Mass-Movement Causes and Landslide Susceptibility in River Valleys of Lowland Areas: A Case Study in the Central Radunia Valley, Northern Poland

This work aims to analyse the mechanisms and factors contributing to shallow soil landslides in river valleys entrenched in lowlands on the example of the Central Radunia Valley. The combination of susceptibility analysis using geographic-information-system-based statistical models, field surveys, a...

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Main Authors: Anna Małka, Lesław Zabuski, Frieder Enzmann, Arkadiusz Krawiec
Format: Article
Language:English
Published: MDPI AG 2023-09-01
Series:Geosciences
Subjects:
Online Access:https://www.mdpi.com/2076-3263/13/9/277
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author Anna Małka
Lesław Zabuski
Frieder Enzmann
Arkadiusz Krawiec
author_facet Anna Małka
Lesław Zabuski
Frieder Enzmann
Arkadiusz Krawiec
author_sort Anna Małka
collection DOAJ
description This work aims to analyse the mechanisms and factors contributing to shallow soil landslides in river valleys entrenched in lowlands on the example of the Central Radunia Valley. The combination of susceptibility analysis using geographic-information-system-based statistical models, field surveys, analysis of archival materials, and numerical modelling for the analysis of slope stability and hydrogeological processes allows for comprehensive landslide reconstruction, mass movement mechanism description, and an explanation of the role of triggering and causal factors. The results emphasise the need for cross-disciplinary studies of shallow soil landslides. The identification and prioritisation of the causal factors indicate that geomorphological conditions play a particularly important role. The current study shows that the greatest influence on landslide formation in the Central Radunia Valley is slope angle, as determined using a high-resolution digital elevation model. The slope angle factor is sufficient to produce a reliable susceptibility map (the areas under the curve of the success rate and prediction rate curves are 87.84% and 85.34%, respectively). However, numerical modelling of slope failure also clearly indicated that there was a significant influence of anthropogenic impacts on the landslide process. We determined that the main triggering factor causing the January 2019 Rutki landslide was related to the drilling of a borehole on 10 January 2019. The water used for drilling hydrated the soil and thus weakened the stability conditions.
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spelling doaj.art-732738e9aac64250a9efeb33bea33dd42023-11-19T10:54:55ZengMDPI AGGeosciences2076-32632023-09-0113927710.3390/geosciences13090277Mass-Movement Causes and Landslide Susceptibility in River Valleys of Lowland Areas: A Case Study in the Central Radunia Valley, Northern PolandAnna Małka0Lesław Zabuski1Frieder Enzmann2Arkadiusz Krawiec3Branch of Marine Geology, Polish Geological Institute—National Research Institute, 5 Kościerska Street, 80-328 Gdansk, PolandInstitute of Hydro-Engineering, Polish Academy of Sciences, 7 Kościerska Street, 80-328 Gdansk, PolandInstitute of Geosciences, Johannes Gutenberg-University Mainz, Johann-Joachim-Becher-Weg 21, D-55128 Mainz, GermanyFaculty of Earth Sciences and Spatial Management, Nicolaus Copernicus University, Lwowska 1, 87-100 Torun, PolandThis work aims to analyse the mechanisms and factors contributing to shallow soil landslides in river valleys entrenched in lowlands on the example of the Central Radunia Valley. The combination of susceptibility analysis using geographic-information-system-based statistical models, field surveys, analysis of archival materials, and numerical modelling for the analysis of slope stability and hydrogeological processes allows for comprehensive landslide reconstruction, mass movement mechanism description, and an explanation of the role of triggering and causal factors. The results emphasise the need for cross-disciplinary studies of shallow soil landslides. The identification and prioritisation of the causal factors indicate that geomorphological conditions play a particularly important role. The current study shows that the greatest influence on landslide formation in the Central Radunia Valley is slope angle, as determined using a high-resolution digital elevation model. The slope angle factor is sufficient to produce a reliable susceptibility map (the areas under the curve of the success rate and prediction rate curves are 87.84% and 85.34%, respectively). However, numerical modelling of slope failure also clearly indicated that there was a significant influence of anthropogenic impacts on the landslide process. We determined that the main triggering factor causing the January 2019 Rutki landslide was related to the drilling of a borehole on 10 January 2019. The water used for drilling hydrated the soil and thus weakened the stability conditions.https://www.mdpi.com/2076-3263/13/9/277mass movementsnumerical modelling of landslideslandslide susceptibilityslope hydrologylowland areasRadunia Valley
spellingShingle Anna Małka
Lesław Zabuski
Frieder Enzmann
Arkadiusz Krawiec
Mass-Movement Causes and Landslide Susceptibility in River Valleys of Lowland Areas: A Case Study in the Central Radunia Valley, Northern Poland
Geosciences
mass movements
numerical modelling of landslides
landslide susceptibility
slope hydrology
lowland areas
Radunia Valley
title Mass-Movement Causes and Landslide Susceptibility in River Valleys of Lowland Areas: A Case Study in the Central Radunia Valley, Northern Poland
title_full Mass-Movement Causes and Landslide Susceptibility in River Valleys of Lowland Areas: A Case Study in the Central Radunia Valley, Northern Poland
title_fullStr Mass-Movement Causes and Landslide Susceptibility in River Valleys of Lowland Areas: A Case Study in the Central Radunia Valley, Northern Poland
title_full_unstemmed Mass-Movement Causes and Landslide Susceptibility in River Valleys of Lowland Areas: A Case Study in the Central Radunia Valley, Northern Poland
title_short Mass-Movement Causes and Landslide Susceptibility in River Valleys of Lowland Areas: A Case Study in the Central Radunia Valley, Northern Poland
title_sort mass movement causes and landslide susceptibility in river valleys of lowland areas a case study in the central radunia valley northern poland
topic mass movements
numerical modelling of landslides
landslide susceptibility
slope hydrology
lowland areas
Radunia Valley
url https://www.mdpi.com/2076-3263/13/9/277
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