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Geochronological investigation of the Danube Djerdap Lake sediments (Serbia): sedimentology and inorganic composition

Само за регистроване кориснике
2020
Аутори
Kašanin-Grubin, Milica
Hagemann, Lukas
Gajica, Gordana
Štrbac, Snežana
Jovančićević, Branimir
Vasić, Nebojša
Šajnović, Aleksandra
Đogo-Mračević, Svetlana
Schwarzbauer, Jan
Чланак у часопису (Објављена верзија)
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Апстракт
The objective of this study is geochronological investigation of sedimentological and inorganic composition, in the Danube Djerdap Lake sediments in order to obtain reliable information about former pollution. Eleven samples were taken from the 135-cm-deep sediment core drilled at the Orlova location. Since the core represents sediments deposited during 1972–2016, the sedimentation rate of ~ 3 cm year−1 was estimated. Grain size, mineralogical and geochemical composition was determined. Sediments are sandy silts and clayey silts, and only the deepest and shallowest layers contain > 30% of sand-size fraction. The highest concentrations of minor elements are found in the oldest sediment (1972–1977) as a consequence of the high flux of the material from variable sources. During the sedimentation period (1975–1990), the concentrations of analyzed elements are generally decreasing until the beginning of 1990s. After this period, there are two distinct decreases and two distinct increases in... concentrations of elements. The fluctuations in minor element concentrations are a consequence of both natural and anthropogenic sources. Granitic rocks situated south are source of minerals that carry minor elements. Enrichment Factor, Geoaccumulation Index, Contamination Factor and Pollution Load Index indicate that concentrations of certain minor elements at specific depositional periods have anthropogenic source.

Кључне речи:
Danube Djerdap Lake / Geochronological investigation / Minor elements / Pollution indices
Извор:
Environmental Geochemistry and Health, 2020, 42, 2, 693-707
Издавач:
  • Springer Nature B.V.
Финансирање / пројекти:
  • Геохемијска испитивања седиментних стена - фосилна горива и загађивачи животне средине (RS-176006)
  • Петрогенеза и минерални ресурси Карпато-балканида и њихов значај у заштити животне средине (RS-176019)
  • Нове технологије за мониторинг и заштиту животног окружења од штетних хемијских супстанци и радијационог оптерећења (RS-43009)

