Estimation of Mineralization Increase in the Under-ice Water Layer of Southern Baikal
- Авторлар: Blinov V.1, Gnatovskii R.1, Zhdanov A.1, Granin N.1
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Мекемелер:
- Limnological Institute, Siberian Branch
- Шығарылым: Том 44, № 10 (2019)
- Беттер: 674-678
- Бөлім: Article
- URL: https://journals.rcsi.science/1068-3739/article/view/231254
- DOI: https://doi.org/10.3103/S1068373919100054
- ID: 231254
Дәйексөз келтіру
Аннотация
Changes in the ionic component of the under-ice mineralization in the southern basin of Lake Baikal in 2001–2016 are analyzed. Data on the under-ice layer mineralization variations derived from water conductivity measurements using the SBE-25 high-precision CTD sonde are compared with the results of calculation of salt separation during the formation and growth of the ice cover. The studies demonstrated that the mineralization increase is affected not only by salinization during ice crystallization but also by the water inflow from the central basin of the lake and from the Selenga River (more than a half of its runoff propagates to Southern Baikal in winter).
Негізгі сөздер
Авторлар туралы
V. Blinov
Limnological Institute, Siberian Branch
Хат алмасуға жауапты Автор.
Email: bwad@lin.irk.ru
Ресей, ul. Ulan-Batorskaya 3, Irkutsk, 664033
R. Gnatovskii
Limnological Institute, Siberian Branch
Email: bwad@lin.irk.ru
Ресей, ul. Ulan-Batorskaya 3, Irkutsk, 664033
A. Zhdanov
Limnological Institute, Siberian Branch
Email: bwad@lin.irk.ru
Ресей, ul. Ulan-Batorskaya 3, Irkutsk, 664033
N. Granin
Limnological Institute, Siberian Branch
Email: bwad@lin.irk.ru
Ресей, ul. Ulan-Batorskaya 3, Irkutsk, 664033