Transformation of abiotic components of the environment in areas of long-existing oil products logistics facilities

Authors

DOI:

https://doi.org/10.17308/geology.2019.1/1721

Keywords:

tank farm, oil pollution, surface sediments, groundwater, atmosphere, sources of pollution, anomalies

Abstract

The main directions of transformation of the abiotic components of the environment in areas of long-existing oil depots are determined. The role of the microrelief of the territory and the particle size distribution of soils during the spread of polluting elements is indicated. The results of the application of a new field device – a portable detector with a MWNT-based piezosensor – for the determination of pe-troleum products in soils and groundwater are presented. The ubiquitous pollution of the industrial site of the tank farm with oil products in concentrations exceeding the MPC by 20–80 times was revealed. Groundwater is maximally polluted in the lower part of the relief, associated with sources of pollution; overpasses of oil products. Pollution levels range from 50 MPC to the complete replacement of water with a lens of a pure oil product.

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Author Biographies

  • Ирина Ивановна Косинова, Voronezh State University

    head of the department of environmental geology, VSU, professor, Doctor of the Geological and Mineralogical Sciences

  • Виктория Александровна Бударина, Voronezh State University

    candidate of legal Sciences, associate Professor of Ecological Geology Department

  • О Г Фонова, Voronezh State University

    graduate student of the department of environmental geology

  • С В Долбилова, Voronezh State University

    master of the department of environmental geology

  • Е В Зинченко, Voronezh State University

    master of the department of environmental geology

References

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Published

2019-02-11

Issue

Section

Hydrogeology, Geoecology

How to Cite

Transformation of abiotic components of the environment in areas of long-existing oil products logistics facilities. (2019). Proceedings of Voronezh State University. Series: Geology, 1, 88-92. https://doi.org/10.17308/geology.2019.1/1721

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