DOI: 10.1007/s10653-019-00403-6

ISSN: 0269-4042

WoS: 000515328200025

Scopus: 2-s2.0-85071416968
[ Google Scholar ]
6
4
URI
https://farfar.pharmacy.bg.ac.rs/handle/123456789/3620
Колекције
  • Radovi istraživača / Researchers’ publications
Институција/група
Pharmacy
TY  - JOUR
AU  - Kašanin-Grubin, Milica
AU  - Hagemann, Lukas
AU  - Gajica, Gordana
AU  - Štrbac, Snežana
AU  - Jovančićević, Branimir
AU  - Vasić, Nebojša
AU  - Šajnović, Aleksandra
AU  - Đogo-Mračević, Svetlana
AU  - Schwarzbauer, Jan
PY  - 2020
UR  - https://farfar.pharmacy.bg.ac.rs/handle/123456789/3620
AB  - The objective of this study is geochronological investigation of sedimentological and inorganic composition, in the Danube Djerdap Lake sediments in order to obtain reliable information about former pollution. Eleven samples were taken from the 135-cm-deep sediment core drilled at the Orlova location. Since the core represents sediments deposited during 1972–2016, the sedimentation rate of ~ 3 cm year−1 was estimated. Grain size, mineralogical and geochemical composition was determined. Sediments are sandy silts and clayey silts, and only the deepest and shallowest layers contain > 30% of sand-size fraction. The highest concentrations of minor elements are found in the oldest sediment (1972–1977) as a consequence of the high flux of the material from variable sources. During the sedimentation period (1975–1990), the concentrations of analyzed elements are generally decreasing until the beginning of 1990s. After this period, there are two distinct decreases and two distinct increases in concentrations of elements. The fluctuations in minor element concentrations are a consequence of both natural and anthropogenic sources. Granitic rocks situated south are source of minerals that carry minor elements. Enrichment Factor, Geoaccumulation Index, Contamination Factor and Pollution Load Index indicate that concentrations of certain minor elements at specific depositional periods have anthropogenic source.
PB  - Springer Nature B.V.
T2  - Environmental Geochemistry and Health
T1  - Geochronological investigation of the Danube Djerdap Lake sediments (Serbia): sedimentology and inorganic composition
VL  - 42
IS  - 2
SP  - 693
EP  - 707
DO  - 10.1007/s10653-019-00403-6
ER  - 
@article{
author = "Kašanin-Grubin, Milica and Hagemann, Lukas and Gajica, Gordana and Štrbac, Snežana and Jovančićević, Branimir and Vasić, Nebojša and Šajnović, Aleksandra and Đogo-Mračević, Svetlana and Schwarzbauer, Jan",
year = "2020",
abstract = "The objective of this study is geochronological investigation of sedimentological and inorganic composition, in the Danube Djerdap Lake sediments in order to obtain reliable information about former pollution. Eleven samples were taken from the 135-cm-deep sediment core drilled at the Orlova location. Since the core represents sediments deposited during 1972–2016, the sedimentation rate of ~ 3 cm year−1 was estimated. Grain size, mineralogical and geochemical composition was determined. Sediments are sandy silts and clayey silts, and only the deepest and shallowest layers contain > 30% of sand-size fraction. The highest concentrations of minor elements are found in the oldest sediment (1972–1977) as a consequence of the high flux of the material from variable sources. During the sedimentation period (1975–1990), the concentrations of analyzed elements are generally decreasing until the beginning of 1990s. After this period, there are two distinct decreases and two distinct increases in concentrations of elements. The fluctuations in minor element concentrations are a consequence of both natural and anthropogenic sources. Granitic rocks situated south are source of minerals that carry minor elements. Enrichment Factor, Geoaccumulation Index, Contamination Factor and Pollution Load Index indicate that concentrations of certain minor elements at specific depositional periods have anthropogenic source.",
publisher = "Springer Nature B.V.",
journal = "Environmental Geochemistry and Health",
title = "Geochronological investigation of the Danube Djerdap Lake sediments (Serbia): sedimentology and inorganic composition",
volume = "42",
number = "2",
pages = "693-707",
doi = "10.1007/s10653-019-00403-6"
}
Kašanin-Grubin, M., Hagemann, L., Gajica, G., Štrbac, S., Jovančićević, B., Vasić, N., Šajnović, A., Đogo-Mračević, S.,& Schwarzbauer, J.. (2020). Geochronological investigation of the Danube Djerdap Lake sediments (Serbia): sedimentology and inorganic composition. in Environmental Geochemistry and Health
Springer Nature B.V.., 42(2), 693-707.
https://doi.org/10.1007/s10653-019-00403-6
Kašanin-Grubin M, Hagemann L, Gajica G, Štrbac S, Jovančićević B, Vasić N, Šajnović A, Đogo-Mračević S, Schwarzbauer J. Geochronological investigation of the Danube Djerdap Lake sediments (Serbia): sedimentology and inorganic composition. in Environmental Geochemistry and Health. 2020;42(2):693-707.
doi:10.1007/s10653-019-00403-6 .
Kašanin-Grubin, Milica, Hagemann, Lukas, Gajica, Gordana, Štrbac, Snežana, Jovančićević, Branimir, Vasić, Nebojša, Šajnović, Aleksandra, Đogo-Mračević, Svetlana, Schwarzbauer, Jan, "Geochronological investigation of the Danube Djerdap Lake sediments (Serbia): sedimentology and inorganic composition" in Environmental Geochemistry and Health, 42, no. 2 (2020):693-707,
https://doi.org/10.1007/s10653-019-00403-6 . .

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