Bukhtarma Reservoir water availability fluctuations on the China-Kazakh trans-boundary Irtysh River

Shamshagul Mashtayeva Sr1, Jay Sagin2, Saltanat Sadvakasova1 and Talgat Usmanov3, (1)L. Gumilev Eurasian National University, Geography, Astana, Kazakhstan, (2)Global Institute for Water Security, University of Saskatchewan, School of Environment and Sustainability, Saskatoon, Canada, (3)National Hydrometeorological Service of the Republic of Kazakhstan, Information Technlogies of Water Resources, Astana, Kazakhstan

Contact First Author: Shamshagul Mashtayeva Sr; shamsha2001@mail.ru

Abstract ID#: 34783

 

English Abstract:
Reduction of surface runoff in the Irtysh River Basin in recent decades is leading to disastrous consequences on the aquatic ecosystem in the region. As a result of the runoff reduction the Bukhtarma reservoir and connected Lake Zaysan are experiencing dramatic problems with water availability. The major tributary is the Black Irtysh River with the upstream located in China. The research work is based on data collected for the period 1960 to 2014. We used the water fluctuations of river runoff, water levels and water release from the Bukhtarma reservoir. Scenarios of the future changes were analyzed with analyses of the natural and anthropogenic impacts on the water availability fluctuations on the Bukhtarma reservoir. With the water intake from the Irtysh River estimated at 2 km3 per year, flow decreases by 21.8% compared to the natural conditions in average watered years. When water subtraction is equal to 3 km3 per year, river flow during the dry year can be reduced by 69.0% compared to the natural conditions.