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WATER, LAND AND FOREST RESOURCES

ANALYSIS OF THE CURRENT STATE OF THE SHELEK RIVER BASIN

A. Zhandiyar 1 , A. Aldiyarova 1 , Ye. Mukhanbet 1 , B. Amantai 1 , A. Muratova 1

1 NJSC "Kazakh National Agrarian Research University", Almaty, Republic of Kazakhstan

doi.org/10.37884/1-2023/18 pp. 155-164 Admitted 02.02.2023 Published 30.03.2023

Abstract

The subject of the study is the current state of the Shelek River. Research methods are systematization of observation data and their statistical processing, methods of hydrological calculations. Two posts on the Shelek River were taken as hydrological measurement and observation points: in Malybai village and on the Bartogai reservoir. Bartogay. The longest observation period on the Shelek river flow is available for the post in Malybai village Malybai post 48 years (1956-2018). Calculations to determine the hydrological characteristics of the Shelek River and Bartogai Reservoir have been carried out. The climatic factors and the calculated characteristics of the annual flow of the river are analysed. In view of the latter, to calculate the annual flow rate and statistical parameters the available observation series was used, which is mainly 48 years.  The natural water resources of the Bartogai reservoir in an average water year is 971.04 million m3 , intended for seasonal regulation of the river flow with its subsequent drawdown during the growing season for irrigation needs.

The great diversity of general natural conditions and the complexity of the orography of the basin determine considerable differences in the nourishment and water regime during the year. The main share of runoff occurs mainly in the spring-summer period (March-October). The main flow is provided by snow and glacier sources. The area under consideration is divided by hydrological conditions into mountainous - zone of runoff formation and plain - area of runoff losses and dissipation.

river basin, gauging station, annual flow, air temperature, precipitation, hydrography, hydrological characteristics

01 Introduction

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02 References

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Citation Links

[1]2023. ANALYSIS OF THE CURRENT STATE OF THE SHELEK RIVER BASIN. Izdenister natigeler. 1 (97) (Mar. 2023), 155–164. DOI:https://doi.org/10.37884/1-2023/18.
(1)ANALYSIS OF THE CURRENT STATE OF THE SHELEK RIVER BASIN. Izdenister natigeler 2023, No. 1 (97), 155-164. https://doi.org/10.37884/1-2023/18.
ANALYSIS OF THE CURRENT STATE OF THE SHELEK RIVER BASIN. (2023). Izdenister Natigeler, 1 (97), 155-164. https://doi.org/10.37884/1-2023/18
ANALYSIS OF THE CURRENT STATE OF THE SHELEK RIVER BASIN. Izdenister natigeler, [S. l.], n. 1 (97), p. 155–164, 2023. DOI: 10.37884/1-2023/18. Disponível em: https://natsus.kaznaru.edu.kz/index.php/research/article/view/222. Acesso em: 15 sep. 2026.
“ANALYSIS OF THE CURRENT STATE OF THE SHELEK RIVER BASIN”. 2023. Izdenister Natigeler, no. 1 (97) (March): 155-64. https://doi.org/10.37884/1-2023/18.
“ANALYSIS OF THE CURRENT STATE OF THE SHELEK RIVER BASIN” (2023) Izdenister natigeler, (1 (97), pp. 155–164. doi:10.37884/1-2023/18.
[1]“ANALYSIS OF THE CURRENT STATE OF THE SHELEK RIVER BASIN”, Izdenister natigeler, no. 1 (97), pp. 155–164, Mar. 2023, doi: 10.37884/1-2023/18.
“ANALYSIS OF THE CURRENT STATE OF THE SHELEK RIVER BASIN”. Izdenister Natigeler, no. 1 (97), Mar. 2023, pp. 155-64, https://doi.org/10.37884/1-2023/18.
“ANALYSIS OF THE CURRENT STATE OF THE SHELEK RIVER BASIN”. Izdenister natigeler, no. 1 (97) (March 30, 2023): 155–164. Accessed September 15, 2026. https://natsus.kaznaru.edu.kz/index.php/research/article/view/222.
1.ANALYSIS OF THE CURRENT STATE OF THE SHELEK RIVER BASIN. Izdenister natigeler [Internet]. 2023 Mar. 30 [cited 2026 Sep. 15];(1 (97):155-64. Available from: https://natsus.kaznaru.edu.kz/index.php/research/article/view/222
1.ANALYSIS OF THE CURRENT STATE OF THE SHELEK RIVER BASIN. Izdenister natigeler. 2023;(1 (97):155-164. doi:10.37884/1-2023/18