Pregled bibliografske jedinice broj: 806495
Use of hydrochemistry and isotopes for improving the knowledge of groundwater flow in a semiconfined aquifer system of the Eastern Slavonia (Croatia)
Use of hydrochemistry and isotopes for improving the knowledge of groundwater flow in a semiconfined aquifer system of the Eastern Slavonia (Croatia) // Catena (Cremlingen), 142 (2016), 153-165 doi:10.1016/j.catena.2016.03.010 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 806495 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Use of hydrochemistry and isotopes for improving the knowledge of groundwater flow in a semiconfined aquifer system of the Eastern Slavonia (Croatia)
Autori
Brkić, Željka ; Briški, Maja ; Marković, Tamara
Izvornik
Catena (Cremlingen) (0341-8162) 142
(2016);
153-165
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
hydrogeology ; conceptual model ; alluvial aquifer ; environmental isotopes (2H ; 18O ; 3H) ; hydrochemical properties ; Sava River basin
Sažetak
Knowledge of groundwater flow, and accordingly, groundwater residence time is immensely important for the sustainable management of groundwater resources. This requires a good conceptual model of the aquifer system. In this paper, a conceptual model based on the interpretations of hydrogeological and hydrochemical data, as well as measurements of environmental tracers (18O, 2H, 3H) was formulated for a semiconfined aquifer system in Eastern Slavonia in Croatia. The aquifer system is composed of Quaternary gravel and sand and silty-clayey interlayers and is covered with low permeability deposits. Measurements of water levels and environmental tracers in the study area clarified the groundwater flow evolution from the recharge area to the discharge area. The content of stable isotopes confirmed that the groundwater originates from precipitation. The tritium content and geochemical processes (such as cation exchange, silicate weathering) suggested a relatively long residence time of groundwater in the part of the aquifer system that is further from the Sava River. The same is confirmed by the results of calculated particle tracking pathlines.
Izvorni jezik
Engleski
Znanstvena područja
Rudarstvo, nafta i geološko inženjerstvo
POVEZANOST RADA
Projekti:
181-1811096-3165 - Osnovna hidrogeološka karta Republike Hrvatske (Brkić, Željka, MZOS ) ( CroRIS)
Ustanove:
Hrvatski geološki institut
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus
