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Tytuł artykułu

Application of electrical and electromagnetic methods to study sedimentary covers in high mountain areas

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The results of geophysical studies conducted with selected electrical and electromagnetic methods in the Kondratowa Valley in the Tatra Mountains (the Carpathian Mountains, Poland) are presented in the article. The surveys were performed with the following methods: electrical resistivity tomography (ERT), georadar (GPR) and conductivity meter (CM). The objective of the noninvasive geophysical measurements was to determine the thickness of the Quaternary postglacial sediments that fill the bottom of the valley and to designate the accumulation of boulders deposited on Quaternary sediments. The results of ERT surveys conducted along the axis of the valley allowed to determine the changeability of the thickness of the postglacial sediments and allowed to designate a few areas of occurrence of boulders. The ERT, GPR and CM surveys conducted across the valley allowed to designate with high accuracy the thickness of the accumulation of boulders sliding down the valley bottom from the couloirs surrounding the valley.
Słowa kluczowe
Czasopismo
Rocznik
Strony
743--755
Opis fizyczny
Bibliogr. 21 poz.
Twórcy
  • Department of Geophysics, Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, Cracow, Poland
autor
  • Department of Applied Geology, Faculty of Earth Sciences, Silesian University, Sosnowiec, Poland
  • Division of Geodesy, Geophysics and Engineering Geology, Department of Geotechnics, Faculty of Environmental Engineering, Cracow University of Technology, Cracow, Poland
autor
  • Institute of Innovative Technologies EMAG, Katowice, Poland
autor
  • Geofizyka Kraków SA, Cracow, Poland
  • Department of Applied Geology, Faculty of Earth Sciences, Silesian University, Sosnowiec, Poland
Bibliografia
  • 1. Annan AP (1999) Practical processing of GPR data. Sensor and Software Inc., Mississauga
  • 2. Annan AP (2001) Ground penetrating radar—workshop notes. Sensor and Software Inc., Mississauga
  • 3. Bac-Moszaszwili M, Gąsienica-Szostak M (1992) Polish Tatra Mountains—geological guide for tourists. Geological Ed., Warsaw
  • 4. Carcione JM, Gei D, Botelho MAB, Osella A, de la Vega M (2006) Fresnel reflection coefficients for GPR-AVO analysis and detection of seawater and NAPL contaminants. Near Surf Geophys 4:253–263
  • 5. Dobiński W, Żogała B, Wzientek K, Litwin L (2008) Results of geophysical surveys on Kasprowy Wierch, the Tatra Mountains, Poland. In: Hauck C, Kneisel C (eds) Applied geophysics in periglacial environments. Cambridge University Press, Cambridge, pp 126–136
  • 6. Gądek B, Rączkowska Z, Wziętek K, Żogała B (2006) The long-term permafrost of the Miedziana Valley (the Slovakian Tatra Mountains) on the basis of the results of geophysical and geomorphological research. In: Borowiec W, Kotarba A, Kownacki A, Krzan Z, Mirek Z (eds) Tatra national park—comparison with other mountainous protected areas. Part 1—earth sciences. TPN–PTPNoZ Org., Cracow, pp 97–104
  • 7. Geonics (2016) User manual of conductivity meter EM34-3XL. Geonics Ltd., Mississauga
  • 8. Klimaszewski M (1988) Relief of Polish Tatra Mountains. Polish Scientific Press, Warsaw
  • 9. Loke MH (1999a) Electrical imaging surveys for environmental and engineering studies—a practical guide to 2-D and 3-D surveys. Geotomosoft Solutions Firm, Penang
  • 10. Loke MH (1999b) Time-lapse resistivity imaging inversion. In: Proceedings of the 5th meeting of the environmental and engineering geophysical society European section, Budapest, Hungary
  • 11. Loke MH, Barker RD (1996) Rapid least-squares inversion of apparent resistivity pseudosections using a quasi-Newton method. Geophys Prospect 44:131–152
  • 12. Mala (2003) Basic and advanced radar theory. MALA GeoScience AB, Mala
  • 13. ReflexW (2016) Manual of ReflexW computer program. SandmeierGeo firm, Karlsruhe
  • 14. Sharma PV (1997) An introduction to applied and environmental geophysics. Cambridge University Press, Cambridge
  • 15. Tomecka-Suchoń S, Gołębiowski T (2010) Using of GPR method for examination of postglacial deposits in the alp of Ornak (the Tatra Mountains). In: Proceedings of XIX congress of the Carpathian-Balkan Geological Association, vol 39, no 1–2, p 394
  • 16. Tomecka-Suchoń S, Gołębiowski T (2011a) Feasibility analysis of using GPR method for the examination of postglacial deposits in mountainous geological environment. Geology 37(3):375–382 (AGH-UST Ed.)
  • 17. Tomecka-Suchoń S, Gołębiowski T (2011b),Using of GPR method for examination of post-glacial deposits in the Alp of Ornak (the Tatra Mountains). Kwartalnik AGH Geologia, Wyd. AGH, Kraków 2011, t. 37, z. 3: pp 375–382
  • 18. Zasadni J, Kłapyta P (2014) The Tatra Mountains during the last glacial maximum. J Maps 10(3):440–456
  • 19. Żogała B, Dubiel R, Gorszczyńska H, Malina R (2001) Geophysical recognition of shallow bed-rock in selected area of Piec Stawow Polskich Valley. Geol Rev XLVI(1–2):111–118
  • 20. Żogała B, Dubiel R, Gorszczyńska H, Malina R (2002) Application of geophysical methods for recognising of shallow part of geological medium with the examples from the Tatra Mountains. In: Borowiec W, Kotarba A, Kownacki A, Krzan Z, Mirek Z (eds) Changes of natural environment in the Tatra Mountains. Part 1—earth sciences. TPN–PTPNoZ Org., Cracow, pp 55–60
  • 21. Żogała B, Dubiel R, Dzik T, Dzik G, Mendecki M (2010) Application of geophysical methods form recognising of rock debris in the Tatra Mountains. In: Kotarba A (ed) Science and management of the Tatra Mountains and their vanity. Part 1—earth sciences. TPN–PTPNoZ Org., Cracow, pp 165–171
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-2a31f7ec-3ceb-469e-ad8e-824339812edb
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