The Aral-Syr Darya Basin

Total Page:16

File Type:pdf, Size:1020Kb

The Aral-Syr Darya Basin THE ARAL-SYR DARYA BASIN Location The territory of the Basin includes the Syr Darya river basin with tributaries, and part of the Aral Sea within the borders of Kazakhstan. The Syr Darya originates outside the Kazakh territory in the Fergana Valley, rises in two headstreams – the Naryn River and the Kara Darya, and flows for 2,212 km (1,374 mi) to the Aral Sea, in the Kazakh territory – 1,746 km (1,085 mi). The largest tributaries of Syr Darya within the Kazakh territory are Keles, Arys, Badam, Boraldai, Bugun, while much smaller rivers run from the South-Western slopes of the Karatau ridge. Apart from the Syr Darya River and the Kazakh segment of the «Hungry Steppe» is irrigated from the Uzbek territory via Dostyk Canal, a portion of the Chirchik river flow is supplied via the CHAKIR canal system, and via the ARTUR canal system and other smaller systems. During the period from 1960 to 2002 the Aral Sea level dropped for more than 22 m, i.e. more than 0.5 m/year on average. In certain years the level dropped by more than 1 m. On the whole in 42 years the area of the Aral Sea shrank from 67,000 (25,869 mi²) to 19,000 km2 (7,335 mi²), i.e. by more than 3.5 times. The volume of water decreased from 1,090 km3 (261.5 mi3) to 130 km3 (31 mi3), i.e. more than 8 times. Average depth decreased from 16m (52.5 ft.) to 6.8 m (22.3 ft.). In 1988-1989 the Aral Sea split into two water bodies – the Greater Sea and the Lesser Sea (North Aral Sea). These two stretches existed earlier and were united by the former Berg Strait. The climate in the Syr Darya Basin, in its plain part in particular, is dry and acutely continental. It is characterized by long and hot summers, unusually cold winters, significant annual and daily variations of air temperature, great dryness of air, small cloudiness, scarcity of rainfall at its uneven annual distribution and insignificant snow cover. According to the Senior Department of Land Use and Land Utilization, the land area within the Syr Darya Basin totals 29,756,430 ha. Population Within the territory of the Basin there are 11 towns, of which Chimkent and Kyzylorda are regional centres, and 21 settlements with the population of more than 40,000 people. The total population of the Basin reaches 3.2 mln.people. Groundwater Total expected groundwater resources of the basin is estimated in thousand m3/day (mln. m3/ year): 24929.9 (9099.4), including by level of mineralization: less than 1 g/dm3 – 9539.9 (3482.1); 1-3 g/dm3 –10293.2 (3757) and 1-10 g/dm3 – 5096.8 (1860.3). Within the analysed territory 65 groundwater deposits and areas are prospected and confirmed with the quantity of recoverable reserves totalling 2708.08 thousand m3/day (1014.7 mln. m3/year), including by level of mineralization, in g/dm3: less than 1 – 2177.58 (794.8) and more than 1 – 602.5 thousand m3/day (219.9 mln. m3/year), by designated purpose distributed as follows, thousand m3/day (mln. m3/year): • Household and drinking water supply – 2679.44 (978); • Industrial water supply – 300.14 (109.6); • Irrigation – 460.5 (168.1); • Mineral water – 4.6 (1.6). Ecosystems On a greater part of the territory the zonal lowland ecosystems have degraded due to grazing, or turned into agricultural land, including irrigated. Water ecosystems – the Aral Sea, lakes, rivers and water storage reservoirs, are forage and nesting grounds for waterfowl and wading birds, spawning locations and feeding grounds of juvenile fish, habitat for muskrats, and a buffer zone between aquatic and terrestrial ecosystems. Due to change of stream conditions and excessive haymowing the coen has qualitatively restructured, floodplain meadows are critically endangered. The area of reed meadows has decreased by 6-7 times since the sixties. The area of tugais decreased by 26-28 times. Meadowlands (pastures, hayfields, pasture haloxylon fields) total 70-80% of the territory and are to various degrees susceptible to maninduced degradation. In total 85% of meadowlands are degraded. Flora of the Syr Darya Basin includes more than 2,000 species of plants, the greater portion belonging to the fl ora of the Karatau Mountains and Western Tien Shan ridge (1,666 species). The flora of the lowlands is much poorer – not more than 400 species, of which 210 can be found in hydromorphic habitats (intrazonal ecosystems). Fauna of the Syr Darya Basin is represented by two types of amphibias, 23 reptiles, 319 birds and more that 40 mammals, of these 34 species of birds are in the Red Book of Kazakhstan (Pink-backed Pelican (Pelecanus rufescens) and Dalmatian Pelican (Pelecanus crispus), little egret (Egretta garzetta), spoonbill (Platalea), glossy ibis (Plegadis falcinellus), marbled duck (Anas angustirostris), white-tailed sea eagle (Haliaeetus albicilla) and great blackheaded gull (Larus ichthyaetus), houbara bustard