On the Specifics of Formation of the Qualitative Characteristics of Waters and Sediments in the Lena River Delta

The paper considers the qualitative characteristics (chemical composition of waters and sediments, biological diversity) of the Lena runoff and their transformation as a result of the biogeochemical pro-cesses taking place in the delta region. The hydrological, hydrochemical, geochemical (chemical c...

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Main Authors: A.A. Chetverova, I.V. Fedorova, L.A. Frolova, G.R. Nigamatzyanova, T.V. Skorospekhova, A.A. Shadrina
Format: Article
Language:English
Published: Kazan Federal University 2017-03-01
Series:Учёные записки Казанского университета: Серия Естественные науки
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Online Access:http://kpfu.ru/portal/docs/F1704924437/159_1_est_8.pdf
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author A.A. Chetverova
I.V. Fedorova
L.A. Frolova
G.R. Nigamatzyanova
T.V. Skorospekhova
A.A. Shadrina
author_facet A.A. Chetverova
I.V. Fedorova
L.A. Frolova
G.R. Nigamatzyanova
T.V. Skorospekhova
A.A. Shadrina
author_sort A.A. Chetverova
collection DOAJ
description The paper considers the qualitative characteristics (chemical composition of waters and sediments, biological diversity) of the Lena runoff and their transformation as a result of the biogeochemical pro-cesses taking place in the delta region. The hydrological, hydrochemical, geochemical (chemical com-position of river sediments), and hydrobiological description of the delta branches at the current stage has been provided. The Lena delta branches are characterized by a wide variety of water discharge values and hydro-dynamic conditions. It has been revealed that the hydrochemical composition of the delta is specific due to the dominance of hydrocarbonates and calcium ions, pH 6.9–7.9, high oxygen saturation conditions (more than 100 % sat.) throughout the water column because of wind activity, high concentrations of dissolved silica (1.1–2.7 mg/L) and iron (0.01–0.07 mg/L) if compared to the world’s mean values in natural freshwater bodies, and low concentrations of trace elements (mainly below the detection limits). The concentrations of nitrates and phosphates have been estimated in the range of 2.6–34.7 µg/L and 3.1–26.2 µg/L, respectively. The bottom and suspended sediments have been assigned to the siliceous type (Si/Al varies from 4.2 to 18 µg/L). The results of the analysis of hydrodynamic conditions, hydrobiological features, geochemical indi-ces, as well as data of the statistical factor analysis, have shown chemical elements redistribution dependencies. Several factors determining the chemical composition of water and sediments in the Lena River delta have been distinguished. The interpretation of these factors reflects the influence of river catchment area, cryogenic processes in the river delta, and biogeochemical processes. Based on the modern multidisciplinary research performed in the Lena delta, it has been demon-strated that processes leading to an inhomogeneous distribution of chemical elements between water (dissolved fraction), suspended matter, and bottom sediments occur in the delta of the river.
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institution Kabale University
issn 2542-064X
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language English
publishDate 2017-03-01
publisher Kazan Federal University
record_format Article
series Учёные записки Казанского университета: Серия Естественные науки
spelling doaj-art-e5c9f7e451304324ba54c67e2dc33fd82024-12-02T05:56:43ZengKazan Federal UniversityУчёные записки Казанского университета: Серия Естественные науки2542-064X2500-218X2017-03-011591122138On the Specifics of Formation of the Qualitative Characteristics of Waters and Sediments in the Lena River DeltaA.A. Chetverova0I.V. Fedorova1L.A. Frolova2G.R. Nigamatzyanova3T.V. Skorospekhova4A.A. Shadrina5St. Petersburg State University, St. Petersburg, 199034 Russia; Arctic and Antarctic Research Institute, St. Petersburg, 199397 RussiaArctic and Antarctic Research Institute, St. Petersburg, 199397 Russia; St. Petersburg State University, St. Petersburg, 199034 RussiaKazan Federal University, Kazan, 420008 RussiaKazan Federal University, Kazan, 420008 RussiaArctic and Antarctic Research Institute, St. Petersburg, 199397 RussiaSt. Petersburg State University, St. Petersburg, 199034 RussiaThe paper considers the qualitative characteristics (chemical composition of waters and sediments, biological diversity) of the Lena runoff and their transformation as a result of the biogeochemical pro-cesses taking place in the delta region. The hydrological, hydrochemical, geochemical (chemical com-position of river sediments), and hydrobiological description of the delta branches at the current stage has been provided. The Lena delta branches are characterized by a wide variety of water discharge values and hydro-dynamic conditions. It has been revealed that the hydrochemical composition of the delta is specific due to the dominance of hydrocarbonates and calcium ions, pH 6.9–7.9, high oxygen saturation conditions (more than 100 % sat.) throughout the water column because of wind activity, high concentrations of dissolved silica (1.1–2.7 mg/L) and iron (0.01–0.07 mg/L) if compared to the world’s mean values in natural freshwater bodies, and low concentrations of trace elements (mainly below the detection limits). The concentrations of nitrates and phosphates have been estimated in the range of 2.6–34.7 µg/L and 3.1–26.2 µg/L, respectively. The bottom and suspended sediments have been assigned to the siliceous type (Si/Al varies from 4.2 to 18 µg/L). The results of the analysis of hydrodynamic conditions, hydrobiological features, geochemical indi-ces, as well as data of the statistical factor analysis, have shown chemical elements redistribution dependencies. Several factors determining the chemical composition of water and sediments in the Lena River delta have been distinguished. The interpretation of these factors reflects the influence of river catchment area, cryogenic processes in the river delta, and biogeochemical processes. Based on the modern multidisciplinary research performed in the Lena delta, it has been demon-strated that processes leading to an inhomogeneous distribution of chemical elements between water (dissolved fraction), suspended matter, and bottom sediments occur in the delta of the river.http://kpfu.ru/portal/docs/F1704924437/159_1_est_8.pdfLena River deltahydrologyhydrochemistrygeochemistry of river sedimentshydrobiologyzooplankton
spellingShingle A.A. Chetverova
I.V. Fedorova
L.A. Frolova
G.R. Nigamatzyanova
T.V. Skorospekhova
A.A. Shadrina
On the Specifics of Formation of the Qualitative Characteristics of Waters and Sediments in the Lena River Delta
Учёные записки Казанского университета: Серия Естественные науки
Lena River delta
hydrology
hydrochemistry
geochemistry of river sediments
hydrobiology
zooplankton
title On the Specifics of Formation of the Qualitative Characteristics of Waters and Sediments in the Lena River Delta
title_full On the Specifics of Formation of the Qualitative Characteristics of Waters and Sediments in the Lena River Delta
title_fullStr On the Specifics of Formation of the Qualitative Characteristics of Waters and Sediments in the Lena River Delta
title_full_unstemmed On the Specifics of Formation of the Qualitative Characteristics of Waters and Sediments in the Lena River Delta
title_short On the Specifics of Formation of the Qualitative Characteristics of Waters and Sediments in the Lena River Delta
title_sort on the specifics of formation of the qualitative characteristics of waters and sediments in the lena river delta
topic Lena River delta
hydrology
hydrochemistry
geochemistry of river sediments
hydrobiology
zooplankton
url http://kpfu.ru/portal/docs/F1704924437/159_1_est_8.pdf
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