The Minsk City Committee for Natural Resources and Environmental Protection explained.
Photo here and further: minskpriroda / Telegram
The water of Tsnyanka Reservoir has turned a strange color. Near the shore, it acquired a pearlescent hue. Minsk residents thought something might have been dumped into the reservoir. But that's not the reason.
Employees of Mingorkompriroda explain — the color of the water changed due to metaphytone, which forms during a natural process.
"Metaphytone — these are fragments of bottom and underwater surface biofouling that have floated to the surface, or plankton that has accumulated on the water's surface. Its main components are algae, bacteria, dead organic matter, invertebrates, and fungi.
According to the results of laboratory observations, the oxygen content in surface water bodies complies with the established normalized values," — say employees of Mingorkompriroda.
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Comments
Вадасховішчы на Свіслачы - на затопленых поймах ракі, часткова забалочаных. Але гэта не значыць на балоце. Розныя суадносіны торфу і ілу.
Мінск на Мінскім узвышшы з вялікімі (для Беларусі) перападамі вышынь. Таксама не балота.
А становішча Цнянкі будзе пагаршацца і ў перспектыве яно можа ператварыцца ў тэхнічны вадаём. Прычынай моцная звышшчыльная забудова Паўночнага Берага і яе антрапагенны ўплыў на экасістэму.
Заслаўскае, як казаў, на пойме Свіслачы ў месцы злучэння з Вячай і Ратамкай.
Факт наяўнасці балот у Мінску не эквівалентны "Минск вообще весь был одно большое болото". Розны рэльеф быў (і застаецца). Самі разважаеце як анекдатычны "гуманітарый".