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Genesis of the silty sands and loams within the periglacial zone in the center of the Russian Plain and the properties of soils developed from them. / Rusakov, A. V.; Kerzum, P. P.; Matinyan, N. N.

в: Eurasian Soil Science, Том 41, № 4, 2008, стр. 347-362.

Результаты исследований: Научные публикации в периодических изданиях › статья

Harvard

Rusakov, AV, Kerzum, PP & Matinyan, NN 2008, 'Genesis of the silty sands and loams within the periglacial zone in the center of the Russian Plain and the properties of soils developed from them', Eurasian Soil Science, Том. 41, № 4, стр. 347-362. https://doi.org/10.1134/S1064229308040017

APA

Rusakov, A. V., Kerzum, P. P., & Matinyan, N. N. (2008). Genesis of the silty sands and loams within the periglacial zone in the center of the Russian Plain and the properties of soils developed from them. Eurasian Soil Science, 41(4), 347-362. https://doi.org/10.1134/S1064229308040017

Vancouver

Rusakov AV, Kerzum PP, Matinyan NN. Genesis of the silty sands and loams within the periglacial zone in the center of the Russian Plain and the properties of soils developed from them. Eurasian Soil Science. 2008;41(4):347-362. https://doi.org/10.1134/S1064229308040017

Author

Rusakov, A. V. ; Kerzum, P. P. ; Matinyan, N. N. / Genesis of the silty sands and loams within the periglacial zone in the center of the Russian Plain and the properties of soils developed from them. в: Eurasian Soil Science. 2008 ; Том 41, № 4. стр. 347-362.

BibTeX

@article{f9fa537287484ed48a6215113c98d191,
title = "Genesis of the silty sands and loams within the periglacial zone in the center of the Russian Plain and the properties of soils developed from them",
abstract = "The genesis and spatial differentiation of the silty sands and loams deposited during the Late Valdai glaciation have been studied in the central part of the Russian Plain within the Mologa-Sheksna Lowland and on terraced slopes of the Ovinishchensk Upland (Yaroslavl oblast). The stratigraphy of these sediments on different elements of the local topography and data on their particle-size distribution suggest that they belong to the same paragenetic group. Some differences in the particle-size distribution can be explained by the specificity of sedimentation in periglacial lakes found at different geomorphic levels (from 102 to 180 m a.s.l.) during the Ostashkov phase of the Valdai glaciation. For the first time, statistically significant differences in the properties of Holocene soils developed at different hypsometric levels have been revealed. The degree of textural differentiation of the soils developed from silty loams increases with an increase in the absolute height of the surface. The analysis of factu",
author = "Rusakov, {A. V.} and Kerzum, {P. P.} and Matinyan, {N. N.}",
year = "2008",
doi = "10.1134/S1064229308040017",
language = "English",
volume = "41",
pages = "347--362",
journal = "Eurasian Soil Science",
issn = "1064-2293",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "4",

}

RIS

TY - JOUR

T1 - Genesis of the silty sands and loams within the periglacial zone in the center of the Russian Plain and the properties of soils developed from them

AU - Rusakov, A. V.

AU - Kerzum, P. P.

AU - Matinyan, N. N.

PY - 2008

Y1 - 2008

N2 - The genesis and spatial differentiation of the silty sands and loams deposited during the Late Valdai glaciation have been studied in the central part of the Russian Plain within the Mologa-Sheksna Lowland and on terraced slopes of the Ovinishchensk Upland (Yaroslavl oblast). The stratigraphy of these sediments on different elements of the local topography and data on their particle-size distribution suggest that they belong to the same paragenetic group. Some differences in the particle-size distribution can be explained by the specificity of sedimentation in periglacial lakes found at different geomorphic levels (from 102 to 180 m a.s.l.) during the Ostashkov phase of the Valdai glaciation. For the first time, statistically significant differences in the properties of Holocene soils developed at different hypsometric levels have been revealed. The degree of textural differentiation of the soils developed from silty loams increases with an increase in the absolute height of the surface. The analysis of factu

AB - The genesis and spatial differentiation of the silty sands and loams deposited during the Late Valdai glaciation have been studied in the central part of the Russian Plain within the Mologa-Sheksna Lowland and on terraced slopes of the Ovinishchensk Upland (Yaroslavl oblast). The stratigraphy of these sediments on different elements of the local topography and data on their particle-size distribution suggest that they belong to the same paragenetic group. Some differences in the particle-size distribution can be explained by the specificity of sedimentation in periglacial lakes found at different geomorphic levels (from 102 to 180 m a.s.l.) during the Ostashkov phase of the Valdai glaciation. For the first time, statistically significant differences in the properties of Holocene soils developed at different hypsometric levels have been revealed. The degree of textural differentiation of the soils developed from silty loams increases with an increase in the absolute height of the surface. The analysis of factu

U2 - 10.1134/S1064229308040017

DO - 10.1134/S1064229308040017

M3 - Article

VL - 41

SP - 347

EP - 362

JO - Eurasian Soil Science

JF - Eurasian Soil Science

SN - 1064-2293

IS - 4

ER -

ID: 5030191