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Hydrogeochemical characterization of a warm spring system in a carbonate mountain range of the Eastern Julian Alps, Slovenia
ID
Serianz, Luka
(
Avtor
),
ID
Rman, Nina
(
Avtor
),
ID
Brenčič, Mihael
(
Avtor
)
PDF - Predstavitvena datoteka,
prenos
(4,57 MB)
MD5: 6D2D5032FCABC07060677AAF01FF0B9A
URL - Izvorni URL, za dostop obiščite
https://www.mdpi.com/2073-4441/12/5/1427
Galerija slik
Izvleček
The Alps represent an area where many deep groundwater circulations occur as thermal springs. In the Bled case study, the thermal water temperature, at it is discharged to the surface, is between 19–23 °C. In order to determine the extent (e.g., geometry) and the origin of the pronounced deep circulation system in the Bled area, chemical and isotopic measurements of waters from different hydrogeological systems were performed (e.g., surface water, thermal water, fresh groundwater). Hydrogeochemical methods were used to tie together the above-mentioned parameters. The results have shown that thermal outflow in Bled is determined by the presence of a deep-water circulation system, where the dissolution of carbonates minerals is the main hydrogeochemical process affecting chemical components of natural water flow. The correlation of the major ions suggests that the recharge area is represented by both limestone and dolomite rocks. Moreover, the results of δ$^{18}$O and δ$^2$H of all samples indicate that the recharge is mainly meteoric precipitation. The recharge altitude was estimated for two sampled fresh groundwater springs. The isotopic compositions of those two springs suggest the range from δ$^{18}$O = −8.68‰, δ$^2$H = −57.4‰ at an elevation of 629 m to δ$^{18}$O = −9.30‰, δ$^2$H = −60.1‰ at an elevation of 1216 m. The isotopic analysis has confirmed that the thermal water recharges from altitudes of 1282–1620 m a.s.l.
Jezik:
Angleški jezik
Ključne besede:
thermal spring
,
groundwater
,
hydrogeochemical characteristics
,
stable isotopes
,
Julian Alps
Vrsta gradiva:
Članek v reviji
Tipologija:
1.01 - Izvirni znanstveni članek
Organizacija:
NTF - Naravoslovnotehniška fakulteta
Status publikacije:
Objavljeno
Različica publikacije:
Objavljena publikacija
Leto izida:
2020
Št. strani:
20 str.
Številčenje:
Vol. 12, iss. 5, art. 1427
PID:
20.500.12556/RUL-133709
UDK:
556.3
ISSN pri članku:
2073-4441
DOI:
10.3390/w12051427
COBISS.SI-ID:
15693059
Datum objave v RUL:
10.12.2021
Število ogledov:
1008
Število prenosov:
141
Metapodatki:
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Objavi na:
Gradivo je del revije
Naslov:
Water
Skrajšan naslov:
Water
Založnik:
Molecular Diversity Preservation International - MDPI
ISSN:
2073-4441
COBISS.SI-ID:
36731653
Licence
Licenca:
CC BY 4.0, Creative Commons Priznanje avtorstva 4.0 Mednarodna
Povezava:
http://creativecommons.org/licenses/by/4.0/deed.sl
Opis:
To je standardna licenca Creative Commons, ki daje uporabnikom največ možnosti za nadaljnjo uporabo dela, pri čemer morajo navesti avtorja.
Začetek licenciranja:
17.05.2020
Sekundarni jezik
Jezik:
Slovenski jezik
Ključne besede:
hidrogeokemija
,
termalna voda
,
izotopi
,
Julijske Alpe
Projekti
Financer:
ARRS - Agencija za raziskovalno dejavnost Republike Slovenije
Program financ.:
Young researchers
Številka projekta:
1000-19-0215
Financer:
ARRS - Agencija za raziskovalno dejavnost Republike Slovenije
Številka projekta:
P1-0020
Naslov:
Podzemne vode in geokemija
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