Genetic and facial structure of quaternary deposits on the territory of the Gomel chemical plant

Authors

  • Oleg V. Shershnyov Francisk Skorina Gomel State University, 104 Saveckaja Street, Gomel 246026, Belarus
  • Aleksandr I. Pavlovskii Francisk Skorina Gomel State University, 104 Saveckaja Street, Gomel 246026, Belarus

Keywords:

quaternary deposits, low permeable layers, genetic type, facies, technogenic deposits

Abstract

Analysis of lithological and genetic features quaternary deposits within the influence zone of industrial objects continues to be an urgent task of modern geology and geoecology. The article presents the results of studies of the lithologic features of quaternary deposits of the first from the surface of the low permeable layer underlying the ground aquifer within the sanitary protection zone of the Gomel chemical plant (GCP). In its structure, genetic types, groups of facies and facial varieties were identified. Large-scale (1 : 25 000) mapping of the established facies of quaternary deposits has been carried out. The present-day appearance of the formed natural and technogenic landscape has been studied. It has been established technolithomorphological changes of the geological and geomorphological basis of natural landscapes took place in the production zone of the plant. Facies of technogenic genesis has been identified.

Author Biographies

  • Oleg V. Shershnyov, Francisk Skorina Gomel State University, 104 Saveckaja Street, Gomel 246026, Belarus

    PhD (geography), docent; associate professor at the department of social and humanitarian disciplines, Institute of skills development and staff retraining

  • Aleksandr I. Pavlovskii, Francisk Skorina Gomel State University, 104 Saveckaja Street, Gomel 246026, Belarus

    PhD (geography), docent; head of the department of geology and geography, faculty of geology and geography

References

  1. Galkin AN. Diffuzionno-osmoticheskie svoistva glinistykh gruntov Gomel’skogo promyshlennogo raiona [Diffusion and osmotic properties of clay soils of Gomel industrial region] [dissertation]. Мoscow: Moscow State University; 1999. 169 p. Russian.
  2. Kotsur VV. Geokhimiya podzemnykh vod zony aktivnogo vodoobmena na territorii vliyaniya Gomel’skogo khimicheskogo zavoda [Geochemistry of underground waters in the zone of active water exchange on the territory influenced by Gomel chemical plant] [abstract of dissertation]. Minsk: Institute of Geological Sciences, National Academy of Sciences of Belarus; 2004. 21 p. Russian.
  3. Zhoglo VG, Galkin AN. Monitoring podzemnykh vod na vodozaborakh i ekologicheski opasnykh ob’ektakh yugo-vostoka Belarusi [Groundwater monitoring at water intakes and environmentally hazardous facilities in the South-East of Belarus]. Vitebsk: Vitebsk State University named after P. M. Masherov; 2008. 161 p. Russian.
  4. Shershnyov OV, Pavlovsky AI, Prilutsky IO. Estimation of scale and extent of contamination of subterranean water in the influence area of the Gomel chemical plant. Prirodnye resursy. 2013;1:44 –50. Russian.
  5. Shershnyov OV. Technogenic hydrogeochemical anomalies within the influence area of industrial chemichal dumps. Journal of the Belarusian State University. Geography and Geology. 2017;1:130 –136. Russian.
  6. San’ko AF, Yartsev VI, Dubman AV. Geneticheskie tipy i fatsii chetvertichnykh otlozhenii Belarusi [Genetic types and facies of quaternary deposits of Belarus]. Minsk: Pravo i ekonomika; 2012. 311 p. Russian.
  7. Lavrushin YuA. Stroenie i formirovanie osnovnykh moren materikovykh oledenenii [Structure and development of ground moraines of continental glaciations]. Moscow: Nauka; 1976. 244 p. Russian.

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Published

2019-06-12

How to Cite

[1]
Shershnyov, O.V. and Pavlovskii, A.I. 2019. Genetic and facial structure of quaternary deposits on the territory of the Gomel chemical plant. Journal of the Belarusian State University. Geography and Geology. 1 (Jun. 2019), 95–103. DOI:https://doi.org/10.33581/2521-6740-2019-1-95-103.