer surface water is well-oxygenated with intensive primaryproduction processes and bottom anoxic layer is characterized by high concentrations of sulfur compounds, nutrients and dissolved organic matter. The depth of anoxic water layer changessea sonally and it is greatly influenced by meteorological conditions, i.e. temperature and rainfall. Vertical mixing occurs during winter when cold, oxygen-rich water from the surface sinks downwards. As a result of mixing, bottom water enriched with nutrients is coming to the surface supporting new phytoplankton and oxygen productions. Results of recent investigations (since 2001 up to now) have showed significant change of organic matter properties what is a consequence of changes in phytoplankton abundance and composition. Also, recent investigations have showed significant change in hydrographic conditions, i.e. temperature and salinity what we believe is closely related with global climate changes
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
098-0982934-2717 - Priroda organske tvari, interakcije s mikrokonstituentima i površinama u okolišu (Ciglenečki-Jušić, Irena, MZOS ) ( CroRIS)
Ustanove:
Institut "Ruđer Bošković", Zagreb
Profili:
Božica Ciglenečki
(autor)
Irena Ciglenečki-Jušić
(autor)
Damir Viličić
(autor)
Elvira Bura-Nakić
(autor)
Frano Kršinić
(autor)
Božena Ćosović
(autor)
Marina Carić-Glunčić
(autor)