Pregled bibliografske jedinice broj: 1180178
Identification of Groundwater Level Decline since the Seventies of the Twentieth Century - Case study of the Zagreb and Samobor-Zaprešić Aquifers, Croatia
Identification of Groundwater Level Decline since the Seventies of the Twentieth Century - Case study of the Zagreb and Samobor-Zaprešić Aquifers, Croatia // 44th Annual Congress of the International Association of Hydrogeologists (IAH) "Groundwater Heritage and Sustainability" - book of abstracts / Posavec, Kristijan ; Marković, Tamara (ur.).
Zagreb: International Association of Hydrogeologists, 2017. str. 12-12 (poster, međunarodna recenzija, sažetak, stručni)
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Naslov
Identification of Groundwater Level Decline since the Seventies of the Twentieth Century - Case study of the Zagreb and Samobor-Zaprešić Aquifers, Croatia
Autori
Posavec, Kristijan ; Vujević, Mate ; Kolačević, Renata
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, stručni
Izvornik
44th Annual Congress of the International Association of Hydrogeologists (IAH) "Groundwater Heritage and Sustainability" - book of abstracts
/ Posavec, Kristijan ; Marković, Tamara - Zagreb : International Association of Hydrogeologists, 2017, 12-12
ISBN
978-953-6907-61-8
Skup
44th Annual Congress of the International Association of Hydrogeologists (IAH) "Groundwater Heritage and Sustainability"
Mjesto i datum
Dubrovnik, Hrvatska, 25.09.2017. - 29.09.2017
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
groundwater level ; decline ; trend ; water supply
Sažetak
Historically, groundwater levels of the Zagreb – Velika Gorica and Samobor – Zaprešić aquifers are continuously declining. Figure 1 presents isopach map of ground water level decline, showing that groundwater levels declined up to 5 m on some parts of the aquifers during the last 40 years. Continuous decline of groundwater levels mainly occur due to continuous dominant erosional processes of the Sava riverbed, i.e. the river transports existing riverbed deposits downstream from Zagreb. Due to lack of sediment transport from the upper parts of the river, where it is regulated by hydropowerplants, the river cuts its course into existing gravel deposits. Decrease in the Sava riverbed causes decrease in water levels of the river, and consequently in groundwater levels of Zagreb – Velika Gorica and Samobor-Zaprešić aquifers, since groundwater level, i.e. water table is permanently connected to the Sava river.
Izvorni jezik
Engleski
Znanstvena područja
Rudarstvo, nafta i geološko inženjerstvo
POVEZANOST RADA
Ustanove:
Rudarsko-geološko-naftni fakultet, Zagreb
Profili:
Kristijan Posavec
(autor)