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Magnetic isotopes as a means to elucidate Earth and environmental chemistry

Авторы: Buchachenko, A. L.
Краткая информация
Маркер записи n 22 3 4500
Контрольный номер uchm18_to87_no8_ss727_ad1
Дата корректировки 13:47:36 13 мая 2025 г.
Кодируемые данные 181015s2018||||RU|||||||||||#||||# rus0|
Системный контрольный номер RUMARS-uchm18_to87_no8_ss727_ad1
AR-MARS
Служба первич. каталог. Научная библиотека Чувашского государственного университета
МАРС
BY-HM0026
Код языка каталог. rus
Код языка издания eng
eng
Индекс УДК 544
543.4/.5
Индекс ББК 24.5
24.46/48
24.5
24.46/48
Таблицы для массовых библиотек
Таблицы для массовых библиотек
Таблицы для массовых библиотек
Таблицы для массовых библиотек
Buchachenko, A. L.
professor
z01710
070
Magnetic isotopes as a means to elucidate Earth and environmental chemistry
[Текст]
A. L. Buchachenko
Иллюстрации/ тип воспроизводства 13 рис., 13 схем
Библиография Библиогр.: с. 739-740 (92 назв. )
Аннотация In Earth and environmental chemistry, magnetic isotopes provide a universal means to identify reaction mechanisms. Mass-independent fractionation of isotopes as a signature of a mechanism occurs by two ways: first, via the magnetic isotope effect (MIE), which is controlled by magnetic, or hyperfine, coupling between unpaired electrons and magnetic nuclei in paramagnetic species (particularly, in radicals), and, second, via the nuclear volume effect (NVE), which is induced by the volume difference between isotopic nuclei. The MIE is the dependence of the reaction rates on the nuclear magnetic moment of reactants and fractionates magnetic and nonmagnetic isotopes, whereas NVE fractionates isotopes with different nuclear volumes. Both effects, MIE and NVE, are supposed to coexist in condensed phases. A decisive test for their differentiation is illustrated by the example of radical pairs with mercury nuclei. Namely, if isotope fractionation is controlled by MIE, the ratio дельта{201}Hg/дельта{199}Hg is expected to be in the range of 1. 05-1. 25 for isotopic enrichment and 0. 80-0. 92 for depletion. If isotope fractionation is controlled by NVE, this ratio is estimated to be in the range of 0. 50-0. 62. In contrast to MIE-induced bidirectional fractionation controlled by the direction of coherent spin conversion of the radical pair (triplet-singlet or vice versa), the NVE induces unidirectional, universal isotope fractionation, which is almost independent of the reaction mechanism. In contrast to MIE which exhibits inversion of the fractionation sign depending on the spin multiplicity of reactants, NVE is incompatible with the inversion of the fractionation sign. The MIE is an unambiguous indicator of the radical mechanisms and dominates in chemical reactions, whereas NVE prevails in nonchemical processes. Chemical scenarios of MIE-induced oxygen, sulfur, iron, silicon, tin, mercury, germanium and uranium isotope fractionation in photostimulated and dark reactions are analyzed in terms of reaction mechanisms including reactions in living organisms. In conclusion, some restrictions, uncertainties and problems in Earth and environmental chemistry are discussed.
Химия
AR-MARS
Физическая химия в целом
AR-MARS
Физико-химические методы анализа
AR-MARS
Ключевые слова изотопные ядра
изотопы
магнитные изотопные эффекты
магнитные изотопы
физика окружающей среды
химия окружающей среды
ядерные объемные эффекты
N. N. Semenov Institute of Chemical Physics
z01100
Москва
Вторичная ответственность
Institute of Problems of Chemical Physics
z01100
Москва
Вторичная ответственность
Science Center in Chernogolovka of the Russian Academy of Sciences
z01100
Вторичная ответственность
P. G. Demidov Yaroslavl State University
z01100
Вторичная ответственность
Lomonosov Moscow State University
Department of Chemistry
z01100
Вторичная ответственность
ISSN 0042-1308
Название источника Успехи химии
Место и дата издания 2018
Прочая информация Т. 87, № 8. - С. 727-740
RU
42813093
20181015
RCR
RU
42813093
20181015
RU
AR-MARS
20181015
RCR
RU
AR-MARS
20181015
Тип документа b
code
year
to
no
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ad
uchm
2018
87
8
727
1
244