Chlamydotis undulata), etc.) and 5 mammals (Vespertilio bobrinskii (Eptesicus bobrinskoi), marbled polecat (Vormela peregusna), Pallas’ cat (Felis manul), goitered gazelle (Gazella subgutturosa) and Asiatic wild ass). The mammals are mainly represented by desert species, the number of which in the Basin is not less than 25, including 11 wide spread species. Industry Industry in the ASB is represented with oilrefining plants (oil and oil gas extraction and processing), mining (nonferrous metals, uranium, building materials); manufacturing (mainly mechanical engineering, food and light industry), as well as production and distribution of electric power, gas and water. The South Kazakhstan region. Manufacturing with its 80.1% share is the dominating industry in the region. The share of gas, water and electricity generation and distribution in the total production reaches 9.9%. Mining accounts for 10.0%. Production of foodstuffs holds the largest share (40%) within the region’s production sector. The Kyzylorda region has great reserves of mineral resources. The region has 66% off- balance reserves of vanadium, 20.1% of zinc, 13.1% of uranium, 13.6% of lead, 2.1% of oil, 1.5% of natural gas, etc. In the Kyzylorda region industrial water supply of NE «KyzylordaEnergyCentre» is provided from its own water diversion facilities on the Syr Darya, JSC «MRTC» and oil-refining plants – from their own groundwater wells. Water for industrial enterprises in the northern industrial district is supplied from the technical water pipeline of NE «KyzylordaEnergyCentre». Main water consumers in Chimkent are large industrial enterprises, inter alia: JSC «Himfarm», Energo Ortalyk-3, Ltd «PetroKazahstan Oil Products», JSC «ShymkentCement», JSC «UzhPoleMetal». Agriculture Of the total ASB area agricultural lands occupy 17,172,880 ha, or 57.71 %, including: arable land – 3.44 %, hayfi elds – 0.83 %, pastures – 52.7 %, other – 0.74 %. Earlier the irrigated land totaled 768,630 ha of the territory, these days – 730,000 ha, or 4.2 % of the total area of agricultural land. Crop production makes 60.3 % of agricultural production. The priority crop produced in the Kyzylorda region is rice (78,000 ha) and in the South Kazakhstan region – cotton (140,000 ha). The Aral – Syr Darya basin occupies one third of the irrigated land in the Republic of Kazakhstan. Due to a number of circumstances about 100,000 ha of irrigated land has not been used in agriculture, which was caused by land degradation and deterioration of irrigation and drainage networks. Irrigated land of the South Kazakhstan region is concentrated in the form of large irrigated tracts, e.g. former Golodnosteppe irrigated tract, Kyzylkum, Arys-Turkestan, Keless tracts and smaller irrigated strips (off-tract land). Irrigated areas were mainly used for production of cotton, fodder and vegetable crops. Of total regularly irrigated area 46 % were under cotton crops, 30 % - fodder crops, 8 % – rice (Kyzylkum tract – 1 stage), and the rest of the area was under vegetables, gardens and vineyards. These days the Syr Darya Basin irrigated land is exploited as follows: cotton – 44 %, fodder crops – 31 %, grain crops – 4 % and other crops. Crop rotation is not always observed. Irrigated land of the Kyzylorda region is also located in large tracts, inter alia: Zhanakorgan- Shieliy, Kyzylordinskiy Left-bank and Rightbank, Kazalinsk. During the whole period of their exploitation the irrigation systems of the region were neither refurbished nor properly serviced or repaired, which explains their high level of wear and tear and, as a consequence, low meliorative efficiency. The Basin has about 1.1 mln. ha of land potentially suitable for irrigation; however, the increase in the irrigated areas is hindered by shortage of irrigating water. Water supply Water supply of towns, settlements and a number of industrial enterprises is ensured through the use of groundwater and surface water. Groundwater is most intensively exploited for household and drinking, industrial water supply, irrigation and pasture watering. As of end 2009 459 settlements of the Basin were united in a central water supply system. The length of the water pipe networks totals 3,200.0 km (1,988 mi). The population of thesesettlements makes 56% of the total population. Formally this part of the population is considered supplied with drinking water. In reality not everyone receives water from the water supply system as the water pipes in the settlements do not cover all the households and are in poor state. On average 50-80% of households are supplied with water. Water supply for the population is organized mainly through the network of standpipes. The inhabitants of 517 populated localities are supplied with water from local sources. The state of water supply in 115 settlements is unsatisfactory as the population has to bring drinking water from neighbouring localities.
