ШУ ӨЗЕНІНДЕГІ ТАСӨТКЕЛ СУ ҚОЙМАСЫ БӨГЕТІНІҢ СЕЙСМИКАЛЫҚ КҮШТЕРГЕ ТӨЗІМДІЛІГІ ТУРАЛЫ

Abstract

The article considers the data of the Tasotkel reservoir on the Shu River. Tasotkel reservoir located in the middle part of the Shu Valley, which expands westward downstream from the mouth of the Shonkemin River. Water management calculations have been performed to regulate seasonal runoff. The period of operation and filling of the reservoir is determined by the ratio of inflow and water consumption entering the reservoir. The filling of the reservoir begins in November and reaches its highest level in April, the water supply by the reservoir begins in the second decade of June and lasts until the end of October. The amount of water discharge from the reservoir is excess runoff and is determined by the need for downstream water. It was revealed that the reservoir is emptied in November-December and works without being filled with the current flow. It is established that all gates of the spillway structure remain open for the passage of the transit flow.