Abstract
Rainfall water plays the basic role in mass movements activation in Polish Carpathians. Its infiltration has impact on seepage processes and changes of pore water pressures and thus affect the strength parameters of soils inside the slopes. Investigated colluviums built from flysch layers of weathered claystones and sandstones were difficult for in situ and laboratory tests. High quality core drillings, sampling, geophysical investigations, laboratory tests and instrumentation provided data for slope stability analysis. Monitoring played a special role in the project. Recognition of weather and groundwater conditions influence on movement’s activation was realized using inclinometer, piezometer, pore pressure and meteorological monitoring instrumentation. In 2010 new automatic, on-line early warning system was installed at Szymbark landslide near the city of Gorlice. Measurements in standard system allowed observation of landslide behavior after intensive precipitations in Polish Carpathians in June 2006 and May-June 2010. Measurements in on-line system started during intensive rainfalls and flood in June 2010. The results confirm the relationship between rainfalls, changes of pore pressure values and displacements activation. The highest rainfalls were followed by intense increase and decrease of pore pressures. The movements usually occurred after precipitations of 200–250 mm, lasted one or a few days depending on the initial saturation conditions. These processes caused reactivation of existing landslides or forming a new ones. Research proved that monitoring of rainfalls, pore pressures and displacements could help in recognition of movement activation triggers for selected landslides. It may be also useful in landslide prediction, remediation works and early warning.
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References
Bednarczyk Z (2012) Geotechnical modeling and monitoring as a basis for stabilization works at two landslide areas in Polish Carpathians. Proceedings of 11th international and 2nd North American symposium on Landslides. The Canadian Geotechnical Society Canada. Taylor & Francis, pp 1419–1425
Bochenek W (2012) Evaluation of precipitation at IG&SO PAS research station in Szymbark during 40-year period (1970–2010) ITP.T.12 z.2 pp 29–44
Gil E, Gilot E, Kotarba A (1974) An early Holocene landslide in the Niski Beskid and its significance for paleogeografical reconstructions. Studia Geom Carpatho-Balc, VIII
Gil E, Dlugosz M (2006) Threshold values of rainfalls triggering selected deep-seated landslides in Polish Carpathians. Studia Geom Carp-Balc 40:21–43
Raczkowski W, Mrozek T (2002) Activating of landsliding in the Polish Flysch Carpathians by the end of 20th century. Studia Geom Carp-Bal 36:91–111
Sawicki L (1917) Landslides and mass movements in Szymbark, western Galicia. Monograph of Department of Natural Science and Mathematic AU, vol 13, pp 3
Starkel L (2011) Temporal and spatial complexity of extreme rainfalls. Land Anal 15:65–80
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© 2015 Springer International Publishing Switzerland
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Bednarczyk, Z. (2015). Monitoring of Rainfall Induced Landslides in Relation to Weather Conditions at Selected Locations in Polish Carpathians. In: Lollino, G., et al. Engineering Geology for Society and Territory - Volume 2. Springer, Cham. https://doi.org/10.1007/978-3-319-09057-3_207
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DOI: https://doi.org/10.1007/978-3-319-09057-3_207
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