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Mineralogy of parent rock and peaty-podzolic soil of Iremel Ridge, Southern Urals. / Khalitov, R. M.; Perova, E. N.; Abakumov, E. V.; Suleimanov, R. R.

In: Eurasian Soil Science, Vol. 50, No. 8, 01.08.2017, p. 961-970.

Research output: Contribution to journal › Article › peer-review

Harvard

Khalitov, RM, Perova, EN, Abakumov, EV & Suleimanov, RR 2017, 'Mineralogy of parent rock and peaty-podzolic soil of Iremel Ridge, Southern Urals', Eurasian Soil Science, vol. 50, no. 8, pp. 961-970. https://doi.org/10.1134/S1064229317080063

APA

Khalitov, R. M., Perova, E. N., Abakumov, E. V., & Suleimanov, R. R. (2017). Mineralogy of parent rock and peaty-podzolic soil of Iremel Ridge, Southern Urals. Eurasian Soil Science, 50(8), 961-970. https://doi.org/10.1134/S1064229317080063

Vancouver

Khalitov RM, Perova EN, Abakumov EV, Suleimanov RR. Mineralogy of parent rock and peaty-podzolic soil of Iremel Ridge, Southern Urals. Eurasian Soil Science. 2017 Aug 1;50(8):961-970. https://doi.org/10.1134/S1064229317080063

Author

Khalitov, R. M. ; Perova, E. N. ; Abakumov, E. V. ; Suleimanov, R. R. / Mineralogy of parent rock and peaty-podzolic soil of Iremel Ridge, Southern Urals. In: Eurasian Soil Science. 2017 ; Vol. 50, No. 8. pp. 961-970.

BibTeX

@article{52068981353141c78e2d46086862090d,
title = "Mineralogy of parent rock and peaty-podzolic soil of Iremel Ridge, Southern Urals",
abstract = "The mineralogy of soils and parent rocks of the Iremel Ridge has been studied by the methods of micromorphology, laser diffraction, computed X-ray microtomography, and X-ray fluorescence analysis. In hard rock and soil, the major minerals have been identified: quartz, illite, and a chlorite-group mineral (Fe analogue of sudoite), as well as accessory minerals: monazite, xenotime, rutile, zircon, and florencite. It has been found that chlorite, illite, and quartz are present in all horizons of the studied peaty-podzolic soil. Insignificant amounts of mixed-layered mineral and kaolinite could be suggested in the T and EL horizons of peaty-podzolic soil. The mixed-layered mineral is most probably of soil origin, which is related to the transformation of illites inherited from the parent rock under acidic conditions.",
keywords = "clay minerals, Histic Retisol, soil mineralogy and micromorphology",
author = "Khalitov, {R. M.} and Perova, {E. N.} and Abakumov, {E. V.} and Suleimanov, {R. R.}",
year = "2017",
month = aug,
day = "1",
doi = "10.1134/S1064229317080063",
language = "English",
volume = "50",
pages = "961--970",
journal = "Eurasian Soil Science",
issn = "1064-2293",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "8",

}

RIS

TY - JOUR

T1 - Mineralogy of parent rock and peaty-podzolic soil of Iremel Ridge, Southern Urals

AU - Khalitov, R. M.

AU - Perova, E. N.

AU - Abakumov, E. V.

AU - Suleimanov, R. R.

PY - 2017/8/1

Y1 - 2017/8/1

N2 - The mineralogy of soils and parent rocks of the Iremel Ridge has been studied by the methods of micromorphology, laser diffraction, computed X-ray microtomography, and X-ray fluorescence analysis. In hard rock and soil, the major minerals have been identified: quartz, illite, and a chlorite-group mineral (Fe analogue of sudoite), as well as accessory minerals: monazite, xenotime, rutile, zircon, and florencite. It has been found that chlorite, illite, and quartz are present in all horizons of the studied peaty-podzolic soil. Insignificant amounts of mixed-layered mineral and kaolinite could be suggested in the T and EL horizons of peaty-podzolic soil. The mixed-layered mineral is most probably of soil origin, which is related to the transformation of illites inherited from the parent rock under acidic conditions.

AB - The mineralogy of soils and parent rocks of the Iremel Ridge has been studied by the methods of micromorphology, laser diffraction, computed X-ray microtomography, and X-ray fluorescence analysis. In hard rock and soil, the major minerals have been identified: quartz, illite, and a chlorite-group mineral (Fe analogue of sudoite), as well as accessory minerals: monazite, xenotime, rutile, zircon, and florencite. It has been found that chlorite, illite, and quartz are present in all horizons of the studied peaty-podzolic soil. Insignificant amounts of mixed-layered mineral and kaolinite could be suggested in the T and EL horizons of peaty-podzolic soil. The mixed-layered mineral is most probably of soil origin, which is related to the transformation of illites inherited from the parent rock under acidic conditions.

KW - clay minerals

KW - Histic Retisol

KW - soil mineralogy and micromorphology

UR - http://www.scopus.com/inward/record.url?scp=85028083227&partnerID=8YFLogxK

U2 - 10.1134/S1064229317080063

DO - 10.1134/S1064229317080063

M3 - Article

AN - SCOPUS:85028083227

VL - 50

SP - 961

EP - 970

JO - Eurasian Soil Science

JF - Eurasian Soil Science

SN - 1064-2293

IS - 8

ER -

ID: 9156847