Characteristic features of the dynamics of carbonate parameters in the eastern part of the Laptev Sea; Oceanology; Vol. 55, iss. 1

Bibliografske podrobnosti
Parent link:Oceanology
Vol. 55, iss. 1.— 2015.— [P. 68-81]
Glavni avtor: Pipko I. I. Irina Ivanovna
Korporativna značnica: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра геологии и разведки полезных ископаемых (ГРПИ)
Drugi avtorji: Pugach S. P. Svetlana Petrovna, Semiletov I. P. Igor Petrovich
Izvleček:Title screen
This report presents the results of studies of the sea water carbonate system performed in September 2011 at the inner, middle, and outer shelf of the east of the Laptev Sea. It was shown that the key factor controlling the carbonate chemistry of the shelf waters during the warm season is the significant terrigenous runoff. In the autumn season, the surface waters of the inner and middle shelf of the eastern part of the Laptev Sea are a source of carbon dioxide to the atmosphere; those of the outer shelf act as a sink of atmospheric CO2. It is found that the waters of the inner shelf of the east of the Laptev Sea over the entire water column are now corrosive against calcium carbonate. The surface and near-bottom waters of the middle shelf are also undersaturated with respect to aragonite. It was shown that the main factors determining the undersaturation are the significant volume of freshwaters supplied with the riverine runoff and the ice melting, as well as the large amount of labile allochthonous organic matter involved into the modern biogeochemical cycle at the shelf. The performed studies showed that the shelf waters of the eastern part of the Laptev Sea constitute one of the most corrosive zones with respect to calcium carbonate in the World Ocean.
Режим доступа: по договору с организацией-держателем ресурса
Jezik:angleščina
Izdano: 2015
Teme:
Online dostop:http://dx.doi.org/10.1134/S0001437015010142
Format: Elektronski Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=640311

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200 1 |a Characteristic features of the dynamics of carbonate parameters in the eastern part of the Laptev Sea  |d Характерные особенности динамики карбонатных параметров вод восточной части моря Лаптевых  |f I. I. Pipko, S. P. Pugach, I. P. Semiletov 
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320 |a [References: p. 81 (50 tit.)] 
330 |a This report presents the results of studies of the sea water carbonate system performed in September 2011 at the inner, middle, and outer shelf of the east of the Laptev Sea. It was shown that the key factor controlling the carbonate chemistry of the shelf waters during the warm season is the significant terrigenous runoff. In the autumn season, the surface waters of the inner and middle shelf of the eastern part of the Laptev Sea are a source of carbon dioxide to the atmosphere; those of the outer shelf act as a sink of atmospheric CO2. It is found that the waters of the inner shelf of the east of the Laptev Sea over the entire water column are now corrosive against calcium carbonate. The surface and near-bottom waters of the middle shelf are also undersaturated with respect to aragonite. It was shown that the main factors determining the undersaturation are the significant volume of freshwaters supplied with the riverine runoff and the ice melting, as well as the large amount of labile allochthonous organic matter involved into the modern biogeochemical cycle at the shelf. The performed studies showed that the shelf waters of the eastern part of the Laptev Sea constitute one of the most corrosive zones with respect to calcium carbonate in the World Ocean. 
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463 |t Vol. 55, iss. 1  |v [P. 68-81]  |d 2015 
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