hrcak mascot   Srce   HID

Original scientific paper

HYDROGEOLOGICAL RELATIONS ON KARSTIFIED ISLANDS - VIS ISLAND CASE STUDY

JOSIP TERZIĆ

Fulltext: croatian, pdf (953 KB) pages 47-58 downloads: 2.186* cite
APA 6th Edition
TERZIĆ, J. (2004). HIDROGEOLOŠKI ODNOSI NA KRŠKIM OTOCIMA – PRIMJER OTOKA VISA. Rudarsko-geološko-naftni zbornik, 16 (1), 47-58. Retrieved from https://hrcak.srce.hr/13360
MLA 8th Edition
TERZIĆ, JOSIP. "HIDROGEOLOŠKI ODNOSI NA KRŠKIM OTOCIMA – PRIMJER OTOKA VISA." Rudarsko-geološko-naftni zbornik, vol. 16, no. 1, 2004, pp. 47-58. https://hrcak.srce.hr/13360. Accessed 17 Oct. 2019.
Chicago 17th Edition
TERZIĆ, JOSIP. "HIDROGEOLOŠKI ODNOSI NA KRŠKIM OTOCIMA – PRIMJER OTOKA VISA." Rudarsko-geološko-naftni zbornik 16, no. 1 (2004): 47-58. https://hrcak.srce.hr/13360
Harvard
TERZIĆ, J. (2004). 'HIDROGEOLOŠKI ODNOSI NA KRŠKIM OTOCIMA – PRIMJER OTOKA VISA', Rudarsko-geološko-naftni zbornik, 16(1), pp. 47-58. Available at: https://hrcak.srce.hr/13360 (Accessed 17 October 2019)
Vancouver
TERZIĆ J. HIDROGEOLOŠKI ODNOSI NA KRŠKIM OTOCIMA – PRIMJER OTOKA VISA. Rudarsko-geološko-naftni zbornik [Internet]. 2004 [cited 2019 October 17];16(1):47-58. Available from: https://hrcak.srce.hr/13360
IEEE
J. TERZIĆ, "HIDROGEOLOŠKI ODNOSI NA KRŠKIM OTOCIMA – PRIMJER OTOKA VISA", Rudarsko-geološko-naftni zbornik, vol.16, no. 1, pp. 47-58, 2004. [Online]. Available: https://hrcak.srce.hr/13360. [Accessed: 17 October 2019]

Abstracts
An approach to the hydrogeological investigations on Adriatic islands is presented on the Island of Vis case study. Infiltration, accumulation and discharge of the groundwater occur in karstified rock mass. Hydrogeological relations are mostly a consequence of the geological setting, because of the complete hydrogeologic barrier in Komiža bay, and relative barrier in the area of karst poljes. Significant research was performed in the 1999 – 2000 period aimed of better understanding of hydrogeological relations. These investigations, as well as reinterpretation of some previously known data, included structural geology, hydrogeology, hydrology and hydrochemistry. Approximate rock mass hydraulic conductivity calculation is also shown, as well as level of its usability in such terrain. Based on all these methods, it is possible to conclude that on the Island of Vis there is no saline water present underneath the entire island. There is only a saline water wedge which is formed on the top of relatively impermeable base rock, some few tens of meters under recent sea level. With such a model, and taking in account the hydrological balance, it is possible to conclude that there is possibility of higher amount of groundwater exploitation then it is today.

Keywords
Vis island, karst; rock mass; hydraulic conductivity; salt/fresh water relations

Hrčak ID: 13360

URI
https://hrcak.srce.hr/13360

[croatian]

Visits: 2.658 *