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Mineralogical–Geochemical Characteristics of the Snow Cover in Areas with Mining and Ore-Processing Facilities. / Opekunov, A. Yu; Opekunova, M. G.; Kukushkin, S. Yu; Yanson, S. Yu; Арестова, Ирина; Sheinerman, N. A.; Spasskii, V. V.; Papyan, E. E.; Elsukova, E. Yu.

In: Geochemistry International, Vol. 59, No. 7, 01.07.2021, p. 711-724.

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@article{0809ff5cc67a43ef9c0bc6e1a85e927c,
title = "Mineralogical–Geochemical Characteristics of the Snow Cover in Areas with Mining and Ore-Processing Facilities",
abstract = "Abstract—: Mineralogical–geochemical properties of snow were studied in the activity areas of the mining and ore-processing companies Severonikel in Monchegorsk, Karelsky Okatysh in Kostomuksha, and Sibay Mining and Processing Company in Sibay. The mineralogical and chemical compositions of the aerosols corresponds to the metallogeny of the study areas and the ore specialization of enterprises. The solid aerosols consist of the rock-forming and accessory minerals and artificial anthropogenic materials: slag particles and Ni–Fe–Co ± Cu aggregates. The presence of microplastics in the composition of solid aerosols was established within residential areas and on the territory of the Kostomuksha State Reserve, which is under the influence of transboundary transport. Concentrations of metals (Fe, Mn, Ni, Cu, Zn, Cd, and Pb) in the aerosols and snowmelt water are much higher than the average concentrations of these metals in the Earth{\textquoteright}s crust and natural waters. The pH of the snowmelt water is determined by the landscape–geochemical conditions and determines the solubility of metals: the minimum in the steppe landscapes of the Sibay area and the maximum in the Monchetundra (Monchegorsk test site). Within the latter, dissolved forms of chalcophiles and Ni predominate over the solid phase. Dust, metal, and ionic loads on the territory have been calculated. Retrospective analysis over the past 25 years has shown significant changes in the composition of aerosols within the Monchegorsk reference area due to the exclusion of the Talnakh ore dressing process from production. Among the studied emission sources of metals, the greatest contribution to the biogeochemical cycling is made by the Severonikel facilities.",
keywords = "aerosols, Kostomuksha, matte, metals, microplastic pollution, mineralogical composition, mining company, Monchegorsk, Sibay, snowmelt water, EMISSIONS, COPPER, NICKEL, CHEMISTRY, KOLA-PENINSULA",
author = "Opekunov, {A. Yu} and Opekunova, {M. G.} and Kukushkin, {S. Yu} and Yanson, {S. Yu} and Ирина Арестова and Sheinerman, {N. A.} and Spasskii, {V. V.} and Papyan, {E. E.} and Elsukova, {E. Yu}",
note = "Publisher Copyright: {\textcopyright} 2021, Pleiades Publishing, Ltd.",
year = "2021",
month = jul,
day = "1",
doi = "10.1134/s0016702921060070",
language = "English",
volume = "59",
pages = "711--724",
journal = "Geochemistry International",
issn = "0016-7029",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "7",

}

RIS

TY - JOUR

T1 - Mineralogical–Geochemical Characteristics of the Snow Cover in Areas with Mining and Ore-Processing Facilities

AU - Opekunov, A. Yu

AU - Opekunova, M. G.

AU - Kukushkin, S. Yu

AU - Yanson, S. Yu

AU - Арестова, Ирина

AU - Sheinerman, N. A.

AU - Spasskii, V. V.

AU - Papyan, E. E.

AU - Elsukova, E. Yu

N1 - Publisher Copyright: © 2021, Pleiades Publishing, Ltd.

PY - 2021/7/1

Y1 - 2021/7/1

N2 - Abstract—: Mineralogical–geochemical properties of snow were studied in the activity areas of the mining and ore-processing companies Severonikel in Monchegorsk, Karelsky Okatysh in Kostomuksha, and Sibay Mining and Processing Company in Sibay. The mineralogical and chemical compositions of the aerosols corresponds to the metallogeny of the study areas and the ore specialization of enterprises. The solid aerosols consist of the rock-forming and accessory minerals and artificial anthropogenic materials: slag particles and Ni–Fe–Co ± Cu aggregates. The presence of microplastics in the composition of solid aerosols was established within residential areas and on the territory of the Kostomuksha State Reserve, which is under the influence of transboundary transport. Concentrations of metals (Fe, Mn, Ni, Cu, Zn, Cd, and Pb) in the aerosols and snowmelt water are much higher than the average concentrations of these metals in the Earth’s crust and natural waters. The pH of the snowmelt water is determined by the landscape–geochemical conditions and determines the solubility of metals: the minimum in the steppe landscapes of the Sibay area and the maximum in the Monchetundra (Monchegorsk test site). Within the latter, dissolved forms of chalcophiles and Ni predominate over the solid phase. Dust, metal, and ionic loads on the territory have been calculated. Retrospective analysis over the past 25 years has shown significant changes in the composition of aerosols within the Monchegorsk reference area due to the exclusion of the Talnakh ore dressing process from production. Among the studied emission sources of metals, the greatest contribution to the biogeochemical cycling is made by the Severonikel facilities.

AB - Abstract—: Mineralogical–geochemical properties of snow were studied in the activity areas of the mining and ore-processing companies Severonikel in Monchegorsk, Karelsky Okatysh in Kostomuksha, and Sibay Mining and Processing Company in Sibay. The mineralogical and chemical compositions of the aerosols corresponds to the metallogeny of the study areas and the ore specialization of enterprises. The solid aerosols consist of the rock-forming and accessory minerals and artificial anthropogenic materials: slag particles and Ni–Fe–Co ± Cu aggregates. The presence of microplastics in the composition of solid aerosols was established within residential areas and on the territory of the Kostomuksha State Reserve, which is under the influence of transboundary transport. Concentrations of metals (Fe, Mn, Ni, Cu, Zn, Cd, and Pb) in the aerosols and snowmelt water are much higher than the average concentrations of these metals in the Earth’s crust and natural waters. The pH of the snowmelt water is determined by the landscape–geochemical conditions and determines the solubility of metals: the minimum in the steppe landscapes of the Sibay area and the maximum in the Monchetundra (Monchegorsk test site). Within the latter, dissolved forms of chalcophiles and Ni predominate over the solid phase. Dust, metal, and ionic loads on the territory have been calculated. Retrospective analysis over the past 25 years has shown significant changes in the composition of aerosols within the Monchegorsk reference area due to the exclusion of the Talnakh ore dressing process from production. Among the studied emission sources of metals, the greatest contribution to the biogeochemical cycling is made by the Severonikel facilities.

KW - aerosols

KW - Kostomuksha

KW - matte

KW - metals

KW - microplastic pollution

KW - mineralogical composition

KW - mining company

KW - Monchegorsk

KW - Sibay

KW - snowmelt water

KW - EMISSIONS

KW - COPPER

KW - NICKEL

KW - CHEMISTRY

KW - KOLA-PENINSULA

UR - http://www.scopus.com/inward/record.url?scp=85111245445&partnerID=8YFLogxK

UR - https://www.mendeley.com/catalogue/24b7a04d-ab9d-33c9-8f3a-002dca1d50da/

U2 - 10.1134/s0016702921060070

DO - 10.1134/s0016702921060070

M3 - Article

AN - SCOPUS:85111245445

VL - 59

SP - 711

EP - 724

JO - Geochemistry International

JF - Geochemistry International

SN - 0016-7029

IS - 7

ER -

ID: 84816265