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SBAS DInSAR and in situ monitoring of the Šumljak landslide (SW Slovenia) dynamics driven by rainfall and piezometric-level fluctuation
ID
Debevec Jordanova, Galena
(
Author
),
ID
Popović, Zdenka
(
Author
),
ID
Yastika, Putu Edi
(
Author
),
ID
Shimizu, Norikazu
(
Author
),
ID
Oštir, Krištof
(
Author
),
ID
Verbovšek, Timotej
(
Author
)
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https://link.springer.com/article/10.1007/s10346-024-02408-4
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Abstract
This paper presents the first attempt at establishing the dynamics of the Šumljak debris slide by using a multidisciplinary approach, including long-term inclinometer and piezometer measurements and a time-series analysis of SAR images for displacement vector estimation. The Šumljak landslide is located in the Rebrnice area, SW Slovenia, where the regional highway Razdrto-Nova Gorica runs through and poses a threat to the highway viaduct’s stability. By combining both ascending and descending Sentinel-1 data, we have estimated $_3$D displacement vectors for the landslide, providing insights into the usability of the technique for this kind of slow-moving landslides. Furthermore, we have combined and compared the SBAS DInSAR results to the displacements measured by inclinometer to evaluate the rate of displacement of the landslide and the viaduct. The inclinometer measurement results show that the landslide has a single sliding plane between the flysch colluvium and the slope deposits and provide the proof of the enlargement of the sliding area above its main scarp. The displacement vectors are spatially heterogenous, suggesting that different sites have different velocities and slightly different directional vectors. These results partly comply with the InSAR results. We further discussed the estimated vectors of displacement and the possible mechanism of movements. By using the piezometric data, we studied the groundwater level fluctuation in relation to daily rainfall and its influence on the displacements. Our findings show a correlation between the movements and the wet/dry season, indicating that the landslide is driven by rainfall and consequently groundwater level fluctuation. In 2020, the groundwater level rise was smaller than in the years before due to less rainfall, resulting in lower velocity of the landslide (5.5 mm/year) than in 2019 (7 mm/year).
Language:
English
Keywords:
debris slide
,
inclinometer
,
piezometer
,
displacement vector estimation
,
time-series analysis
,
SBAS DInSAR
Work type:
Article
Typology:
1.01 - Original Scientific Article
Organization:
NTF - Faculty of Natural Sciences and Engineering
FGG - Faculty of Civil and Geodetic Engineering
Publication status:
Published
Publication version:
Version of Record
Year:
2025
Number of pages:
Str. 1397-1411
Numbering:
Vol. 22, iss. 5
PID:
20.500.12556/RUL-169230
UDC:
55
ISSN on article:
1612-510X
DOI:
10.1007/s10346-024-02408-4
COBISS.SI-ID:
236335875
Publication date in RUL:
20.05.2025
Views:
345
Downloads:
146
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Record is a part of a journal
Title:
Landslides : Journal of the international consortium on landslides
Publisher:
Springer
ISSN:
1612-510X
COBISS.SI-ID:
2274913
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.
Projects
Funder:
ARIS - Slovenian Research and Innovation Agency
Funding programme:
Young researchers
Funder:
ARIS - Slovenian Research and Innovation Agency
Project number:
P1-0195
Name:
Geookolje in geomateriali
Funder:
ARIS - Slovenian Research and Innovation Agency
Project number:
P2-0406
Name:
Opazovanje Zemlje in geoinformatika
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