Pregled bibliografske jedinice broj: 1170072
Groundwater Recharge Assessment Using Multi Component Analysis: Case Study at the NW Edge of the Varaždin Alluvial Aquifer, Croatia
Groundwater Recharge Assessment Using Multi Component Analysis: Case Study at the NW Edge of the Varaždin Alluvial Aquifer, Croatia // Water, 14 (2022), 42; 1-14 doi:10.3390/w14010042 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 1170072 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Groundwater Recharge Assessment Using Multi
Component Analysis: Case Study at the NW Edge of
the Varaždin Alluvial Aquifer, Croatia
Autori
Karlović, Igor ; Marković, Tamara ; Vujnović, Tatjana
Izvornik
Water (2073-4441) 14
(2022), 42;
1-14
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
groundwater recharge ; surface water–groundwater interaction ; stable water isotopes ; mixing model ; Varaždin alluvial aquifer
Sažetak
Exploring the interaction between precipitation, surface water, and groundwater has been a key subject of many studies dealing with water quality management. The Varaždin aquifer is an example of an area where high nitrate content in groundwater raised public concern, so it is important to understand the aquifer recharge for proper management and preservation of groundwater quality. The NW part of the Varaždin aquifer has been selected for study area, as precipitation, Drava River, accumulation lake, and groundwater interact in this area. In this study, groundwater and surface water levels, water temperature, water isotopes (2H and 18O), and chloride (Cl−) were monitored in precipitation, surface water, and groundwater during the four-year period to estimate groundwater recharge. Head contour maps were constructed based on the groundwater and surface water levels. The results show that aquifer is recharged from both Drava River and accumulation lake for all hydrological conditions– low, mean, and high groundwater levels. The monitoring results of water temperature, chloride content, and stable water isotopes were used as tracers, i.e. as an input to the mixing model for estimation of the contribution ratio from each recharge source. The calculation of mixing proportions showed that surface water is a key mechanism of groundwater recharge in the study area, with a contribution ratio ranging from 55% to 100% depending on the proximity of the observation well to surface water.
Izvorni jezik
Engleski
Znanstvena područja
Geologija, Rudarstvo, nafta i geološko inženjerstvo
Napomena
Igor Karlović i Tamara Marković su glavni autori
ovog rada.
POVEZANOST RADA
Projekti:
IP-2016-06-5365 - Podrijetlo, ponašanje i modeliranje transporta nitrata u varaždinskom aluvijalnom vodonosniku (TRANITAL) (Marković, Tamara, HRZZ - 2016-06) ( CroRIS)
Ustanove:
Državni hidrometeorološki zavod,
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