ВЛИЯНИЕ УРОВНЕВОГО РЕЖИМА ВОДЫ НА РАЗВИТИЕ ПРОЦЕССОВ ГИДРОМОРФИЗМА В РАЙОНЕ КАТТАКУРГАНСКОГО ВОДОХРАНИЛИЩА
В статье исследуется процесс гидроморфизма почв вокруг Каттакурганского водохранилища. По результатам
исследований установлено, что на южном, западном и восточном бортах водохранилища распространены типичные
серосуглинистые почвы, не подвергшиеся гидроморфизму, в то время как на северном борту формируется слабая, средняя
и сильная степень гидроморфизма. Это обусловлено разницей высот между северным и остальными бортами
водохранилища, которая составляет 55-60 метров над уровнем моря, а отводящие и подводящие каналы расположены
именно на северном борту.
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