Shallow movements in clay rich rocks detected during subnormal precipitation period

0511803 - ÚSMH 2020 RIV CZ eng J - Článek v odborném periodiku
Balek, Jan - Klimeš, Jan - Blahůt, Jan - Štroner, M. - Urban, R. - Hartvich, Filip
Shallow movements in clay rich rocks detected during subnormal precipitation period.
Acta geodynamica et geomaterialia. Roč. 16, č. 4 (2019), s. 409-417. ISSN 1214-9705. E-ISSN 2336-4351
Grant CEP: GA MŠMT(CZ) LM2015079; GA MŠMT(CZ) LM2015084
Institucionální podpora: RVO:67985891
Klíčová slova: Landslide * SAA sensor * MEMS * Monitoring * Displacements * Precipitation * Temperature
Obor OECD: Geology
Impakt faktor: 1.227, rok: 2019
Způsob publikování: Open access
https://www.irsm.cas.cz/materialy/acta_content/2019_doi/Balek_AGG_2019_0034.pdf

The paper aims at the evaluation of the landslide movement monitoring near Třebenice town in the České středohoří hilly land, Czechia. The monitored period between May of 2017 and January 2019 is characterized by negative effective precipitations and continually decreasing ground water levels in conditions of Cretaceous sedimentary rocks of different permeability. In the spring of 2017, the SAA (ShapeAccelArray) sensor was installed into the borehole placed one the most active part of the landslide area. Sensor was stabilized in 16 m depth, 2.5 m under the deepest sliding plane. SAA sensor automatically registers absolute values of displacements in different layers. The results indicate a slow movement above the shallower (4 m deep) sliding plane, with velocities changing significantly based on annual period from 3 mm/month during spring to 0 mm during late summer and autumn months. Measured displacements were confronted with course of GWLs, temperature and potential effective precipitation, to discover causes of the reversible movement.
Trvalý link: http://hdl.handle.net/11104/0302051