izpis_h1_title_alt

Hydrogeochemical characterization of a warm spring system in a carbonate mountain range of the Eastern Julian Alps, Slovenia
ID Serianz, Luka (Author), ID Rman, Nina (Author), ID Brenčič, Mihael (Author)

.pdfPDF - Presentation file, Download (4,57 MB)
MD5: 6D2D5032FCABC07060677AAF01FF0B9A
URLURL - Source URL, Visit https://www.mdpi.com/2073-4441/12/5/1427 This link opens in a new window

Abstract
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.

Language:English
Keywords:thermal spring, groundwater, hydrogeochemical characteristics, stable isotopes, Julian Alps
Work type:Article
Typology:1.01 - Original Scientific Article
Organization:NTF - Faculty of Natural Sciences and Engineering
Publication status:Published
Publication version:Version of Record
Year:2020
Number of pages:20 str.
Numbering:Vol. 12, iss. 5, art. 1427
PID:20.500.12556/RUL-133709 This link opens in a new window
UDC:556.3
ISSN on article:2073-4441
DOI:10.3390/w12051427 This link opens in a new window
COBISS.SI-ID:15693059 This link opens in a new window
Publication date in RUL:10.12.2021
Views:564
Downloads:111
Metadata:XML RDF-CHPDL DC-XML DC-RDF
:
Copy citation
Share:Bookmark and Share

Record is a part of a journal

Title:Water
Shortened title:Water
Publisher:Molecular Diversity Preservation International - MDPI
ISSN:2073-4441
COBISS.SI-ID:36731653 This link opens in a new window

Licences

License:CC BY 4.0, Creative Commons Attribution 4.0 International
Link:http://creativecommons.org/licenses/by/4.0/
Description:This is the standard Creative Commons license that gives others maximum freedom to do what they want with the work as long as they credit the author.
Licensing start date:17.05.2020

Secondary language

Language:Slovenian
Keywords:hidrogeokemija, termalna voda, izotopi, Julijske Alpe

Projects

Funder:ARRS - Slovenian Research Agency
Funding programme:Young researchers
Project number:1000-19-0215

Funder:ARRS - Slovenian Research Agency
Project number:P1-0020
Name:Podzemne vode in geokemija

Similar documents

Similar works from RUL:
Similar works from other Slovenian collections:

Back