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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2021
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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) |
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water dam hydrotechnical construction geophysical methods water flow Hydraulic engineering TC1-978 Water supply for domestic and industrial purposes TD201-500 |
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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 |
_version_ |
1718431367109279744 |