Recommended publications
  • Selected Works of Chokan Valikhanov Selected Works of Chokan Valikhanov
    SELECTED WORKS OF CHOKAN VALIKHANOV CHOKAN OF WORKS SELECTED SELECTED WORKS OF CHOKAN VALIKHANOV Pioneering Ethnographer and Historian of the Great Steppe When Chokan Valikhanov died of tuberculosis in 1865, aged only 29, the Russian academician Nikolai Veselovsky described his short life as ‘a meteor flashing across the field of oriental studies’. Set against his remarkable output of official reports, articles and research into the history, culture and ethnology of Central Asia, and more important, his Kazakh people, it remains an entirely appropriate accolade. Born in 1835 into a wealthy and powerful Kazakh clan, he was one of the first ‘people of the steppe’ to receive a Russian education and military training. Soon after graduating from Siberian Cadet Corps at Omsk, he was taking part in reconnaissance missions deep into regions of Central Asia that had seldom been visited by outsiders. His famous mission to Kashgar in Chinese Turkestan, which began in June 1858 and lasted for more than a year, saw him in disguise as a Tashkent mer- chant, risking his life to gather vital information not just on current events, but also on the ethnic make-up, geography, flora and fauna of this unknown region. Journeys to Kuldzha, to Issyk-Kol and to other remote and unmapped places quickly established his reputation, even though he al- ways remained inorodets – an outsider to the Russian establishment. Nonetheless, he was elected to membership of the Imperial Russian Geographical Society and spent time in St Petersburg, where he was given a private audience by the Tsar. Wherever he went he made his mark, striking up strong and lasting friendships with the likes of the great Russian explorer and geographer Pyotr Petrovich Semyonov-Tian-Shansky and the writer Fyodor Dostoyevsky.
    [Show full text]
  • Diversity and Ecology of Periphytonic Algae in the Arys River Basin, Kazakhstan
    Journal of Ecology & Natural Resources ISSN: 2578-4994 Diversity and Ecology of Periphytonic Algae in the Arys River Basin, Kazakhstan 1 2 Barinova SS *, Krupa EG Research Article 1Institute of Evolution, University of Haifa, Israel Volume 1 Issue 1 2 Republican State Enterprise on the Right of Economic Use "Institute of Zoology", Received Date: June 27, 2017 Ministry of Education and Science, Science Committee, Republic of Kazakhstan Published Date: July 15, 2017 DOI: 10.23880/jenr-16000106 *Corresponding author: Barinova SS, Institute of Evolution, University of Haifa, Mount Carmel, 199 Abba Khoushi Ave., Haifa 3498838, Israel, E-mail: [email protected] Abstract No one information about algal community diversity from the Arys River basin was before this study. The first data about algal and cyanobacteria species diversity was represented for the Arys River basin and compared it to freshwater algae patterns of the related mountain regions. Altogether 82 species were found in 28 samples of phytoperiphyton on 13 sampling stations of the Arys River and its tributaries. Diatoms prevail in studied algal flora. Bioindication characterize the Arys River waters as temperate, moderately oxygenated, fresh, neutral water affected by a low to moderate level of organic pollution, Class II-III of water quality. The pattern of algae and cyanobacteria diversity distribution depends on altitude and local climatic and environmental conditions. Bacillariophyta species was richest in high mountain habitats, green algae, cyanobacteria and charophytes avoid high mountain habitats and have negative correlation with altitude. These results can be used as indicator of environmental changes in the mountainous areas. Three floristic groups were recognized in the studied river communities corresponding to the upper, middle and lower parts of the watershed.
