Chalcophile elements (Hg, Cd, Pb, and As) in bottom sediments of water bodies of the white sea catchment area on the kola peninsula

2006 ◽  
Vol 44 (2) ◽  
pp. 205-208 ◽  
Author(s):  
V. A. Dauvalter
Keyword(s):  
Kola Peninsula ◽  
Bottom Sediments ◽  
Catchment Area ◽  
White Sea ◽  
Water Bodies ◽  
The White Sea ◽  
Chalcophile Elements

scholarly journals The Study of Uranium Accumulation in Marine Bottom Sediments: Effect of Redox Conditions at the Time of Sedimentation

Geosciences ◽  
2021 ◽  
Vol 11 (8) ◽  
pp. 332
Author(s):  
Nadezhda Khaustova ◽  
Yulia Tikhomirova ◽  
Svetlana Korost ◽  
Elena Poludetkina ◽  
Andrey Voropaev ◽  
...  
Keyword(s):  
Bottom Sediments ◽  
White Sea ◽  
Uranium Content ◽  
Black Shales ◽  
Redox Conditions ◽  
Source Rocks ◽  
Shelf Zone ◽  
The Black Sea ◽  
The White Sea ◽  
Run Off

To evaluate the effect of redox conditions at the sedimentation stage on uranium content and U/TOC ratio in marine source rocks, we analyzed the accumulation of uranium in modern marine bottom sediments formed in different redox conditions. The behavior of uranium from bottom sediments formed in oxidizing and sub-oxidizing settings has been studied on the sediments of the Upper Pleistocene–Holocene age accumulated in the coastal area of the White Sea (Kandalaksha Gulf). We studied the content of uranium, Eh, pH, TOC, C, H, N, and S element and isotope compositions and other parameters in two sampled columns of bottom sediments at a depth of 0–2.5 m. The composition of sediments was typical for the shelf zone where marine genesis mixes with the continental run-off. The upper layer of sediments (0–50 cm) were characterized by oxidizing conditions (Eh ~ 400 mV); with the increase in depth, redox conditions changed from oxidizing to reducing (0 ÷ 200 mV). The uranium concentration in the upper layer was 1–1.5 ppm, U/TOC ratio varied in the range of 0.8–1.1 ppmU/%TOC. The uranium content and U/TOC ratio increased up to the values of 2.6 ppm and 1.4 ppmU/%TOC at a depth of 0.5−2.5 m, respectively, but the general content of uranium in the studied environment was close to the values characterizing continental run-off. The results obtained for the White Sea sediments were compared with the sediment of the Black Sea, formed in the anoxic conditions of hydrogen sulfide contamination. In these conditions, the uranium content varied from 10 to 20 ppm. The obtained data were interpreted using thermodynamic modeling of the uranium forms in the seawater at different pH and Eh. This study demonstrated that the change of redox conditions from oxidizing to reducing leads to increased uranium content due to a decrease in uranium’s solubility in water. These results show that oxidation–reduction potential could be one of the most important factors controlling uranium content in black shales formed in the marine environment.

Socio-economic development scenarios of the White Sea regions.

2021 ◽  
pp. 52-69
Author(s):  
Anna E. Kurilo ◽  
◽  
Pavel V. Druzhinin ◽  
Keyword(s):  
Economic Development ◽  
Catchment Area ◽  
White Sea ◽  
The Arctic ◽  
Arctic Zone ◽  
The White Sea ◽  
Development Scenarios ◽  
Arctic Regions ◽  
Macroeconomic Indicators ◽  
Scenario Approach

In the process of creating a national system of strategic planning and within the framework of normative economics, the scenario approach provides opportunities for constructing goals and directions of socio-economic territories development. Being a planning tool the scenario approach allows forming the directions of regional development. These processes take particular relevance for the regions of our country that are the parts of the Arctic zone, especially in increased interest and attention to these territories resources from other external agents. The main aim of this paper is to elaborate development scenarios for the regions, which are fully or partially included in the Arctic zone and the White Sea catchment area. Based on the dynamics analysis of the main macroeconomic indicators and development trends for 1990–2019, the dependence of indicators for forecasting socio-environmental and economic development of these regions, was built. We applied scenario approach to describe possible development scenarios of Arctic regions in the White Sea catchment area. The novelty of the work is the construction of matrix of development scenarios of the Arctic regions, united by belonging to the White Sea catchment area. The analysis results of macroeconomic indicators for three elements of sustainable development show that the regions have rather weak economic development, stagnation of social indicators and difficult environmental situation. We outlined the problems constraining the development of Arctic regions in the White Sea catchment area and the directions to their solutions. To reach the trajectory of sustainable development is possible under condition of coordination and implementation of the measures taken by the state and regional authorities. This scenario of development strategy according to the innovation trajectory will allow to consolidate activity of federal, regional and municipal authorities of these territories. The integrated development program of the Arctic regions in the White Sea catchment area can be a coordinating platform.

