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Tytuł artykułu

Mapping of the north-eastern part of Kozłowicka buried valley based on geoelectrical data

Treść / Zawartość
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The paper is aiming to determinate the extent of the northeastern arm of Kozłowicka buried valley on the grounds of own research by means of electrical resistivity tomography – ERT and available archival researches. On the Hydrogeological map of Poland, Żyrardów sheet (Felter and Nowicki, 1998a, b) Kozłowicka buried valley was differentiated as an individual hydrogeological unit. The results of the analysis show that the extent of the structure, defined by its upper boundary, differs significantly from the one suggested on the sheet of Hydrogeological map of Poland. Since there was no data available in the northeastern part of the discussed arm of Kozłowicka buried valley, the northern boundary was defined only based on available geoelectrical sounding profiles (Czerwińska, 1988; Topolewska, 2015). In order to confirm suggested solution, geoelectrical research by means of electrical resistivity tomography (ERT) was conducted. The measurements were performed along 3 profiles located in the area of interest. The authors would like to point out the need of the usage of ERT in mapping and studying buried structures that might be groundwater reservoirs. As a result, one obtains quasi-continuous image of electrical resistivity of the subsurface. Due to the contrast of electrical properties of sediments, it is possible to determine upper and bottom surfaces of electrical properties sediments, it is possible to determine upper and bottom surfaces of buried structures, formed within glacial deposits.
Czasopismo
Rocznik
Strony
91--101
Opis fizyczny
Bibliogr. 40 poz., rys.
Twórcy
  • Faculty of Geology, University of Warsaw, ul. Żwirki i Wigury 93, 02-089 Warszawa, Poland
autor
  • Faculty of Geology, University of Warsaw, ul. Żwirki i Wigury 93, 02-089 Warszawa, Poland
autor
  • Faculty of Geology, University of Warsaw, ul. Żwirki i Wigury 93, 02-089 Warszawa, Poland
Bibliografia
  • Ahmad, J., Schmitt, D.R., 2005. Seismic and resistivity imaging for Quaternary channels, Rainbow Lake Northwest Alberta, Canada. CSEG RECORDER 30, 40–43.
  • Aning, A.A., Sackey, N., Jakalia, I.S., Sedoawu, O., Tetteh, E.H., Hinson, G., Akorlie, R.K., Appiah, D., Quaye, E.K., 2014. Electrical Resistivity as a Geophysical Mapping Tool; A Case Study Of The New Art Department, Knust- Ghana. International Journal of Scientific and Research Publications 4 (1), 1–7.
  • Balcerkiewicz, Z., 1989. Hydrogeological documentation of groundwater resources in Quaternary sediments in the region of Żyrardów – Feliksów – Stanisławów (Dokumentacja hydro- geologiczna zasobów wód podziemnych w utworach czwartorzędowych w rejonie Żyrardów – Feliksów – Stanisławów.) Przeds. Produkcji Różnej, Handlu i Usług DEMPOL Poznań (in Polish).
  • Białostocki, R., Farbisz, J., 2007. Geoelectrical resistivity surveys. Current state and possibilities of taking advantage of the results (Badania geoelektryczne-elektrooporowe. Stan aktualny i możliwości wykorzystania wyników.) Geofizyka. Biuletyn Informacyjny 5, 28–41 (in Polish).
  • Binley, A., Cassiani, G., Middleton, R., Winship, P., 2002. Vadose zone flow model parameterisation using cross-borehole radar and resistivity imaging. Journal of Hydrology 267, 147–159.
  • Black, R.A., Frischknecht, F.C., Hazlewood, R.M, Jackson, W.H., 1962. Geophysical methods of exploring for buried channels in the Monument Valley area, Arizona and Utah, Bulletin 1083, 161–288.
  • Chongoa, M. Wibroeb, J., Staal-Thomsenb, K., Mosesb, M., Nyambea, I.A., Larsenc, F. Bauer-Gottweinb, P., 2011. The use of Time Domain Electromagnetic method and Continuous Vertical Electrical Sounding to map groundwater salinity in the Barotse subbasin, Zambia. Physics and Chemistry of the Earth, Parts A/B/C, 36, 14–15, 798–805.
  • Czerwińska, I., 1988. Documentation of geoelectrical surveys, subject: Water intake – Żyrardów (Dokumentacja badań geoelektrycznych, temat: Ujęcie wody – Żyrardów) (in Polish).
  • Dahlin, T., 1996. 2D resistivity surveying for environmental and engineering applications. First Break 14 (7), 275–283.
  • Dahlin, T., Zhou, B., 2006. Multiple-gradient array measurements for multichannel 2D resistivity imaging. Near Surface Geo- physics 4 (2), 113–123.
  • Daily, W., Ramirez, A., Binley, A., LeBrecque, D., 2004. Electrical resistance tomography. The Leading Edge 23(5), 438–442.
  • Ercoli, M., Pauselli, C., Forte, E., Di Matteo, L., Mazzocca, M., Frigeri, A., Federico C., 2012. A multidisciplinary geological and geophysical approach to define structural and hydrogeological implications of the Molinaccio spring (Spello, Italy). Journal of Applied Geophysics 77, 72–82.
  • Farbisz, J., Białostocki, R., Zochniak, K., 2010. Geoelectrical resistivity surveys in PBG – yesterday, today and in the coming years (Badania geoelektryczne-elektrooporowe w PBG – wczoraj, dziś i w perspektywie najbliższych lat.) Geofizyka, Biuletyn Informacyjny 8, 86–107 (in Polish).
  • Felter, A., Nowicki, Z., 1998a. Comment to hydrogeological map of Poland 1:50 000, sheet Żyrardów no. 557 (Objaśnienia do Mapy hydrogeologicznej Polski w skali 1:50,000 arkusz Żyrardów (557)) (in Polish).
