FEATURES OF MINERALIZATION OF THE KAZAKHSTAN PART OF THE SYRDARIA RIVERKAZAKHSTAN
DOI:
https://doi.org/10.54668/2789-6323-2022-104-1-115-128Keywords:
hydrochemical regime, mineralization, main ions, intra-annual distribution of mineralizationAbstract
The article changes the question of the mineralization of the Kazakh part of the Syrdarya River. The hydrological posts Kokbulak were chosen as the main creators, which is a border post for assessing the degree of mineralization of pine from the side of Uzbekistan and Kazaly, which in turn is the closure of the creator, taking into account the needs of the river ecosystem of the lower reaches and the Aral Sea. The article analyzes the changes in the total mineralization and the main ions of the Kazakhstani part of the river. Syrdarya, depending on the water content of the year (25%, 50%, 75%, 95% availability) both for periods with a conditionally natural and disturbed regime. A general analysis of changes in the intra-annual total distribution of minerals and groups of basic ions showed that at an important level, i.e. in the disturbed period of the absence of winter maxima and summer minima, there was more room for stochasticity alien to the conditionally natural period of the hydrological regime.
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