The usefulness of ground-penetrating radar images for the research of a large sand-bed braided river: case study from the Vistula River (central Poland)
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Keywords

sedimentary architecture
sand-bed braided river
lithofacies
ground-penetrating radar
radar facies
Vistula River

How to Cite

Lejzerowicz, A., Kowalczyk, S., & Wysocka, A. (2014). The usefulness of ground-penetrating radar images for the research of a large sand-bed braided river: case study from the Vistula River (central Poland). Geologos, 20(1), 35–47. https://doi.org/10.2478/logos-2014-0003

Abstract

Ground-penetrating radar (GPR) surveys and sedimentological outcrop analyses were combined in order to determine the reflection patterns and internal architecture of terrace deposits of the Vistula River at Kępa Zawadowska in the southern part of Warsaw (central Poland). The sedimentary analyses concerned the granulometric composition and lithofacies analysis. The 34 GPR profiles, which were obtained in two outcrops, using a Malå RAMAC/GPR system with 500-MHz and 250-MHz shielded antennas, were up to 100 m long. The most characteristic ground-penetrating radar profiles are presented; they show a high-resolution data set of radar facies. The GPR data suggest the presence of three geophysically different units, namely with high-angle inclined reflections (radar facies 1), with discontinuous undulating or trough-shaped reflections (radar facies 2), and with low-angle reflections (radar facies 3). The internal structure of the fluvial deposits was obtained by integration of the GPR and sedimentological data, which combination provides a more accurate visualisation of sedimentary units than do reconstructions that are based only on standard lithologic point data.

https://doi.org/10.2478/logos-2014-0003
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References

Ashworth, P.J., Sambrooh Smith, G.H., Best J.L., Bridge, J.S., Lane, S.N., Lunt I.A., Reesink, A.J.H., Simpson, C.J. & Thomas, R.E., 2011. Evolution and sedimentology of a channel fill in the sandy braided South Saskatchewan River and its comparision to the deposits of an adjacent compound bar. Sedimentology 58, 1860-1883.

Babiński, Z., 1992. Współczesne procesy korytowe dolnej Wisły [The present-day fluvial processes of the lower Vistula River]. Geographical Notes 157, 171 pp. (in Polish with English summary).

Daniels, D.J., 2004. Ground-penetrating radar (2nd ed.). The Institute of Electrical Engineers, London, 726 pp.

Eyles, N., Eyles, C.H. & Miall, A.D., 1983. Lithofacies types and vertical profile models; an alternative approach to the description and environmantal interpretation of glacial diamict and diamictite sequences. Sedimentology 30, 293-410.

Fal, B., Bogdanowicz, E., Czernuszenko, W., Dobrzyńska, I. & Koczyńska, A., 1997. Przepływy charakterystyczne głównych rzek polskich w latach 1951-1990 [Characteristic flows in main Poland’s rivers in the years 1951-1990]. Materiały Badawcze IMGW, Seria Hydrologia i Oceanologia 21, 174pp. (in Polish)

Falkowski, T., 2006. Naturalne czynniki stabilizujące wybrane odcinki strefy korytowej Wisły środkowej [Factors of natural stability of the middle Vistula River channel zones]. Treatises and Monographs of Warsaw University of Life Sciences 312, 128 pp. (in Polish with English summary)

Folk, R.L. & Ward, W.C., 1957. Brazos River bar: a study in the significance of grain size parameters. Journal of Sedimentary Petrology 27, 3-26.

Haczewski, G. & Kukulak, J., 2004. Early Holocene landslide-dammed lake in Bieszczady Mountains (Polish eastern Carpathians) and its evolution. Studia Geomorphologica Carpatho-Balcanica 38, 83-96.

Hickin, A.S., Kerr, B., Barchyn, T.E. & Paulen, R.C., 2009. Ground-penetrating radar and capacitively coupled resistivity to investigate fluvial architecture and grain-size distribution of a gravel floodplain in Northeast British Columbia, Canada. Journal of Sedimentary Research 79, 457-477.

Jol, H.M., 2009. Ground penetrating radar - theory and applications. Elsevier (London), 524 pp.

Karczewski, J., Ortyl, Ł. & Pasterniak, M., 2011. Zarys metody georadarowej. Wydanie 2. [Outline of GPR method. 2nd edition] Wydawnictwa AGH (Kraków), 346 pp.

Lamparski, P., 2004. Formy i osady czwartorzędowe w świetle badań georadarowych [Quaternary forms and deposits in the light of ground penetrating radar investigations]. Prace Geograficzne 194, 1-115. (in Polish with English summary)

Leclerc, R.F. & Hickin, E.J., 1997. The internal structure of scrolled floodplain deposits based on ground penetrating radar, North Thompson river, British Columbia. Geomorphology 21, 17-38.

Lunt, I.A., Bridge, J.S. & Tye, R.S., 2004. A quantitative, three-dimensional model of gravelly braided rivers. Sedimentology 51, 377-414.

Miall, A.D., 1977. A review of the braided river depositional environment. Earth-Science Reviews 13, 1-62.

Miall, A.D., 1985. Architectural element analysis: a new method of facies analysis applied to fluvial deposits. Earth-Science Reviews 22, 261-308.

