Ground Subsidence in the City of Tuzla (Bosnia & Herzegovina)
Keywords:
Salt deposit exploitation, Ground collapsing, Topographic survey, Satellite, GPSAbstract
Since the year 1955, when the salt deposits exploitation activities were carried out in the city of Tuzla and surroundings, dramatic ground collapsing phenomena occurred. Up to 10 meters of sinking in the last half century produced several damages with regards to buildings and infrastructures, leading to the demolition of the most compromised part of the city by the inhabitants. Traditional topographic survey was used in order to monitor the land deformations from the 50' till presentwith the establishment of a dense topographic network around the sinking area. The analisys of the huge dataset of altimetric data, the correlation with the boreholes activities and the introduction of more productive modern technologies (satellite technologies, GPS for geodesy) for repeated land monitoring are the object of this paper.
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References
Čeliković, R., & Imamović, E. (2016). Continuous GNSS movement monitoring in the zone of influence of Tuzla salt deposit. Int Symp Eng Geodesy, 2016, 489-498.
Čeliković, R., Imamović, E., Salihović, R., & Sušić, A. (2014). Prostorno vremenska analiza vertikalnih pomjeranja terena u Tuzli za period 2008–2012. Proceedings of GEO-EXPO, 38-44.
Cicic, S. (2002). Geological composition and tectonic terrain of Bosnia and Herzegovina. Geological guidebook through Bosnia and Herzegovina. Sarajevo-Geological Survey of Federation Bosnia and Herzegovina, Ustanicka, Sarajevo.
Ferhatbegović, Z. (2004). Geological features of the central part of the Tuzla basin. Doctoral dissertation. Faculty of Mining and Geology and Civil Engineering, University of Tuzla.
Hrvatović, H. (2006). Geological guidebook through Bosnia and Herzegovina. Geological Survey of Federation Bosnia and Herzegovina, Sarajevo.
Ibreljić, I., Kudumović, F., & Ahmetbegović, S. (2007). Economy and ecology of natural resources in Tuzla area (Bosnia and Herzegovina) in the past and future projections. In Proceedings of the Joint Congress of the European Regional Science Association and ASRDLF, 1-7.
Katzer, F. (1903). Geological guide through Bosnia and Herzegovina, Sarajevo. Geological Guidebook through Bosnia and Herzegovina. Sarajevo-Geological Survey of Federation Bosnia and Herzegovina, Ustanicka, Sarajevo.
Mancini, F., Stecchi, F., & Gabbianelli, G. (2009). GIS-based assessment of risk due to salt mining activities at Tuzla (Bosnia and Herzegovina). Engineering Geology, 109(3-4), 170-182.
Soklić, I. (1959). Miocene Paleogeography and origin of salt deposits in Tuzla. Geological Guidebook through Bosnia and Herzegovina. Sarajevo-Geological Survey of Federation Bosnia and Herzegovina, Ustanicka, Sarajevo.
Soklić, I. (1964). Origin and structures of the Tuzla basin. Geoloski glasnik. Geological Guidebook through Bosnia and Herzegovina. Sarajevo-Geological Survey of Federation Bosnia and Herzegovina, Ustanicka, Sarajevo.
Stecchi, F., Antonellini, M., & Gabbianelli, G. (2009). Curvature analysis as a tool for subsidence-related risk zones identification in the city of Tuzla (BiH). Geomorphology, 107(3-4), 316-325.
Stevanović, P. (1977). Geology of the Bosnia and Herzegovina, Book 3 - Cenozoic periods. Geological Guidebook through Bosnia and Herzegovina, Sarajevo-Geological Survey of Federation Bosnia and Herzegovina, Ustanicka, Sarajevo.
Tari, V., & Pamić, J. (1998). Geodynamic evolution of the northern Dinarides and the southern part of the Pannonian Basin. Tectonophysics, 297(1-4), 269-281.
Vrabac, S. (1999). Facial and biostratigraphic characteristics of Badenian and Sarmatian in North Bosnia (in Bosnian), Tuzla. Geological Guidebook through Bosnia and Herzegovina. Sarajevo-Geological Survey of Federation Bosnia and Herzegovina, Ustanicka, Sarajevo.