Химический состав гидрокриогенной системы: снег на льду–лёд–подлёдная вода озера Байкал

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Представлены результаты исследований гидрокриогенной системы: снег на льду–лёд–подлёдная вода, полученные в зимний период 2016/17 г. на акватории озера Байкал. Показаны особенности химического состава, распределение водородного показателя, минерализации, ионный состав и основные закономерности миграции макро- и микроэлементов гидрокриогенной системы снег на льду–лёд–подлёдная вода.

Об авторах

И. Б. Воробьева

Институт географии им. В.Б. Сочавы СО РАН

Автор, ответственный за переписку.
Email: irina-vorobyeva@yandex.ru
Россия, Иркутск

Н. В. Власова

Институт географии им. В.Б. Сочавы СО РАН

Email: irina-vorobyeva@yandex.ru
Россия, Иркутск

И. А. Белозерцева

Институт географии им. В.Б. Сочавы СО РАН

Email: irina-vorobyeva@yandex.ru
Россия, Иркутск

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