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Insights into the landslide processes by hydrogeochemical and isotopic characterization : The case study of the Slano blato landslide (SW Slovenia)
ID
Debevec Jordanova, Galena
(
Author
),
ID
Kanduč, Tjaša
(
Author
),
ID
Vreča, Polona
(
Author
),
ID
Verbovšek, Timotej
(
Author
)
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MD5: D26C99C7A5666BFDB73D5A1B8E79F43F
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https://www.mdpi.com/2073-4441/18/3/318
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Abstract
This study evaluates the role of groundwater in the dynamics of the Slano blato landslide using hydrogeochemical and stable isotope data. Results show that deep groundwater inflow significantly affected the landslide behavior, as demonstrated by pronounced hydrogeochemical and isotopic differences among springs. Springs within the landslide differ markedly from those in similar geological settings of the Vipava Valley, indicating a distinct local groundwater system. Groundwater is present within the landslide body even during dry periods. Waters originate mainly from a higher karstic recharge area and flow through deep flysch strata, particularly fractured sandstones, where they become enriched in dissolved ions, especially K+ and SO42−, and show increased mineralization in the lower parts of the landslide. Saturation indices indicate slight oversaturation with calcite and dolomite and equilibrium with quartz for most samples, reflecting interaction with carbonates and flysch sandstones. Elevated sulphate concentrations and near-equilibrium conditions for mirabilite and thenardite suggest salt-related deterioration of landslide material, enhanced by evaporation. Stable isotope data (δ13CDIC, δ18O, δ2H) indicate dominant carbonate recharge, meteoric origin, evaporation effects, and long-term waterrock interaction. This study highlights the need for additional isotope tracers, groundwater age indicators, seasonal monitoring, and on-site meteorological measurements to improve interpretation.
Language:
English
Keywords:
earth flow
,
mud flow
,
groundwater
,
stable isotopes
,
hydrogeochemistry
,
slope mass movements
Work type:
Article
Typology:
1.01 - Original Scientific Article
Organization:
NTF - Faculty of Natural Sciences and Engineering
Publication status:
Published
Publication version:
Author Accepted Manuscript
Publication date:
27.01.2026
Year:
2026
Number of pages:
Str. 1-24
Numbering:
Vol. 18, iss. 3
PID:
20.500.12556/RUL-178709
UDC:
55
ISSN on article:
2073-4441
DOI:
10.3390/w18030318
COBISS.SI-ID:
266581763
Publication date in RUL:
17.02.2026
Views:
216
Downloads:
125
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Record is a part of a journal
Title:
Water
Shortened title:
Water
Publisher:
MDPI
ISSN:
2073-4441
COBISS.SI-ID:
36731653
Licences
License:
CC BY-NC 4.0, Creative Commons Attribution-NonCommercial 4.0 International
Link:
http://creativecommons.org/licenses/by-nc/4.0/
Description:
A creative commons license that bans commercial use, but the users don’t have to license their derivative works on the same terms.
Projects
Funder:
ARIS - Slovenian Research and Innovation Agency
Project number:
P1-0195-2018
Name:
Geookolje in geomateriali
Funder:
ARIS - Slovenian Research and Innovation Agency
Project number:
Young Researcher program
Name:
Young Researcher program
Funder:
ARIS - Slovenian Research and Innovation Agency
Project number:
P1-0143-2020
Name:
Kroženje snovi v okolju, snovna bilanca in modeliranje okoljskih procesov ter ocena tveganja
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