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Uranium as a possible criterion for the hydro-chemical alteration of betafite. / Hosseinpour Khanmiri , M.; Янсон, Светлана Юрьевна; Fomin, E.V.; Titov, A. V.; Гребенюк, Андрей Владимирович; Полеховский, Юрий Степанович; Bogdanov, R. V.

в: Physics and Chemistry of Minerals, Том 45, № 6, 01.06.2018, стр. 549-562.

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

Harvard

Hosseinpour Khanmiri , M, Янсон, СЮ, Fomin, EV, Titov, AV, Гребенюк, АВ, Полеховский, ЮС & Bogdanov, RV 2018, 'Uranium as a possible criterion for the hydro-chemical alteration of betafite.', Physics and Chemistry of Minerals, Том. 45, № 6, стр. 549-562. https://doi.org/10.1007/s00269-018-0941-6

APA

Hosseinpour Khanmiri , M., Янсон, С. Ю., Fomin, E. V., Titov, A. V., Гребенюк, А. В., Полеховский, Ю. С., & Bogdanov, R. V. (2018). Uranium as a possible criterion for the hydro-chemical alteration of betafite. Physics and Chemistry of Minerals, 45(6), 549-562. https://doi.org/10.1007/s00269-018-0941-6

Vancouver

Hosseinpour Khanmiri M, Янсон СЮ, Fomin EV, Titov AV, Гребенюк АВ, Полеховский ЮС и пр. Uranium as a possible criterion for the hydro-chemical alteration of betafite. Physics and Chemistry of Minerals. 2018 Июнь 1;45(6):549-562. https://doi.org/10.1007/s00269-018-0941-6

Author

Hosseinpour Khanmiri , M. ; Янсон, Светлана Юрьевна ; Fomin, E.V. ; Titov, A. V. ; Гребенюк, Андрей Владимирович ; Полеховский, Юрий Степанович ; Bogdanov, R. V. / Uranium as a possible criterion for the hydro-chemical alteration of betafite. в: Physics and Chemistry of Minerals. 2018 ; Том 45, № 6. стр. 549-562.

BibTeX

@article{f29c1a852ba34f49aa907fd62c48a1fd,
title = "Uranium as a possible criterion for the hydro-chemical alteration of betafite.",
abstract = "Hydro-chemical processes significantly alter the original composition of metamict minerals. In the work presented here, an attempt was made to reconstruct the chemical composition of betafite in the earlier stages of its geological history. The time scale is determined by the leaching rate of the isotope 238U, a process that takes its course in line with first-order kinetics, or something close to it. The leaching rate constant of this uranium isotope was assessed. Based on available data in the literature, the hydro-chemical behavior of various atoms in group A of betafite was analyzed. The chemical composition of the mineral was calculated taking into account the total charge of the cations that the betafite had at the time it was formed, or possibly the last time it was completely reformed as a result of diverse endogenic processes. ",
keywords = "Calculations of mineral formula, Chemical shift of X-ray Lα - line, Chemical weathering, Half-leaching time, Leaching kinetic, Metamict minerals, Redox-state of uranium",
author = "{Hosseinpour Khanmiri}, M. and Янсон, {Светлана Юрьевна} and E.V. Fomin and Titov, {A. V.} and Гребенюк, {Андрей Владимирович} and Полеховский, {Юрий Степанович} and Bogdanov, {R. V.}",
year = "2018",
month = jun,
day = "1",
doi = "10.1007/s00269-018-0941-6",
language = "English",
volume = "45",
pages = "549--562",
journal = "Physics and Chemistry of Minerals",
issn = "0342-1791",
publisher = "Springer Nature",
number = "6",

}

RIS

TY - JOUR

T1 - Uranium as a possible criterion for the hydro-chemical alteration of betafite.

AU - Hosseinpour Khanmiri , M.

AU - Янсон, Светлана Юрьевна

AU - Fomin, E.V.

AU - Titov, A. V.

AU - Гребенюк, Андрей Владимирович

AU - Полеховский, Юрий Степанович

AU - Bogdanov, R. V.

PY - 2018/6/1

Y1 - 2018/6/1

N2 - Hydro-chemical processes significantly alter the original composition of metamict minerals. In the work presented here, an attempt was made to reconstruct the chemical composition of betafite in the earlier stages of its geological history. The time scale is determined by the leaching rate of the isotope 238U, a process that takes its course in line with first-order kinetics, or something close to it. The leaching rate constant of this uranium isotope was assessed. Based on available data in the literature, the hydro-chemical behavior of various atoms in group A of betafite was analyzed. The chemical composition of the mineral was calculated taking into account the total charge of the cations that the betafite had at the time it was formed, or possibly the last time it was completely reformed as a result of diverse endogenic processes.

AB - Hydro-chemical processes significantly alter the original composition of metamict minerals. In the work presented here, an attempt was made to reconstruct the chemical composition of betafite in the earlier stages of its geological history. The time scale is determined by the leaching rate of the isotope 238U, a process that takes its course in line with first-order kinetics, or something close to it. The leaching rate constant of this uranium isotope was assessed. Based on available data in the literature, the hydro-chemical behavior of various atoms in group A of betafite was analyzed. The chemical composition of the mineral was calculated taking into account the total charge of the cations that the betafite had at the time it was formed, or possibly the last time it was completely reformed as a result of diverse endogenic processes.

KW - Calculations of mineral formula

KW - Chemical shift of X-ray Lα - line

KW - Chemical weathering

KW - Half-leaching time

KW - Leaching kinetic

KW - Metamict minerals

KW - Redox-state of uranium

UR - http://www.scopus.com/inward/record.url?scp=85041129110&partnerID=8YFLogxK

U2 - 10.1007/s00269-018-0941-6

DO - 10.1007/s00269-018-0941-6

M3 - Article

VL - 45

SP - 549

EP - 562

JO - Physics and Chemistry of Minerals

JF - Physics and Chemistry of Minerals

SN - 0342-1791

IS - 6

ER -

ID: 28273638