Application of Combined Geophysical Methods for the Examination of a Water Dam Subsoil

The paper presents the results of geophysical measurements that were carried out in the vicinity of the water dam/water reservoir supplying the city of Bielsko-Biala with drinking water. The measurements were performed in order to non-invasively detect faults, fractured zones and areas filled with b...

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Autores principales: Tomisław Gołębiowski, Bogdan Piwakowski, Michał Ćwiklik, Antoni Bojarski
Formato: article
Lenguaje:EN
Publicado: MDPI AG 2021
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Acceso en línea:https://doaj.org/article/9fcdfcbaee54494a97fe9e2ea7cb7053
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spelling oai:doaj.org-article:9fcdfcbaee54494a97fe9e2ea7cb70532021-11-11T19:53:26ZApplication of Combined Geophysical Methods for the Examination of a Water Dam Subsoil10.3390/w132129812073-4441https://doaj.org/article/9fcdfcbaee54494a97fe9e2ea7cb70532021-10-01T00:00:00Zhttps://www.mdpi.com/2073-4441/13/21/2981https://doaj.org/toc/2073-4441The paper presents the results of geophysical measurements that were carried out in the vicinity of the water dam/water reservoir supplying the city of Bielsko-Biala with drinking water. The measurements were performed in order to non-invasively detect faults, fractured zones and areas filled with breccia, which may be, at the same time, a preferential path of groundwater flow. The aforementioned factors influence the stability of the dam. The general identification of the examined media was realized by the electrical resistivity tomography method. The ERT surveys were supplemented by capacitively-coupled resistivity. The electrical methods allowed them to recognize geological settings, indicate possible fault locations, and point out the fault plane as a path of water flow. The ground penetrating radar method detected fractured and filled water areas and underground water paths in the dam’s forefield as a result of the method’s very high resolution. The high resolution seismic reflection method provided a clear and high resolution image of the relatively deep geological structure and verified a location and the run of the faults. In general, the complex geophysical-geological interpretation enabled classification of the unconsolidated/fractured zones associated with faults as a place where the erosion process is the most intense and can bring danger on the dam. Finally, it was confirmed that the area should be the subject of geophysical monitoring.Tomisław GołębiowskiBogdan PiwakowskiMichał ĆwiklikAntoni BojarskiMDPI AGarticlewater damhydrotechnical constructiongeophysical methodswater flowHydraulic engineeringTC1-978Water supply for domestic and industrial purposesTD201-500ENWater, Vol 13, Iss 2981, p 2981 (2021)
institution DOAJ
collection DOAJ
language EN
topic water dam
hydrotechnical construction
geophysical methods
water flow
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
spellingShingle water dam
hydrotechnical construction
geophysical methods
water flow
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
Tomisław Gołębiowski
Bogdan Piwakowski
Michał Ćwiklik
Antoni Bojarski
Application of Combined Geophysical Methods for the Examination of a Water Dam Subsoil
description The paper presents the results of geophysical measurements that were carried out in the vicinity of the water dam/water reservoir supplying the city of Bielsko-Biala with drinking water. The measurements were performed in order to non-invasively detect faults, fractured zones and areas filled with breccia, which may be, at the same time, a preferential path of groundwater flow. The aforementioned factors influence the stability of the dam. The general identification of the examined media was realized by the electrical resistivity tomography method. The ERT surveys were supplemented by capacitively-coupled resistivity. The electrical methods allowed them to recognize geological settings, indicate possible fault locations, and point out the fault plane as a path of water flow. The ground penetrating radar method detected fractured and filled water areas and underground water paths in the dam’s forefield as a result of the method’s very high resolution. The high resolution seismic reflection method provided a clear and high resolution image of the relatively deep geological structure and verified a location and the run of the faults. In general, the complex geophysical-geological interpretation enabled classification of the unconsolidated/fractured zones associated with faults as a place where the erosion process is the most intense and can bring danger on the dam. Finally, it was confirmed that the area should be the subject of geophysical monitoring.
format article
author Tomisław Gołębiowski
Bogdan Piwakowski
Michał Ćwiklik
Antoni Bojarski
author_facet Tomisław Gołębiowski
Bogdan Piwakowski
Michał Ćwiklik
Antoni Bojarski
author_sort Tomisław Gołębiowski
title Application of Combined Geophysical Methods for the Examination of a Water Dam Subsoil
title_short Application of Combined Geophysical Methods for the Examination of a Water Dam Subsoil
title_full Application of Combined Geophysical Methods for the Examination of a Water Dam Subsoil
title_fullStr Application of Combined Geophysical Methods for the Examination of a Water Dam Subsoil
title_full_unstemmed Application of Combined Geophysical Methods for the Examination of a Water Dam Subsoil
title_sort application of combined geophysical methods for the examination of a water dam subsoil
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/9fcdfcbaee54494a97fe9e2ea7cb7053
work_keys_str_mv AT tomisławgołebiowski applicationofcombinedgeophysicalmethodsfortheexaminationofawaterdamsubsoil
AT bogdanpiwakowski applicationofcombinedgeophysicalmethodsfortheexaminationofawaterdamsubsoil
AT michałcwiklik applicationofcombinedgeophysicalmethodsfortheexaminationofawaterdamsubsoil
AT antonibojarski applicationofcombinedgeophysicalmethodsfortheexaminationofawaterdamsubsoil
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