Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
The spatio-temporal distribution of elements in the bottom sediments of Lake Onego and small lakes located on the catchment area of Onego Ice Lake. / Strakhovenko, Vera D.; Belkina, Natalia A.; Efremenko, Natalia A. и др.
в: Vestnik of Saint Petersburg University. Earth Sciences, Том 68, № 4, 2023.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - The spatio-temporal distribution of elements in the bottom sediments of Lake Onego and small lakes located on the catchment area of Onego Ice Lake
AU - Strakhovenko, Vera D.
AU - Belkina, Natalia A.
AU - Efremenko, Natalia A.
AU - Potakhin, Maxim S.
AU - Subetto, Dmitry A.
AU - Malov, Viktor I.
AU - Ovdina, Ekaterina A.
N1 - The research was supported by the RFBR project No. 19-05-50014 (study of mineral and geochemical composition of sedimentary material and bottom sediments) and was done on state assignment of IGM SB RAS (№ 122041400193-7) (estimation the rates of modern sedimentation by the activity of137Cs and 210Pb), state assignment to the HSPU of Russia No. VRFY-2023-0010 of the Ministry of Education of the Russian Federation state assignment to the NWPI KarRC RAS No. 0185-2021-0006 (fieldwork on the bottom sediments sampling and the study of their composition). Публикация для корректировки.
PY - 2023
Y1 - 2023
N2 - The work presents the results of a comprehensive mineralogical and geochemical study of Late Pleistocene-Holocene bottom sediments of Lake Onego and small lakes located in the territory belonging to Onego Ice Lake. Methods of ICP-MS, atomic absorption spectrometry, X-ray fluorescence analysis, X-ray phase method (XRD), scanning electron microscopy (SEM), and gamma-spectrometric method were used. The geochemical composition of the terrigenous fraction reflects the mineral composition and is permanent for the all bottom sediments cores of Lake Onego and small lakes during time interval about 12,000 years. For the first time, detailed mineralogical studies of sediments have shown that the composition of mineral associations of the terrigenous fraction is similar in the bottom sediment cores of Lake Onego and small lakes. The association of authigenic minerals in bottom sediments is distinguished by the presence of pyrite framboids in small lakes, and crystalline aggregates of Fe-phosphate, ferruginous illites and chlorites in Lake Onego. Sedimentation rates established by the study of correlations the indicator technogenic radioisotope 137Cs and atmospheric 210Pb. In the bottom sediments of small lakes, sedimentation rates vary from lake to lake, as well as in various areas of Lake Onego in the range from 0.05 cm/year to 0.30 cm/year.
AB - The work presents the results of a comprehensive mineralogical and geochemical study of Late Pleistocene-Holocene bottom sediments of Lake Onego and small lakes located in the territory belonging to Onego Ice Lake. Methods of ICP-MS, atomic absorption spectrometry, X-ray fluorescence analysis, X-ray phase method (XRD), scanning electron microscopy (SEM), and gamma-spectrometric method were used. The geochemical composition of the terrigenous fraction reflects the mineral composition and is permanent for the all bottom sediments cores of Lake Onego and small lakes during time interval about 12,000 years. For the first time, detailed mineralogical studies of sediments have shown that the composition of mineral associations of the terrigenous fraction is similar in the bottom sediment cores of Lake Onego and small lakes. The association of authigenic minerals in bottom sediments is distinguished by the presence of pyrite framboids in small lakes, and crystalline aggregates of Fe-phosphate, ferruginous illites and chlorites in Lake Onego. Sedimentation rates established by the study of correlations the indicator technogenic radioisotope 137Cs and atmospheric 210Pb. In the bottom sediments of small lakes, sedimentation rates vary from lake to lake, as well as in various areas of Lake Onego in the range from 0.05 cm/year to 0.30 cm/year.
KW - 137Cs
KW - 210Pb
KW - Lake Onego
KW - Onego Ice Lake
KW - bottom sediments
KW - geochemistry
KW - mineralogy
KW - sedimentation rate
KW - small lakes
UR - https://www.scopus.com/record/display.uri?eid=2-s2.0-85179938349&origin=inward&txGid=df0dc12cd57cbf9124ea9815839d7abe
UR - https://www.mendeley.com/catalogue/f135752d-3f75-3911-8288-337eb886eee0/
U2 - 10.21638/spbu07.2023.404
DO - 10.21638/spbu07.2023.404
M3 - Article
VL - 68
JO - Vestnik of Saint Petersburg University. Earth Sciences
JF - Vestnik of Saint Petersburg University. Earth Sciences
SN - 2541-9668
IS - 4
ER -
ID: 59773117