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Hydrogeological analysis of topography-driven groundwater flow in a low temperature geothermal aquifer system in the Julian Alps, Slovenia
ID
Serianz, Luka
(
Author
),
ID
Markelj, Anže
(
Author
),
ID
Rman, Nina
(
Author
),
ID
Brenčič, Mihael
(
Author
),
ID
Mádl-Szőnyi, Judit
(
Author
)
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MD5: 8935A2BC9920740EE2E65D3BD61B36EA
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https://link.springer.com/article/10.1007/s10040-024-02866-z
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Abstract
Groundwater flow and heat distribution was investigated in the regional karstic-fissured aquifer-aquitard system near Lake Bled in the Slovenian, eastern Julian Alps. The area features thermal springs with temperatures of 19–23 °C which are exploited by abstraction wells. The occurrence of low-temperature geothermal systems, which are common in the Alps, are associated with specific hydrogeological conditions, such as vertical hydraulic connectivity between different geological formations, relatively large elevation differences along flow paths, and the concentrated upwelling of geothermal water to the surface. The occurrence of the low-temperature geothermal field is explained by the presence of a hydraulically conductive fault along with a regional groundwater flow pattern that supports deep groundwater circulation. Hydraulic measurements and temperature data were collected from springs and wells in the area to support the analysis of flow patterns, together with the construction of a basin-scale 2D numerical flow and heat transport simulation. The diverse topographic and geological conditions result in a multi-scale groundwater flow system. The discharge of thermal waters in the Lake Bled area is a consequence of the upwelling of deep groundwater induced by a combination of the ~650 m difference in hydraulic head and hydrogeological heterogeneity and anisotropy, related to faulting of the geological formations. In addition, individual flow subsystems were found to significantly affect the natural heat distribution and travel times within the basin-scale system. The study highlights the combination of a basin scale approach taking into consideration local to regional-scale heterogeneities and faults in order to better understand the hydrogeological behaviour of Alpine groundwater systems.
Language:
English
Keywords:
basin-scale groundwater flow
,
thermal conditions
,
carbonate rocks
,
groundwater recharge
,
Slovenia
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:
2025
Number of pages:
Str. 237–256
Numbering:
Vol. 33, iss. 1
PID:
20.500.12556/RUL-167350
UDC:
556.3
ISSN on article:
1431-2174
DOI:
10.1007/s10040-024-02866-z
COBISS.SI-ID:
226023171
Publication date in RUL:
17.02.2025
Views:
442
Downloads:
94
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Record is a part of a journal
Title:
Hydrogeology journal
Shortened title:
Hydrogeol. j.
Publisher:
Springer Nature, International Association of Hydrogeologists
ISSN:
1431-2174
COBISS.SI-ID:
316757
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.
Secondary language
Language:
Slovenian
Keywords:
podzemna voda
,
termalna voda
,
vodonosnik
,
tok podzemne vode
,
karbonatne kamnine
,
napajanje
Projects
Funder:
ARIS - Slovenian Research and Innovation Agency
Project number:
P1-0020
Name:
Podzemne vode in geokemija
Funder:
ARIS - Slovenian Research and Innovation Agency
Funding programme:
Young researchers
Project number:
1000-19-0215
Funder:
Other - Other funder or multiple funders
Funding programme:
Tempus Public Foundation, Bilateral State Scholarship
Funder:
Other - Other funder or multiple funders
Funding programme:
National Multidisciplinary Laboratory for Climate Change
Project number:
RRF-2.3.1-21-2022-00014
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