Mycielska-Dowigałło, E., 1995. Wybrane cechy teksturalne osadów i ich wartość interpretacyjna [Selected textural features of deposits and their interpretation value]. [In:] E. Mycielska-Dowgiałło & J. Rutkowski (Eds): Metody badań osadów czwartorzędowych. Wybrane metody i interpretacja wyników [Research studies of the Quaternary sediments. Some methods and interpretation of the results]. Faculty of Geography and Regional Studies, University of Warsaw Press (Warszawa), 29-104. (in Polish with English summary)

Mycielska-Dowgiałło, E., 2007. Metody badań cech teksturalnych osadów klastycznych i wartość interpre tacyjna wyników [Research methods for textural features of clastic deposits and their significance for interpretation]. [In:] E. Mycielska-Dowgiałło & J. Rutkowski (Eds): Badania cech teksturalnych osadów czwartorzędowych i wybrane metody oznaczania ich wieku [Textural features studies of quaternary deposits and selected methods their age determination]. SWPR Press (Warszawa), 95-180. (in Polish with English summary)

Neal, A., 2004. Ground-penetrating radar and its use in sedimentology: principles, problems and progress. Earth-Science Reviews 66, 261-330.

Olszak, J. & Karczewski, J., 2008. Przydatność profilowań georadarowych w interpretacji budowy tarasów rzecznych (dolina Kamienicy, polskie Karpaty zewnętrzne) [Usefulness of GPR measurements in interpretation of structures of river terraces (Kamienica River Valley, Polish Outer Carpathians)]. Przegląd Geologiczny 56, 330-334. (in Polish with English summary)

Racinowski, R., Szczypek, T. & Wach, T., 2001. Prezentacja i interpretacja wyników badań uziarnienia osadów czwartorzędowych [Presentation and interpretation of the results on the granulation of quaternary sediments]. Silesian University (Katowice), 146 pp. (in Polish)

Rice, S.P., Church, M., Woolridge, C.L. & Hickin, E.J., 2009. Morphology and evolution of bars of a wandering gravel-bed river; lower Fraser river, British Columbia, Canada. Sedimentology 56, 709-736.

Sambrook Smith, G.H., Ashworth, P.J., Best, J.L., Woodward, J. & Simpson, C.J., 2006. The sedimentology and alluvial architecture of the sandy braided South Saskatchewan River, Canada. Sedimentology 53, 413-434.

Skelly, R.L., Bristow, Ch.S. & Ethridge, F.G., 2003. Architecture of channel-belt deposits in an aggrading shallow sandbed braided river: the lower Niobrara river, northeast Nebraska. Sedimentary Geology 158, 249-270.

Słowik, M., 2011. Reconstructing migration phases of meandering channels by means of ground-penetrating radar (GPR): the case of the Obra River, Poland. Journal of Soils and Sediments 11, 1262-1278.

Słowik M., 2012. Influence of measurement conditions on depth range and resolution of GPR images: the example of lowland valley alluvial fill (the Obra River, Poland). Journal of Applied Geophysics 85, 1-14.

Starkel, L., 2011. Historia doliny Wisły od ostatniego zlodowacenia do dziś [Evolution of the Vistula River valley since the last glaciation till present]. Monographies of Polish Academy of Science 2, 263 pp. (in Polish with English summary)

Van Dam, R. L., 2001. Causes of ground-penetrating radar reflections in sediment. Ph.D. thesis Vrije Universiteit Amsterdam, 110 pp.

Van Dam, R.L. & Schlager, W., 2000. Identifying causes of ground-penetrating radar reflections using time-domain reflectometry and sedimentological analyses. Sedimentology 47, 435-450.

Vandenberghe J. & Van Overmeeren, R.A., 1999. Ground penetrating radar images of selected fluvial deposits in the Netherlands. Sedimentary Geology 128, 245-270.

Woodward, J., Ashworth, P.J., Best, J.L., Sambrook Smith, G.H. & Simpson, C.J., 2003. The use and application of GPR in sandy fluvial environments: methodological considerations. [In:] C.S.Bristow & H.M. Jol (Eds): Ground penetrating radar in sediments. Geological Society, London, Special Publications 211, 127-142.

Zieliński, T., 1995. Kod litofacjalny i litogenetyczny - konstrukcja i zastosowanie [Lithofacies and genetic codes: construction and application]. [In:] E. Mycielska- Dowgiałło & J. Rutkowski (Eds): Metody badań osadów czwartorzędowych. Wybrane metody i interpretacja wyników [Research studies of the Quaternary sediments. Some methods and interpretation of the results] . University of Warsaw Press (Warszawa), 220-235. (in Polish with English summary)

Zieliński, T., 1998. Litofacjalna identyfikacja osadów rzecznych [Lithofacial identification of alluvial sediments]. [In:] E. Mycielska-Dowgiałło (Ed.): Struktury sedymentacyjne sedymentacyjne i postsedymentacyjne postsedymentacyjne w osadach czwartorzędowych [Sedimentary and postsedimentary structures in Quaternary sediments and their value for interpretation]. Faculty of Geography and Regional Studies, University of Warsaw Press (Warszawa), 195-260. (in Polish)

Zieliński, T. & Pisarska-Jamroży, M., 2012. Jakie cechy litologiczne osadów warto kodować, a jakie nie? [Which features of deposits should be included in a code and which not?] Przegląd Geologiczny 60, 387-397. (in Polish with English summary).