Chemical composition of particulate matter and element fluxes in the eastern Norwegian Sea, NS Komsomolets wreck site area

This paper reports results of a geochemical study of suspended particulate matter and particle fluxes in the Norwegian Sea above the Bear Island slope. Concentrations of suspended particles and the main components of suspended matter were determined in the euphotic, intermediate (clean water), and b...

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Bibliographic Details
Main Author: Lukashin, Vyacheslav N
Format: Dataset
Language:English
Published: PANGAEA 2008
Subjects:
Akademik Mstislav Keldysh
AMK24
AMK24-2497
AMK24-2498
AMK31
AMK31-3087
AMK31-3088
AMK31-3099
AMK33
AMK33-3236
AMK33-3237
AMK33-3237TR
AMK33-3238
AMK36
AMK36-3501
AMK36-3502
AMK36-3518
AMK36-3521
AMK36-3522
AMK36-3525
AMK36-3529
AMK36-3532
Archive of Ocean Data
ARCOD
Bottle
Niskin 30-L
Komsomolets
NIS_30L
Norwegian Sea
Trap
sediment
TRAPS
Bear Island
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.725824
https://doi.org/10.1594/PANGAEA.725824
Description
Summary:This paper reports results of a geochemical study of suspended particulate matter and particle fluxes in the Norwegian Sea above the Bear Island slope. Concentrations of suspended particles and the main components of suspended matter were determined in the euphotic, intermediate (clean water), and bottom nepheloid layers. It was shown that biogenic components are predominant in water above the nepheloid layer, whereas suspended matter of the nepheloid layer is formed by resuspension of lithogenic components of bottom sediments. Chemical compositions of suspended matter and material collected in sediment traps are identical.

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