Occurrence Forms of Heavy Metals in the Bottom Sediments of the White Sea

2018 ◽  
pp. 241-270 ◽  
Author(s):  
Liudmila L. Demina ◽  
Dmitry F. Budko ◽  
Alexander N. Novigatsky ◽  
Tatiana N. Alexсeeva ◽  
Anastasia I. Kochenkova
Keyword(s):  
Heavy Metals ◽  
Bottom Sediments ◽  
White Sea ◽  
The White Sea

Geochemistry of terricolous lichens in the White Sea catchment area

2013 ◽  
Vol 450 (1) ◽  
pp. 514-520 ◽  
Author(s):  
V. P. Shevchenko ◽  
O. S. Pokrovsky ◽  
D. P. Starodymova ◽  
E. V. Vasyukova ◽  
A. P. Lisitzin ◽  
...  
Keyword(s):  
Catchment Area ◽  
White Sea ◽  
The White Sea ◽  
Terricolous Lichens

Comparative analysis of the microelemental composition of seston and bottom sediments in the White Sea

2006 ◽  
Vol 406 (1) ◽  
pp. 136-140 ◽  
Author(s):  
G. A. Leonova ◽  
V. A. Bobrov ◽  
V. P. Shevchenko ◽  
A. A. Prudkovskii
Keyword(s):  
Comparative Analysis ◽  
Bottom Sediments ◽  
White Sea ◽  
The White Sea ◽  
Microelemental Composition

scholarly journals Problems of the time of foundation and the tectonic evolution of the Onega — Kandalaksha paleorift in the light of the data of isotopic geochronology

2018 ◽  
pp. 5-11
Author(s):  
A. S. Baluev ◽  
S. Yu. Kolodyazhny ◽  
E. N. Terekhov ◽  
V. A. Lebedev ◽  
P. A. Serov
Keyword(s):  
Kola Peninsula ◽  
Tectonic Evolution ◽  
White Sea ◽  
Water Area ◽  
The White Sea ◽  
Isotope Method ◽  
Isotopic Geochronology ◽  
The Baltic ◽  
Baltic Area ◽  
Different Sources

Kandalaksha graben, located in the water-area of the White sea, is a part of the Onega-Kandalaksha paleorift of the Riphean time of foundation. It is filled with the terrigenous formations of the Terskaya suites ranging from 3 to 8 km by depth, while the age of the rocks of the Terskaya suite is still controversial, and according to different sources, ranges from 1300 to 670 Ma. This means that the time of the formation of Kandalaksha Graben is not precisely defined. In 2016, on the Tersky Bank of the Kola Peninsula, a sample of sandstones of the suite was selected. The age of the rock of 1390±25 Ma, i.e. the boundary of the early and middle Riphean, was determined by the K-Ar isotope method.. This corresponds to the time of the beginning of the stretching of the lithosphere and continental rifting. Quartz-microcline metasomatites formed on sand-shale spit of Terskaya suite in the zone of amethyst deposit of Cape Korablik gave the age of 821±170 Ma, determined by Sm-Nd method, and fluorite of the same rocks gave the age of 690±71 Ma. The last value is close to the age of the basalts from the Onega depression, defined by the same method. These data correspond to the momentum of stretching of the passive Timan margin of the Baltic area at the end of the late Riphean.

BOTTOM SEDIMENTS OF LAKES AND STREAMS OF DVINA BAY OF THE WHITE SEA COASTAL AREAS AS AN INDICATOR OF ANTHROPOGENIC IMPACT (BY THE EXAMPLE OF MERCURY POLLUTION) _

2017 ◽  
Author(s):  
Boris Krasnoyarskiy ◽  
Boris Krasnoyarskiy ◽  
Asya Ovsepyan ◽  
Asya Ovsepyan ◽  
Yury Fedorov ◽  
...  
Keyword(s):  
Bottom Sediments ◽  
Anthropogenic Impact ◽  
White Sea ◽  
Mercury Content ◽  
Mercury Pollution ◽  
Scientific School ◽  
The White Sea ◽  
Subarctic Region ◽  
Low Concentrations ◽  
Surrounding Areas

The article analyzes the data of expedition studies conducted by the team of the leading scientific school of Professor Fedorov Yu.A. in the Archangelsk region for more then 10-years period of researches. The materials of mercury content obtained for samples of bottom sediments sampled in the mouth area of the Northern Dvina River, the lakes of Arkhangelsk and the surrounding areas, at Dvina Bay and different areas of the White Sea. Based on the available data and having considered the results of the authors working on the subject of mercury pollution in the subarctic region, conclusions about the level of anthropogenic impact on water bodies and streams of the Arkhangelsk region are justified. Factors that contribute to the formation of relatively high and low concentrations of mercury in sediments identified. The effects of mechanical, hydrochemical, hydrological barriers analyzed. The natural background of mercury in the bottom sediments of the region revealed. Comparative analysis of the accumulation of mercury in the bottom sediments of the study area and other parts of the subarctic region realized. Opportunities and conditions for existence of the effect of "secondary pollution" discussed.

Lithology, biostratigraphy, and geochronology of the late pleistocene-holocene sediments on the coast of Onega bay of the White sea

2019 ◽  
Vol 485 (2) ◽  
pp. 221-225
Author(s):  
V. V. Kolka ◽  
O. P. Korsakova ◽  
N. B. Lavrova ◽  
T. S. Shelekhova ◽  
N. E. Zaretskaya
Keyword(s):  
Late Pleistocene ◽  
Bottom Sediments ◽  
Radiocarbon Dating ◽  
White Sea ◽  
The White Sea ◽  
Southeastern Part ◽  
Sedimentary Sequences ◽  
Onega Bay ◽  
Holocene Sediments ◽  
Sea Coast

This paper reports on the lithological, micropaleontological, and chronometric data (radiocarbon dating) for one of the areas of the White Sea coast. The sedimentary sequences were studied in the current lake basins, which were separated from the large basin at different times. The basin was situated in the head of the current Onega Bay. On the basis of these data, the bottom sediments were stratified and the Late Pleistocene-Holocene paleogeographic settings were reconstructed for the southeastern part of Onega Bay.

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