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Micromorphological features of the fine earth and skeletal fractions of soils of West Antarctica in the areas of Russian Antarctic stations. / Abakumov, E.V.; Gagarina, E.I.; Sapega, V.F.; Vlasov, D.Y.

In: Eurasian Soil Science, Vol. 46, No. 12, 2013, p. 1219-1229.

Research output: Contribution to journal › Article

Harvard

Abakumov, EV, Gagarina, EI, Sapega, VF & Vlasov, DY 2013, 'Micromorphological features of the fine earth and skeletal fractions of soils of West Antarctica in the areas of Russian Antarctic stations', Eurasian Soil Science, vol. 46, no. 12, pp. 1219-1229. https://doi.org/10.1134/S1064229313120028

APA

Abakumov, E. V., Gagarina, E. I., Sapega, V. F., & Vlasov, D. Y. (2013). Micromorphological features of the fine earth and skeletal fractions of soils of West Antarctica in the areas of Russian Antarctic stations. Eurasian Soil Science, 46(12), 1219-1229. https://doi.org/10.1134/S1064229313120028

Vancouver

Abakumov EV, Gagarina EI, Sapega VF, Vlasov DY. Micromorphological features of the fine earth and skeletal fractions of soils of West Antarctica in the areas of Russian Antarctic stations. Eurasian Soil Science. 2013;46(12):1219-1229. https://doi.org/10.1134/S1064229313120028

Author

Abakumov, E.V. ; Gagarina, E.I. ; Sapega, V.F. ; Vlasov, D.Y. / Micromorphological features of the fine earth and skeletal fractions of soils of West Antarctica in the areas of Russian Antarctic stations. In: Eurasian Soil Science. 2013 ; Vol. 46, No. 12. pp. 1219-1229.

BibTeX

@article{0de7005d4b1b46ba88ba69e449776cbd,
title = "Micromorphological features of the fine earth and skeletal fractions of soils of West Antarctica in the areas of Russian Antarctic stations",
abstract = "Micromorphological features of the fine earth and skeletal fractions of soils of West Antarctica forming under different conditions of pedogenesis have been studied in the areas of Russian Antarctic stations. The processes of mineral weathering and alteration of rock fragments are more pronounced in the Subantarctic soils with better developed humification and immobilization of iron compounds under conditions of surface overmoistening. The biogenic accumulative processes in the soils of King George Island result in the appearance of initial forms of humic plasma that have not been detected in the Antarctic soils in the areas of the Russkaya and Leningradskaya stations. Humus films on mineral grains are present in the soils of King George Island, and organic plasmic material is present in the ornithogenic soils under penguin guano on Lindsey Island. High latitude Antarctic soils may contain surface concentrations of organic matter; rock fragments are covered by iron oxides and soluble salts. The formation of a",
keywords = "soils of West Antarctica, micromorphological features, soil processes, microprobe analysis",
author = "E.V. Abakumov and E.I. Gagarina and V.F. Sapega and D.Y. Vlasov",
year = "2013",
doi = "10.1134/S1064229313120028",
language = "English",
volume = "46",
pages = "1219--1229",
journal = "Eurasian Soil Science",
issn = "1064-2293",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "12",

}

RIS

TY - JOUR

T1 - Micromorphological features of the fine earth and skeletal fractions of soils of West Antarctica in the areas of Russian Antarctic stations

AU - Abakumov, E.V.

AU - Gagarina, E.I.

AU - Sapega, V.F.

AU - Vlasov, D.Y.

PY - 2013

Y1 - 2013

N2 - Micromorphological features of the fine earth and skeletal fractions of soils of West Antarctica forming under different conditions of pedogenesis have been studied in the areas of Russian Antarctic stations. The processes of mineral weathering and alteration of rock fragments are more pronounced in the Subantarctic soils with better developed humification and immobilization of iron compounds under conditions of surface overmoistening. The biogenic accumulative processes in the soils of King George Island result in the appearance of initial forms of humic plasma that have not been detected in the Antarctic soils in the areas of the Russkaya and Leningradskaya stations. Humus films on mineral grains are present in the soils of King George Island, and organic plasmic material is present in the ornithogenic soils under penguin guano on Lindsey Island. High latitude Antarctic soils may contain surface concentrations of organic matter; rock fragments are covered by iron oxides and soluble salts. The formation of a

AB - Micromorphological features of the fine earth and skeletal fractions of soils of West Antarctica forming under different conditions of pedogenesis have been studied in the areas of Russian Antarctic stations. The processes of mineral weathering and alteration of rock fragments are more pronounced in the Subantarctic soils with better developed humification and immobilization of iron compounds under conditions of surface overmoistening. The biogenic accumulative processes in the soils of King George Island result in the appearance of initial forms of humic plasma that have not been detected in the Antarctic soils in the areas of the Russkaya and Leningradskaya stations. Humus films on mineral grains are present in the soils of King George Island, and organic plasmic material is present in the ornithogenic soils under penguin guano on Lindsey Island. High latitude Antarctic soils may contain surface concentrations of organic matter; rock fragments are covered by iron oxides and soluble salts. The formation of a

KW - soils of West Antarctica

KW - micromorphological features

KW - soil processes

KW - microprobe analysis

U2 - 10.1134/S1064229313120028

DO - 10.1134/S1064229313120028

M3 - Article

VL - 46

SP - 1219

EP - 1229

JO - Eurasian Soil Science

JF - Eurasian Soil Science

SN - 1064-2293

IS - 12

ER -

ID: 7410555