Short-lived 224Ra and 223Ra isotopes in the Anadyr River–Bering Sea system

A. N. Charkin, O. V. Dudarev, A. N. Salyuk, N. E. Shakhova, V. I. Sergienko, I. P. Semiletov

Результат исследований: Материалы для журналаСтатья

1 цитирование (Scopus)

Выдержка

The first results of activity measurement of short-lived radium isotopes dissolved in water in the Anadyr River–Bering Sea transit system are presented. The trends of the radionuclide behavior after passage through high-gradient river–coastal sea water mixing zone were identified and the exchange rate of the horizontal mixing was determined. The 224Ra/223Ra activity ratio was used to construct the “radium age” model, which served for estimating the residence time of brackish water in the Anadyr River estuary. The factors affecting this value were elucidated.

Язык оригиналаАнглийский
Страницы (с-по)211-214
Число страниц4
ЖурналDoklady Chemistry
Том476
Номер выпуска1
DOI
СостояниеОпубликовано - 1 сен 2017

Отпечаток

Radium
Isotopes
Water
Estuaries
Radioisotopes
Rivers
Saline Waters

ASJC Scopus subject areas

  • Chemistry(all)

Цитировать

Short-lived 224Ra and 223Ra isotopes in the Anadyr River–Bering Sea system. / Charkin, A. N.; Dudarev, O. V.; Salyuk, A. N.; Shakhova, N. E.; Sergienko, V. I.; Semiletov, I. P.

В: Doklady Chemistry, Том 476, № 1, 01.09.2017, стр. 211-214.

Результат исследований: Материалы для журналаСтатья

Charkin, A. N. ; Dudarev, O. V. ; Salyuk, A. N. ; Shakhova, N. E. ; Sergienko, V. I. ; Semiletov, I. P. / Short-lived 224Ra and 223Ra isotopes in the Anadyr River–Bering Sea system. В: Doklady Chemistry. 2017 ; Том 476, № 1. стр. 211-214.
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AU - Shakhova, N. E.

AU - Sergienko, V. I.

AU - Semiletov, I. P.

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AB - The first results of activity measurement of short-lived radium isotopes dissolved in water in the Anadyr River–Bering Sea transit system are presented. The trends of the radionuclide behavior after passage through high-gradient river–coastal sea water mixing zone were identified and the exchange rate of the horizontal mixing was determined. The 224Ra/223Ra activity ratio was used to construct the “radium age” model, which served for estimating the residence time of brackish water in the Anadyr River estuary. The factors affecting this value were elucidated.

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