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Pedogenic and lithogenic features in the mineralogical composition of chernozem developed from red-earth deposits. / Lesovaya, S. N.; Kapichka, A.; Petrovskii, E.; Aparin, B. F.

в: Eurasian Soil Science, Том 36, № 12, 01.12.2003, стр. 1325-1333.

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

Harvard

Lesovaya, SN, Kapichka, A, Petrovskii, E & Aparin, BF 2003, 'Pedogenic and lithogenic features in the mineralogical composition of chernozem developed from red-earth deposits', Eurasian Soil Science, Том. 36, № 12, стр. 1325-1333.

APA

Lesovaya, S. N., Kapichka, A., Petrovskii, E., & Aparin, B. F. (2003). Pedogenic and lithogenic features in the mineralogical composition of chernozem developed from red-earth deposits. Eurasian Soil Science, 36(12), 1325-1333.

Vancouver

Lesovaya SN, Kapichka A, Petrovskii E, Aparin BF. Pedogenic and lithogenic features in the mineralogical composition of chernozem developed from red-earth deposits. Eurasian Soil Science. 2003 Дек. 1;36(12):1325-1333.

Author

Lesovaya, S. N. ; Kapichka, A. ; Petrovskii, E. ; Aparin, B. F. / Pedogenic and lithogenic features in the mineralogical composition of chernozem developed from red-earth deposits. в: Eurasian Soil Science. 2003 ; Том 36, № 12. стр. 1325-1333.

BibTeX

@article{06f73814079f40d8b2a7d6d1cd692689,
title = "Pedogenic and lithogenic features in the mineralogical composition of chernozem developed from red-earth deposits",
abstract = "Specific features of the mineralogical composition of phyllosilicates and iron oxides in a mountainous chernozem developed from red-earth calcareous deposits in the North Caucasus are analyzed. This soil is characterized by a vividly manifested set of features inherited from the parent rock. An association of clay minerals with the predominance of hydromica is identified in the clay fraction. Mineral forms of iron in the clay fraction are represented by hematite and magnetite diagnosed by the method of M{\"o}ssbauer spectroscopy and thermomagnetic measurements. A decrease in the intensity of basal reflections from plane (001) and an increase in the intensity of basal reflections from plane (020) in the upper soil horizons are conditioned by the weathering of hydromica accompanied by some disordering of its crystalline lattice. The disordering of the crystalline lattice of hematite also takes place in the clay fraction from upper soil horizons.",
author = "Lesovaya, {S. N.} and A. Kapichka and E. Petrovskii and Aparin, {B. F.}",
year = "2003",
month = dec,
day = "1",
language = "English",
volume = "36",
pages = "1325--1333",
journal = "Eurasian Soil Science",
issn = "1064-2293",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "12",

}

RIS

TY - JOUR

T1 - Pedogenic and lithogenic features in the mineralogical composition of chernozem developed from red-earth deposits

AU - Lesovaya, S. N.

AU - Kapichka, A.

AU - Petrovskii, E.

AU - Aparin, B. F.

PY - 2003/12/1

Y1 - 2003/12/1

N2 - Specific features of the mineralogical composition of phyllosilicates and iron oxides in a mountainous chernozem developed from red-earth calcareous deposits in the North Caucasus are analyzed. This soil is characterized by a vividly manifested set of features inherited from the parent rock. An association of clay minerals with the predominance of hydromica is identified in the clay fraction. Mineral forms of iron in the clay fraction are represented by hematite and magnetite diagnosed by the method of Mössbauer spectroscopy and thermomagnetic measurements. A decrease in the intensity of basal reflections from plane (001) and an increase in the intensity of basal reflections from plane (020) in the upper soil horizons are conditioned by the weathering of hydromica accompanied by some disordering of its crystalline lattice. The disordering of the crystalline lattice of hematite also takes place in the clay fraction from upper soil horizons.

AB - Specific features of the mineralogical composition of phyllosilicates and iron oxides in a mountainous chernozem developed from red-earth calcareous deposits in the North Caucasus are analyzed. This soil is characterized by a vividly manifested set of features inherited from the parent rock. An association of clay minerals with the predominance of hydromica is identified in the clay fraction. Mineral forms of iron in the clay fraction are represented by hematite and magnetite diagnosed by the method of Mössbauer spectroscopy and thermomagnetic measurements. A decrease in the intensity of basal reflections from plane (001) and an increase in the intensity of basal reflections from plane (020) in the upper soil horizons are conditioned by the weathering of hydromica accompanied by some disordering of its crystalline lattice. The disordering of the crystalline lattice of hematite also takes place in the clay fraction from upper soil horizons.

UR - http://www.scopus.com/inward/record.url?scp=9144247759&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:9144247759

VL - 36

SP - 1325

EP - 1333

JO - Eurasian Soil Science

JF - Eurasian Soil Science

SN - 1064-2293

IS - 12

ER -

ID: 49131524