FEATURES OF INTRADAY FLUCTUATIONS IN WATER QUALITY INDICATORS OBSERVED IN THE KAMA RESERVOIR

Authors

  • Anatoly P. Lepikhin Mining Institute of the Ural Branch of the Russian Academy of Sciences, Perm, Russia
  • Tatyana P. Lyubimova Institute of Continuous Media Mechanics of the Ural Branch of the Russian Academy of Sciences, Perm, Russia
  • Andrey V. Bogomolov Mining Institute of the Ural Branch of the Russian Academy of Sciences, Perm, Russia
  • Maksim A. Oputin Mining Institute of the Ural Branch of the Russian Academy of Sciences, Perm, Russia
  • Tatyana N. Sintsova Mining Institute of the Ural Branch of the Russian Academy of Sciences, Perm, Russia

DOI:

https://doi.org/10.17072/2079-7877-2024-3-70-82

Keywords:

reservoirs, water quality, water supply, vertical stratification

Abstract

To solve a wide range of problems related to the protection and rational use of water bodies, it is fundamentally
important to assess fluctuations in the variability of indicators of their chemical composition. In this case, as a rule, seasonal and monthly fluctuations are considered and analyzed. This is due, most of all, to the features of the current monitoring system. The transition to automated measurement systems makes it possible to study and analyze much shorter-period processes, such as inter- and
intra-day fluctuations.
Currently, these fluctuations in water quality indicators in reservoirs are an insufficiently studied phenomenon, although they
play an important role both in shaping the consumer properties of water and ensuring the environmental safety of water bodies. These
fluctuations are especially relevant for water bodies located in zones of active technogenesis, which are the most important sources of
water supply for the largest industrial complexes.
The article examines the processes recorded in two sections of the Kama Reservoir: the lower one, directly adjacent to the
Kama Hydroelectric Power Station, and the upper one, located in the zone of pinching out of its backwater. In the lower section, the
quality of water taken in winter is characterized by pronounced inter- and intra-day fluctuations caused by significant changes in water
discharge rates in the lower pool. At the same time, in the upper section of the reservoir, located in the zone of backwater wedging out,
these fluctuations are observed in the warm period, during the formation of vertical stratification of water masses. These phenomena
occur with a significant decrease in the slopes of the water surface and, accordingly, a decrease in current speeds.

Author Biographies

  • Anatoly P. Lepikhin, Mining Institute of the Ural Branch of the Russian Academy of Sciences, Perm, Russia

    Doctor of Geographical Sciences, Professor,
    Chief Researcher

  • Tatyana P. Lyubimova, Institute of Continuous Media Mechanics of the Ural Branch of the Russian Academy of Sciences, Perm, Russia

    Doctor of Physical and Mathematical Sciences,
    Professor, Head of the Laboratory

  • Andrey V. Bogomolov, Mining Institute of the Ural Branch of the Russian Academy of Sciences, Perm, Russia

    Candidate of Engineering Sciences, Senior Researcher

  • Maksim A. Oputin, Mining Institute of the Ural Branch of the Russian Academy of Sciences, Perm, Russia

    Engineer

  • Tatyana N. Sintsova, Mining Institute of the Ural Branch of the Russian Academy of Sciences, Perm, Russia

    Leading Engineer

Downloads

Published

2024-10-11

How to Cite

FEATURES OF INTRADAY FLUCTUATIONS IN WATER QUALITY INDICATORS OBSERVED IN THE KAMA RESERVOIR. (2024). Geographical Bulletin, 3(70), 70-82. https://doi.org/10.17072/2079-7877-2024-3-70-82

Similar Articles

1-10 of 161

You may also start an advanced similarity search for this article.