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


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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.

作者简介

V. Grebenshchikova

Vinogradov Institute of Geochemistry, Siberian Branch

编辑信件的主要联系方式.
Email: vgreb@igc.irk.ru
俄罗斯联邦, Irkutsk, 650033

M. Kuzmin

Vinogradov Institute of Geochemistry, Siberian Branch

Email: vgreb@igc.irk.ru
俄罗斯联邦, Irkutsk, 650033

O. Proydakova

Vinogradov Institute of Geochemistry, Siberian Branch

Email: vgreb@igc.irk.ru
俄罗斯联邦, Irkutsk, 650033

O. Zarubina

Vinogradov Institute of Geochemistry, Siberian Branch

Email: vgreb@igc.irk.ru
俄罗斯联邦, Irkutsk, 650033

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