    [Show full text]
  • Dam Safety in Central Asia
    ECONOMIC COMMISSION FOR EUROPE Geneva Water Series No. 5 Dam safety in Central Asia: Capacity-building and regional cooperation UNITED NATIONS ECE/MP.WAT/26 ECONOMIC COMMISSION FOR EUROPE Geneva Water Series № 5 DAM SAFETY IN CENTRAL ASIA: CAPACITY-BUILDING AND REGIONAL COOPERATION UNITED NATIONS New York and Geneva 2007 ii NOTICE The designations employed and the presentation of the material in this publication do not imply the expression of any opinion whatsoever on the part of the Secretariat of the United Nations concerning the legal status of any country, territory, city or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. ECE/MP.WAT/26 UNECE Information Unit Phone: +41 (0)22 917 44 44 Palais des Nations Fax: +41 (0)22 917 05 05 CH-1211 Geneva 10 E-mail: [email protected] Switzerland Website: http://www.unece.org UNITED NATIONS PUBLICATION Sales No E.07.II.E.10 ISBN 92-1-116962-1 ISSN 1020-0886 Copyright © United Nations, 2007 All rights reserved Printed at United Nations, Geneva (Switzerland) iii FOREWORD The United Nations Economic Commission for Europe (UNECE), in particular through its Convention on the Protection and Use of Transboundary Watercourses and International Lakes, is engaged in promoting cooperation on the management of shared water resources in Central Asia – a pre-condition for sustainable development in the subregion. One direction of activities is promoting the safe operation of more than 100 large dams, most of which are situated on transboundary rivers. Many of these dams were built 40 to 50 years ago, and due to limited resources for their maintenance and the inadequacy of a legal framework for their safe operation, the risk of accidents is increasing.
    [Show full text]
  • 6. Current Status of the Environment
    6. Current Status of the Environment 6.1. Natural Environment 6.1.1. Desertification Kazakhstan has more deserts within its territory than any other Central Asian country, and approximately 66% of the national land is vulnerable to desertification in various degrees. Desertification is expanding under the influence of natural and artificial factors, and some people, called “environmental refugees,” are obliged to leave their settlements due to worsened living environments. In addition, the Government of RK (Republic of Kazakhstan) issued an alarm in the “Environmental Security Concept of the Republic of Kazakhstan 2004-2015” that the crisis of desertification is not only confined to Kazakhstan but could raise problems such as border-crossing emigration caused by the rise of sandstorms as well as the transfer of pollutants to distant locations driven by large air masses. (1) Major factors for desertification Desertification is taking place due to the artificial factors listed below as well as climate, topographic and other natural factors. • Accumulated industrial wastes after extraction of mineral resources and construction of roads, pipelines and other structures • Intensive grazing of livestock (overgrazing) • Lack of farming technology • Regulated runoff to rivers • Destruction of forests 1) Extraction of mineral resources Wastes accumulated after extraction of mineral resources have serious effects on the land. Exploration for oil and natural gas requires vast areas of land reaching as much as 17 million hectares for construction of transportation systems, approximately 10 million hectares of which is reportedly suffering ecosystem degradation. 2) Overgrazing Overgrazing is the abuse of pastures by increasing numbers of livestock. In the grazing lands in mountainous areas for example, the area allocated to each sheep for grazing is 0.5 hectares, compared to the typical grazing space of 2 to 4 hectares per sheep.
    [Show full text]
  • The Aral Sea Basin Is Located in the Centre of Eurasian Continent And
    The Aral Sea Basin is located in the centre of Eurasian continent and covers the territory of Tajikistan, Uzbekistan, major part of Turkmenistan, part of Kyrgyzstan, southern part of Kazakhstan and northern part of Afghanistan. Water resources of the Aral Sea basin are formed in surface and underground sources and glaciers. Surface waters are mainly concentrated in the basins of the two main rivers of the region –Amudarya and Syrdarya. Independent hydrographic basins (gravitating towards the Amudarya and Syrdarya rivers) create Kashkadarya, Zaravshan, Murgab, Tedjen, Chu, Talas rivers that lost connection with the main rivers many centuries ago. The territory can be divided to three main zones on the conditions of formation and transformation of the surface flow in the region: • zone, where the flow is formed (area of feeding in mountainous regions); • zone of transit and dispersion of flow; • delta zones. Numerous glaciers are concentrated in the mountain systems of the Central Asia, which give rise to practically all large rivers of the region, the water of which is intensively used in the national economy. The major part of glaciers is located in the territory of the Republic of Tajikistan and the Republic of Kyrgyzstan. On the whole, water resources in the Aral Sea basin are not equally distributed. 55,4% of the flow in the basin are formed within the territory of Tajikistan, in Kyrgyzstan – 25,3%, in Uzbekistan – 7,6%, in Kazakhstan – 3,9%, in Turkmenistan – 2,4%, on the territory of Afghanistan and other countries, share of which is not significant (China, Pakistan) – around 5,4% of the flow is formed.
