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HYDROGEOCHEMICAL CHARACTERISTICS OF THE ST. IVAN SPRING IN ISTRIA, CROATIA

Tatjana Vlahović

Puni tekst: engleski, pdf (2 MB) str. 29-36 preuzimanja: 1.010* citiraj
APA 6th Edition
Vlahović, T. (2000). HYDROGEOCHEMICAL CHARACTERISTICS OF THE ST. IVAN SPRING IN ISTRIA, CROATIA. Rudarsko-geološko-naftni zbornik, 12 (1), 29-36. Preuzeto s https://hrcak.srce.hr/5030
MLA 8th Edition
Vlahović, Tatjana. "HYDROGEOCHEMICAL CHARACTERISTICS OF THE ST. IVAN SPRING IN ISTRIA, CROATIA." Rudarsko-geološko-naftni zbornik, vol. 12, br. 1, 2000, str. 29-36. https://hrcak.srce.hr/5030. Citirano 14.06.2021.
Chicago 17th Edition
Vlahović, Tatjana. "HYDROGEOCHEMICAL CHARACTERISTICS OF THE ST. IVAN SPRING IN ISTRIA, CROATIA." Rudarsko-geološko-naftni zbornik 12, br. 1 (2000): 29-36. https://hrcak.srce.hr/5030
Harvard
Vlahović, T. (2000). 'HYDROGEOCHEMICAL CHARACTERISTICS OF THE ST. IVAN SPRING IN ISTRIA, CROATIA', Rudarsko-geološko-naftni zbornik, 12(1), str. 29-36. Preuzeto s: https://hrcak.srce.hr/5030 (Datum pristupa: 14.06.2021.)
Vancouver
Vlahović T. HYDROGEOCHEMICAL CHARACTERISTICS OF THE ST. IVAN SPRING IN ISTRIA, CROATIA. Rudarsko-geološko-naftni zbornik [Internet]. 2000 [pristupljeno 14.06.2021.];12(1):29-36. Dostupno na: https://hrcak.srce.hr/5030
IEEE
T. Vlahović, "HYDROGEOCHEMICAL CHARACTERISTICS OF THE ST. IVAN SPRING IN ISTRIA, CROATIA", Rudarsko-geološko-naftni zbornik, vol.12, br. 1, str. 29-36, 2000. [Online]. Dostupno na: https://hrcak.srce.hr/5030. [Citirano: 14.06.2021.]

Sažetak
In addition to geological, hydrogeological investigations and groundwater tracing, detailed surveying of the groundwater quality is becoming particularly important for environmental impact monitoring on karst aquifers. Groundwater quality data contain two types of information i.e. the natural chemistry of water and its modifications caused by antropogenic impacts. The method of results presentation as well as the importance of water quality surveying particularly with respect to the indicators showing its natural chemistry, are shown here exemplified by the St. Ivan spring in Istria, Croatia. Natural chemistry of the groundwater is a consequence of hydrogeochemical facies, and it is used here for interpretation of spring generating conditions and the origin of groundwater. Results obtained so far confirm that the extent of recharge area of the spring change in dependence of the hydrological conditions. Hydrogeochemical characteristics of the spring are presented graphically in the form of correlation diagrams showing major groundwater parameters, saturation conditions and trends of particular parameters as a function of time.

Ključne riječi
hydrogeochemistry; karst; groundwater; Istria; Croatia

Hrčak ID: 5030

URI
https://hrcak.srce.hr/5030

[hrvatski]

Posjeta: 1.696 *