The use of ground-penetration method for identification of lithological boundaties in fluvial relief forms


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Abstract

The article presents the studies of defining litological boundaries in fluvial forms of relief by a ground-penetration radar method. Restrictions of the method use, prospects of its application in fluvial geomorphology and geoecology are proved.

About the authors

Grigory Vladimirovich Lobanov

Bryansk State University named after Academician I.G.Petrovsky

Email: lobanov_grigorii@mail.ru
кандидат географических наук, доцент; Брянский государственный университет им. акад. И.Г.Петровского; Bryansk State University named after Academician I.G.Petrovsky

Alexandra Vasiljevna Polyakova

Bryansk State University named after Academician I.G.Petrovsky

Email: slavyanka56@mail.ru
аспирант; Брянский государственный университет им. акад. И.Г.Петровского; Bryansk State University named after Academician I.G.Petrovsky

Konstantin Yurjevich Mikheev

Bryansk State University named after Academician I.G.Petrovsky

Email: mighty_k@mail.ru
лаборант-исследователь; Брянский государственный университет им. акад. И.Г.Петровского; Bryansk State University named after Academician I.G.Petrovsky

References

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  5. Leclerc R.F. and Hickin E.J. (1997) The internal structure of scrolled floodplain deposits based on ground-penetrating radar, North Thompson River, British Columbia // Geomorphology. 1997. Vol. 21(1). P. 17-25, 29-38.
  6. Slowik M. Changes of river bed pattern and traces of anthropogenic intervention: The example of using GPR method (the Obra River, western Poland) // Applied Geography. 2011. Vol. 31(2). P. 784-799.
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