Nalazite se na CroRIS probnoj okolini. Ovdje evidentirani podaci neće biti pohranjeni u Informacijskom sustavu znanosti RH. Ako je ovo greška, CroRIS produkcijskoj okolini moguće je pristupi putem poveznice www.croris.hr
izvor podataka: crosbi !

The Effect of the Seawter Intrusion on the Robinzon Coastal Spring (CROSBI ID 135168)

Prilog u časopisu | izvorni znanstveni rad | međunarodna recenzija

Buljan, Renato ; Marković, Tamara ; Peh, Zoran The Effect of the Seawter Intrusion on the Robinzon Coastal Spring // Geologia Croatica, 59 (2006), 2; 137-145-x

Podaci o odgovornosti

Buljan, Renato ; Marković, Tamara ; Peh, Zoran

engleski

The Effect of the Seawter Intrusion on the Robinzon Coastal Spring

The Robinzon Spring, located 70 m from the seacoast, is a freshwater, perennial spring with a yield ranging from the maximum 2 m3 /s to the minimum 0.165 m3 /s. The spring occurs at the contact between per- meable carbonate rocks and impermeable flysch deposits. This con- tact is deeply weathered, eroded and submerged below sea level. Such conditions emphasize the delicate relationship between the fresh- and seawater. The objective of the study was to shed more light on the hydrogeological setting of the spring’ s underground recharge area by means of borehole measurements and preexisting knowledge about the dynamics of the fresh- and seawater acquired from similar cases. The spring’ s underground area is divided into three zones: (i) zone of good water circulation (rockfall material and fractured dolomite), (ii) zone of poor water circulation (massive dolomites), and (iii) zone of ‘ ’ trapped’ ’ water (contact between the dolomite and flysch deposits).

Salt-water/freshwater relationship; Coastal aquifer; Karst; Croatia

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

Podaci o izdanju

59 (2)

2006.

137-145-x

objavljeno

1330-030X

1333-4875

Povezanost rada

Geologija, Rudarstvo, nafta i geološko inženjerstvo