  • Felter, A., Nowicki, Z., 1998b. Hydrogeological map of Poland 1:50,000, sheet Żyrardów no. 557 (Mapa hydrogeologiczna Polski w skali 1:50 000 arkusz Żyrardów (557)) (in Polish).
  • Felter, A., Nowicki, Z., 2003. Groundwater reservoirs in buried Quaternary valleys in the west Mazowsze area. Współczesne Problemy Hydrogeologii. Tom XI, (1), 69–76. Wyd. PGdań. Gdańsk
  • Herbich, P., Kazimierski, B., Knyszyński, F., Prażak, J., Nowicki, Z., 2007. Subregion Middle Vistula Lowland (Subregion środkowej Wisły nizinny). in: Paczyński, B., Sadurski, A., (Eds.) Regional hydrogeology of Poland (Hydrogeologia Regionalna Polski), t. 1, Freshwater (Wody słodkie), 205–219. Państwowy Insytut Geologiczny. Warszawa (in Polish).
  • Kemna, A., Kulessa, B., Vereecken, H., 2002. Imaging and characterisation of subsurface solute transport using electrical resistivity tomography (ERT) and equivalent transport models. Journal of Hydrology 267 (3–4), 125–146.
  • Khaki, M., Yusoff, I., Islami, N., Saboohi, S., 2016. Integrated geoelectrical and hydrogeochemical investigation for map- ping the aquifer at Langat Basin, Malaysia. Environmental Earth Sciences 75, 304.
  • Kondracki, J., 2009. Regional geography of Poland (Geografia regionalna Polski). PWN (in Polish).
  • Linder, L., Marks, L., 1999. New approach to stratigraphy of palaeolake and glacial sediments of the younger Middle Pleis- tocene in mid-eastern Poland. Geol. Quart. 43, 1–8.
  • Lindner, L., Marks, L., 2012. Climatostratigraphic subdivision of the Pleistocene Middle Polish Complex in Poland. Przegląd Geologiczny 60 (1), 36–45.
  • Loke, M.H., Lane Jr., J.W., 2004. Inversion of data from electrical resistivity imaging surveys in water-covered areas, Explor. Geophys. 35 (4), 266–271.
  • Loke, M.H., Chambers, J.E., Rucker, D.F., Kuras, O., Wilkinson, P.B., 2013. Recent developments in the direct-current geoelectrical imaging method. Journal of Applied Geophysics 95, 135–156.
  • Mastrocicco, M., Vignoli, G., Colombani, N., Zeid, N.A., 2010. Surface electrical resistivity tomography and hydrogeological characterization to constrain groundwater flow modeling in an agricultural field site near Ferrara (Italy). Environmental Earth Sciences 61 (2), 311–322.
  • Palacky, G.V., 1987. Resistivity characteristics of geologic targets. Electromagnetic methods in applied geophysics. Theory 1, 52–129.
  • Ratnakumari, Y., Rai, S.N., Thiagarajan, S., Kumar, D., 2012. 2D Electrical resistivity imaging for delineation of deeper aquifers in a part of the Chandrabhaga river basin, Nagpur District, Maharashtra, India. Current science 102 (1), 61–69.
  • Różycki, S.Z., 1972. Pleistocene of Central Poland in the back- ground of Late Tertiary (Plejstocen Polski Środkowej na tle przeszłości w górnym trzeciorzędzie). PWN. Warszawa (in Polish).
  • Różycki, S.Z., 1980. Principles of stratigraphic subdivisions of Quaternary of Poland. Quatern. Stud. Pol. 2, 99–106.
  • Saleh, H., Samsudin, A.R., 2013. Geoelectrical resistivity characterization of sedimentary rocks in Dent Peninsular, Lahad Datu, Sabah. Borneo Science 32, 33–43.
  • Samouëlian, A., Cousin, I., Tabbagh, A., Bruand, A., Richard, G., 2005. Electrical resistivity survey in soil science: a review. Soil and Tillage Research 83 (2), 173–193.
  • Smith, E.M., 1974. Exploration for a Buried Valley by Resistivity and Thermal Probe Surveys. Ground Water 12 (2), 78–83.
  • Smith, R.C., Sjogren, D.B., 2006. An evaluation of electrical resistivity imaging (ERI) in Quaternary sediments, southern Alberta, Canada. Geosphere 2(6), 287–298.
  • Szalewicz, H., 1993. Detailed Geological Map of Poland in scale 1:50,000, sheet Żyrardów (Szczegółowa mapa geologiczna Polski ark. Żyrardów.)
  • Topolewska, S., 2015. Hydrogeological mapping of northeastern arm of Kozłowicka buried valley by means of ERT and ves. Master thesis. Faculty of Geology, University of Warsaw.
  • van Overmeeren, R.A., Ritsema, I.L., 1988. Continuous vertical electrical sounding. First Break 6(10), 313–324.
  • van Schoor, M., 2002. Detection of sinkholes using 2D electrical resistivity imaging. Journal of Applied Geophysics 50, 393–399.
  • Wysocki, R., 1996. Annex to the documentation PGK Żyrardów(Aneks do dokumentacji PGK Żyrardów) (in Polish).
  • Zhou, Q.Y., Shimada, J., Sato, A., 2001. Three-dimensional spatial and temporal monitoring of soil water content using electrical resistivity tomography. Water Resources Research 37, 273–286.
  • Zhou, W., Beck, B.F., Adams, A.L., 2002. Effective electrode array in mapping karst hazards in electrical resistivity tomography.Environ. Geol. 42, 922–928.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-72970cd7-32b9-40aa-8e53-2e0eef487d77
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