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On the feasibility of determining the 230Th activity in minerals without the addition of a Th radiotracer. / Hosseinpour Khanmiri, Mohammad; Bogdanov, Roman V.

в: Applied Radiation and Isotopes, Том 133, 01.03.2018, стр. 57-60.

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

Harvard

Hosseinpour Khanmiri, M & Bogdanov, RV 2018, 'On the feasibility of determining the 230Th activity in minerals without the addition of a Th radiotracer', Applied Radiation and Isotopes, Том. 133, стр. 57-60. https://doi.org/10.1016/j.apradiso.2017.12.018

APA

Hosseinpour Khanmiri, M., & Bogdanov, R. V. (2018). On the feasibility of determining the 230Th activity in minerals without the addition of a Th radiotracer. Applied Radiation and Isotopes, 133, 57-60. https://doi.org/10.1016/j.apradiso.2017.12.018

Vancouver

Hosseinpour Khanmiri M, Bogdanov RV. On the feasibility of determining the 230Th activity in minerals without the addition of a Th radiotracer. Applied Radiation and Isotopes. 2018 Март 1;133:57-60. https://doi.org/10.1016/j.apradiso.2017.12.018

Author

Hosseinpour Khanmiri, Mohammad ; Bogdanov, Roman V. / On the feasibility of determining the 230Th activity in minerals without the addition of a Th radiotracer. в: Applied Radiation and Isotopes. 2018 ; Том 133. стр. 57-60.

BibTeX

@article{2c7018ecd3af410d92807769de6195b1,
title = "On the feasibility of determining the 230Th activity in minerals without the addition of a Th radiotracer",
abstract = "The necessity of measuring the radioactivity of the 230Тh nuclide arises when attempting to solve a number of geochemical or geochronological problems based on the effects of radioactive disequilibrium in the 238U series. It is the authors{\textquoteright} opinion that the use of the traditional α- and β-emitters of thorium as a radiotracer in order to determine the activity of 230Тh leads to various inconveniences and difficulties of a technical nature. The authors recommend using the 234Тh isotope contained in the study sample as the simplest and most natural way of measuring the chemical yield of the targeted nuclide (230Тh). A sequence of radio-analytical procedures is proposed that will provide a correct assessment of the radioactivity of 230Тh. In addition, a specific example and an evaluation of the accuracy of the proposed methodology are presented, using actual experimental data.",
keywords = "Disequilibrium in the U series, Radiotracer, Registration coefficient, α-and β-emitters of thorium, URANIUM, alpha-and beta-emitters of thorium, Disequilibrium in the U-238 series, TRACER",
author = "{Hosseinpour Khanmiri}, Mohammad and Bogdanov, {Roman V.}",
year = "2018",
month = mar,
day = "1",
doi = "10.1016/j.apradiso.2017.12.018",
language = "English",
volume = "133",
pages = "57--60",
journal = "Applied Radiation and Isotopes",
issn = "0969-8043",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - On the feasibility of determining the 230Th activity in minerals without the addition of a Th radiotracer

AU - Hosseinpour Khanmiri, Mohammad

AU - Bogdanov, Roman V.

PY - 2018/3/1

Y1 - 2018/3/1

N2 - The necessity of measuring the radioactivity of the 230Тh nuclide arises when attempting to solve a number of geochemical or geochronological problems based on the effects of radioactive disequilibrium in the 238U series. It is the authors’ opinion that the use of the traditional α- and β-emitters of thorium as a radiotracer in order to determine the activity of 230Тh leads to various inconveniences and difficulties of a technical nature. The authors recommend using the 234Тh isotope contained in the study sample as the simplest and most natural way of measuring the chemical yield of the targeted nuclide (230Тh). A sequence of radio-analytical procedures is proposed that will provide a correct assessment of the radioactivity of 230Тh. In addition, a specific example and an evaluation of the accuracy of the proposed methodology are presented, using actual experimental data.

AB - The necessity of measuring the radioactivity of the 230Тh nuclide arises when attempting to solve a number of geochemical or geochronological problems based on the effects of radioactive disequilibrium in the 238U series. It is the authors’ opinion that the use of the traditional α- and β-emitters of thorium as a radiotracer in order to determine the activity of 230Тh leads to various inconveniences and difficulties of a technical nature. The authors recommend using the 234Тh isotope contained in the study sample as the simplest and most natural way of measuring the chemical yield of the targeted nuclide (230Тh). A sequence of radio-analytical procedures is proposed that will provide a correct assessment of the radioactivity of 230Тh. In addition, a specific example and an evaluation of the accuracy of the proposed methodology are presented, using actual experimental data.

KW - Disequilibrium in the U series

KW - Radiotracer

KW - Registration coefficient

KW - α-and β-emitters of thorium

KW - URANIUM

KW - alpha-and beta-emitters of thorium

KW - Disequilibrium in the U-238 series

KW - TRACER

UR - http://www.scopus.com/inward/record.url?scp=85039449658&partnerID=8YFLogxK

U2 - 10.1016/j.apradiso.2017.12.018

DO - 10.1016/j.apradiso.2017.12.018

M3 - Article

AN - SCOPUS:85039449658

VL - 133

SP - 57

EP - 60

JO - Applied Radiation and Isotopes

JF - Applied Radiation and Isotopes

SN - 0969-8043

ER -

ID: 28282329