Physical and Chemical Composition of Water in Lake Kara-Kir
DOI:
https://doi.org/10.47494/mesb.v13i.620Keywords:
chloride, sulfate, photosynthesis, Karakir, seasonality, reservoir, lake, mineral substances, pelagialAbstract
Lake Kara-kir is located in the northwest of the Bukhara oasis. The total area of the lake is 26.5-27.2 thousand hectares. The physicochemical composition of lake water changes depending on the seasons of the year. the fact that the amount of chlorides contained in water is 3.6 - 3.7 g / l, and sulfates in high concentration 5.0 - 5.2 g / l, indicates that the degree of salinity occurs due to chloride -sulphates. The readings for dissolved cislarod in water vary, mainly depending on the intensity of photosynthesis and aeration of the water
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