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Organic matter in the bottom sediments of the Ob Bay : Distribution, nature, and sources. / Petrova, V. I.; Batova, G. I.; Kursheva, A. V.; Litvinenko, I. V.; Konovalov, D. A.

в: Geochemistry International, Том 48, № 2, 01.02.2010, стр. 140-151.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Petrova, VI, Batova, GI, Kursheva, AV, Litvinenko, IV & Konovalov, DA 2010, 'Organic matter in the bottom sediments of the Ob Bay: Distribution, nature, and sources', Geochemistry International, Том. 48, № 2, стр. 140-151. https://doi.org/10.1134/S0016702910020035

APA

Petrova, V. I., Batova, G. I., Kursheva, A. V., Litvinenko, I. V., & Konovalov, D. A. (2010). Organic matter in the bottom sediments of the Ob Bay: Distribution, nature, and sources. Geochemistry International, 48(2), 140-151. https://doi.org/10.1134/S0016702910020035

Vancouver

Petrova VI, Batova GI, Kursheva AV, Litvinenko IV, Konovalov DA. Organic matter in the bottom sediments of the Ob Bay: Distribution, nature, and sources. Geochemistry International. 2010 Февр. 1;48(2):140-151. https://doi.org/10.1134/S0016702910020035

Author

Petrova, V. I. ; Batova, G. I. ; Kursheva, A. V. ; Litvinenko, I. V. ; Konovalov, D. A. / Organic matter in the bottom sediments of the Ob Bay : Distribution, nature, and sources. в: Geochemistry International. 2010 ; Том 48, № 2. стр. 140-151.

BibTeX

@article{505c1fe2506c4dd7bfd99c0f5b852b2f,
title = "Organic matter in the bottom sediments of the Ob Bay: Distribution, nature, and sources",
abstract = "The lateral variability of main geochemical parameters of dispersed organic matter (DOM) in the bottoms sediments of the Ob Bay was studied using materials of areal geological survey. It was found that they correspond to background compositions of estuarine-delta facies of the Western Arctic shelf, being mainly determined by the influx of river run-off and coastal abrasion. The distribution of DOM and its components is controlled by the hydrodynamic regime of the water area and grain-size composition of sediments. The molecular composition of hydrocarbon markers (n-alkanes, cyclanes, and arenes) confirms the dominant role of terrigenous humic material in the formation of DOM of the bottom sediments, while temporal stability of quantitative and qualitative geochemical characteristics indicates the stability of the Ob Bay ecosystem.",
author = "Petrova, {V. I.} and Batova, {G. I.} and Kursheva, {A. V.} and Litvinenko, {I. V.} and Konovalov, {D. A.}",
year = "2010",
month = feb,
day = "1",
doi = "10.1134/S0016702910020035",
language = "English",
volume = "48",
pages = "140--151",
journal = "Geochemistry International",
issn = "0016-7029",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "2",

}

RIS

TY - JOUR

T1 - Organic matter in the bottom sediments of the Ob Bay

T2 - Distribution, nature, and sources

AU - Petrova, V. I.

AU - Batova, G. I.

AU - Kursheva, A. V.

AU - Litvinenko, I. V.

AU - Konovalov, D. A.

PY - 2010/2/1

Y1 - 2010/2/1

N2 - The lateral variability of main geochemical parameters of dispersed organic matter (DOM) in the bottoms sediments of the Ob Bay was studied using materials of areal geological survey. It was found that they correspond to background compositions of estuarine-delta facies of the Western Arctic shelf, being mainly determined by the influx of river run-off and coastal abrasion. The distribution of DOM and its components is controlled by the hydrodynamic regime of the water area and grain-size composition of sediments. The molecular composition of hydrocarbon markers (n-alkanes, cyclanes, and arenes) confirms the dominant role of terrigenous humic material in the formation of DOM of the bottom sediments, while temporal stability of quantitative and qualitative geochemical characteristics indicates the stability of the Ob Bay ecosystem.

AB - The lateral variability of main geochemical parameters of dispersed organic matter (DOM) in the bottoms sediments of the Ob Bay was studied using materials of areal geological survey. It was found that they correspond to background compositions of estuarine-delta facies of the Western Arctic shelf, being mainly determined by the influx of river run-off and coastal abrasion. The distribution of DOM and its components is controlled by the hydrodynamic regime of the water area and grain-size composition of sediments. The molecular composition of hydrocarbon markers (n-alkanes, cyclanes, and arenes) confirms the dominant role of terrigenous humic material in the formation of DOM of the bottom sediments, while temporal stability of quantitative and qualitative geochemical characteristics indicates the stability of the Ob Bay ecosystem.

UR - http://www.scopus.com/inward/record.url?scp=77951951004&partnerID=8YFLogxK

U2 - 10.1134/S0016702910020035

DO - 10.1134/S0016702910020035

M3 - Article

AN - SCOPUS:77951951004

VL - 48

SP - 140

EP - 151

JO - Geochemistry International

JF - Geochemistry International

SN - 0016-7029

IS - 2

ER -

ID: 47855563