Hidrogeološke značajke sliva rijeke Korane na području između Slunja i Velemerića

master's thesis

• Title: Hidrogeološke značajke sliva rijeke Korane na području između Slunja i Velemerića : diplomski rad
• Title (english): Hydrogeological characteristics of Korana river catchment area between Slunj and Velemerić : master's thesis
• Author: Sara Vuković
• Mentor: Jelena Parlov (mentor)
• Committee member: Jelena Parlov
• Committee member: Andrea Bačani
• Committee member: Dario Perković
• Granter: University of Zagreb; Faculty of Mining, Geology and Petroleum Engineering; (Department of Geology and Geological Engineering); Zagreb
• Defense date and country: 2014-09-25, Croatia
• Scientific / art field, discipline and subdiscipline: TECHNICAL SCIENCES; Mining, Petroleum and Geology Engineering; Geological Engineering

Abstract

Krš je krajolik specifičnih površinskih i podzemnih formi te nastaje kao rezultat strukturno-tektonskih
i kemijskih procesa koji utječu na topive sedimentne stijene. Na oblikovanje krškog reljefa utječu i
klima te pedološke i vegetacijske osobine određenog područja. U ovom diplomskom radu promatra se
područje između Slunja i Velemerića koje je zanimljivo, jer tu rijeka Korana djeluje kao dren
podzemne vode. Na temelju dosadašnjih spoznaja o geološkim, strukturno-tektonskim i
hidrogeološkim odnosima opisano je područje oko rijeke Korane, te je određena granica i površina
sliva prema navedenim značajkama. Hidrogeološka uloga rijeke Korane protumačena je i pomoću
bilance vode, gdje je, prema izračunatim podacima, dobiven odnos ulaza i izlaza vode iz priljevnog
područja. Dobiven je pozitivan odnos, ΔQ = + 1,70 m3/s, što ukazuje na višak vode u sustavu, odnosno
veći izlaz vode od ulaza. Višak vode može biti posljedica podzemnih dotoka u sliv, odnosno premale
površine priljevnog područja. Može se pretpostaviti da neki vodotoci koje smo izostavili iz sliva na
temelju topografije ipak pripadaju slivu Korane, primjerice sliv potoka Surdup. Hidrogeološki odnosi
na zapadnoj granici priljevnog područja daju mogućnost potrebnog proširenja površine sliva za oko 50
km2.

Abstract (english)

Abstract: Karst is a landscape with a specific surface and underground forms, which occurs as a result of
structural-tectonic and chemical processes that influence soluble sedimentary rocks. The formation of
the karst topography is also influenced by the climate, soil and vegetation of a particular area. This
thesis deals with a catchment area of the Korana River between Slunj and Velemerić which is
interesting because the Korana River in this area functions as the drain of the groundwater. Based on
recent studies of geological, structural-tectonic and hydrogeological relations, the area around the
Korana River is described and the boundary and surface of the basin according to the above mentioned
features is determined. The hydrogeological role of the Korana River is interpreted by using the water
balance, which provided, according to the calculated data, the ratio of input and output of water from
the catchment area. There was a positive ratio, ΔQ = + 1.70 m3 / s, which indicates an excess of water
in the system or a larger output of water than the input. Excess water could be the result of
groundwater inflow into the basin or a small surface area. It can be assumed that some streams that
have been left out of the basin still belong to the basin of the Korana River, like stream Surdup.
Hydrogeology at the western border inflow offers the possibility of extending the catchment area for
about 50 km2.

• Keywords: hidrogeologija; Korana; bilanca voda
• Keywords (english): hydrogeology; river Korana; water balance
• Language: croatian
• URN:NBN: urn:nbn:hr:169:688770
• Study programme: Title: Geological Engineering; Study programme type: university; Study level: graduate; Academic / professional title: magistar/magistra inženjer/inženjerka geološkog inženjerstva (magistar/magistra inženjer/inženjerka geološkog inženjerstva)
• Type of resource: Text
• File origin: Born digital
• Access conditions: Access restricted to students and staff of home institution
• Created on: 2016-01-12 08:36:38