Long-Term Geochemical Monitoring of the Source of the Angara River (Runoff from Lake Baikal)

V. I. Grebenshchikova; M. I. Kuzmin; O. A. Proydakova; O. V. Zarubina

doi:10.1134/S1028334X18060028

Long-Term Geochemical Monitoring of the Source of the Angara River (Runoff from Lake Baikal)

Авторы: Grebenshchikova V.I.¹, Kuzmin M.I.¹, Proydakova O.A.¹, Zarubina O.V.¹
Учреждения:
1. Vinogradov Institute of Geochemistry, Siberian Branch
Выпуск: Том 480, № 2 (2018)
Страницы: 735-740
Раздел: Geochemistry
URL: https://ogarev-online.ru/1028-334X/article/view/193337
DOI: https://doi.org/10.1134/S1028334X18060028
ID: 193337

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Аннотация

The long-term data (1950–2017) on the chemical composition of the water from the source of the Angara River, which is the only run-off from Lake Baikal, a large and clean fresh water reservoir, are presented. The absence of water contamination despite the anthropogenic influence is shown. The similarity and constancy of the current composition of the waters in the lake and the Angara River are recorded. It is recommended to continue geochemical studies of this unique world heritage site.