Formation specifics of engineering geological conditions in Belarus under the influence of erosion processes
- Authors: Pavlovsky A.I.1, Galkin A.N.2, Krasovskaya I.A.2, Shershnev O.V.3
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Affiliations:
- Belarusian National Technical University
- Masherov Vitebsk State University
- Skorina Gomel State University
- Issue: No 4 (2024)
- Pages: 3-13
- Section: Articles
- URL: https://ogarev-online.ru/0869-7809/article/view/274963
- DOI: https://doi.org/10.31857/S0869780924040012
- EDN: https://elibrary.ru/SGMTKO
- ID: 274963
Cite item
Abstract
The article presents the results of a comprehensive study of the development conditions and features of water erosion manifestation in various natural and economic settings as an important condition of the formation of engineering geological features of the territory. The authors have established that the development, forms of manifestation and intensity of water erosion processes in the territory of Belarus, with all the diversity of natural and economic situations, are controlled by the energy potential of the relief, the basin structure of the territory and human economic activity. Engineering geological conditions were typified for the development of water erosion processes. The most complex engineering geological situations are observed within the marginal glacial uplands, which have a high energy potential of the topography, a two-rock type of ground massif, and a complex basin structure; as well as in areas of active economic development.
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About the authors
A. I. Pavlovsky
Belarusian National Technical University
Author for correspondence.
Email: aipavlovsky@mail.ru
Belarus, pr. Nezavisimosti 65, Minsk, 220013
A. N. Galkin
Masherov Vitebsk State University
Email: galkin-alexandr@yandex.ru
Belarus, Moskovskii pr., 33, Vitebsk, 210038
I. A. Krasovskaya
Masherov Vitebsk State University
Email: galkin-alexandr@yandex.ru
Belarus, Moskovskii pr., 33, Vitebsk, 210038
O. V. Shershnev
Skorina Gomel State University
Email: natstudy@yandex.ru
Belarus, Sovetskaya ul., 104, Gomel, 246028
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