Hidrogeološki odnosi koprivničkih vodocrpilišta

master's thesis

• Title: Hidrogeološki odnosi koprivničkih vodocrpilišta : diplomski rad
• Title (english): Hydrogeological relations among well-fields of Koprivnica : master's thesis
• Author: Karmela Dinčec
• Mentor: Željko Duić (mentor)
• Committee member: Željko Duić
• Committee member: Uroš Barudžija
• 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: 2013-09-26, Croatia
• Scientific / art field, discipline and subdiscipline: TECHNICAL SCIENCES; Mining, Petroleum and Geology Engineering; Geological Engineering

Abstract

Koprivnička vodocrpilišta nalaze se na području Koprivničke Podravine koja pripada strukturnoj
jedinici Dravskog bazena. Crpilišta Ivanščak i Lipovec, smješteni na području Koprivničke
Podravine međusobno se nalaze na relativno maloj udaljenosti, međutim istraživanja su pokazala
različitu geometriju vodonosnika, hidrauličke značajke te razliku u prirodnoj kakvoći podzemne
vode. U ovom diplomskom radu razrađen je utjecaj geoloških struktura na razliku hidrogeoloških
značajki i kakvoće vode između crpilišta Ivanščak i Lipovec. Na crpilištu Ivanščak debljina
vodonosnog kompleksa iznosi oko 40 metara, dok na crpilišu Lipovec debljina iznosi oko 150
metara. Pokazalo se da su uzroci ovih razlika uvjeti taloženja koji ovise o pokretima duž rasjeda,
koji graniče s pojedinim strukturama.

Abstract (english)

Abstract: The well-fields of Koprivnica are located in Koprivnička Podravina that belongs to Drava basin
structural unit. Well-fields Lipovec and Ivanščak, located in Koprivnička Podravina, are positioned
relatively close the each other. However, studies have shown different geometries of two aquifers,
the difference in hydraulic characteristics and the difference in natural groundwater quality as well.
In this paper, the impact of the geological structures on the difference in hydrogeological
characteristics and on the difference in the water quality among the well-fields, Ivanščak and
Lipovec, are elaborated. At the well-field Ivanščak, thickness of the aquifer complex is about 40
meters, while at the well-field Lipovec thickness of the aquifer complex is about 150 meters. It has
been shown that depositional conditions are the main causes of these differences. Changes in
depositional conditions depends on the movements along particular faults, which border the main
geological structures in the area.

• Keywords: crpilište Ivanščak; crpilište Lipovec; geološke strukture; podzemna voda; kakvoća vode
• Keywords (english): wellfield Ivanščak; wellfield Lipovec; geological structures; groundwater; groundwater quality
• Language: croatian
• URN:NBN: urn:nbn:hr:169:154274
• 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: 2016-01-20 13:43:13