    [Show full text]
  • Kazakhstan), As Influenced by Climate Variation and Human Activity
    sustainability Article Variation in Runoff of the Arys River and Keles River Watersheds (Kazakhstan), as Influenced by Climate Variation and Human Activity Sanim Bissenbayeva 1,2,3,4, Jilili Abuduwaili 1,2,3,*, Dana Shokparova 4 and Asel Saparova 5 1 State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China 2 Research Center for Ecology and Environment of Central Asia, Chinese Academy of Sciences, Urumqi 830011, China 3 Research Center for Ecology and Environment of Central Asia, University of Chinese Academy of Sciences, Beijing 100049, China 4 Department of Geography, Land Management and Cadastre, Al-Farabi Kazakh National University, Almaty 050040, Kazakhstan 5 Institute of Geography, Satbayev University, Almaty 050010, Kazakhstan * Correspondence: [email protected] Received: 27 July 2019; Accepted: 29 August 2019; Published: 2 September 2019 Abstract: Runoff formation is a complex meteorological-hydrological process impacted by many factors, especially in the inland river basin. In this study, long-term (1960–2015) river runoff and climate data in the Arys and Keles River watersheds (Kazakhstan) were gathered to analyze the impacts of climate variation and human activity on runoff. The non-parametric Kendall test and the Pettitt test were used to identify trends and change points in the time data series. It was found that both watersheds had significant upward trends in temperature and potential evapotranspiration data, and insignificant upward trends in the runoff. Change points in annual runoff were identified around the year 1973. The hydrological sensitivity method was employed to evaluate the impacts of climate variation and human activity on mean annual runoff based on precipitation and potential evapotranspiration.
    [Show full text]
  • Review of Key Reforms in Urban Water Supply and Sanitation Sector
    Review of Key Reforms in Urban Water Supply and Sanitation Sector Draft Report Version 2 November 2004 Prepared by Vodokanal-Invest- Consulting, Moscow Contents GLOSSARY .................................................................................................................................................. 3 1. INTRODUCTION............................................................................................................................... 4 2. LEGAL AND INSTITUTIONAL REFORMS ................................................................................. 6 2.1. OVERVIEW OF LEGAL SETUP........................................................................................................... 6 2.1.1. Management of, and Ownership in, Communal Water Supply and Sanitation Systems ............ 6 2.1.2. Public Relations. Accounting for Water Consumption. Billing and Payment Procedures ............ 7 2.1.3. Service Quality. Standards and Norms ...................................................................................... 7 2.2. PRIVATE SECTOR PARTICIPATION IN URBAN WATER SUPPLY AND SANITATION ............................ 8 2.1.1. Legal Framework for Private Sector Participation ................................................................... 8 2.1.2. Incentives for, and Main Trends in, Private Sector Involvement............................................... 8 3. ECONOMIC STANDING OF URBAN WATER SUPPLY AND SANITATION SECTOR....... 9 3.1. REVIEW OF CURRENT SITUATION...................................................................................................
    [Show full text]
  • Long-Term Variations in Runoff of the Syr Darya River Basin Under Climate Change and Human Activities
    ChinaXiv合作期刊 Long-term variations in runoff of the Syr Darya River Basin under climate change and human activities Sanim BISSENBAYEVA1,2,3,4, Jilili ABUDUWAILI1,2,3*, Assel SAPAROVA5, Toqeer AHMED6 1 State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China; 2 Research Center for Ecology and Environment of Central Asia, Chinese Academy of Sciences, Urumqi 830011, China; 3 University of Chinese Academy of Sciences, Beijing 100049, China; 4 Al-Farabi Kazakh National University, Almaty 050040, Kazakhstan; 5 Institute of Geography, Satbayev University, Almaty 050010, Kazakhstan; 6 Centre for Climate Research and Development, COMSATS University Islamabad, Tarlai Kalan 45550, Pakistan Abstract: In this study, we analyzed the hydrological and meteorological data from the Syr Darya River Basin during the period of 1930–2015 to investigate variations in river runoff and the impacts of climate change and human activities on river runoff. The Syr Darya River, which is supplied by snow and glacier meltwater upstream, is an important freshwater source for Central Asia, as nearly half of the population is concentrated in this area. River runoff in this arid region is sensitive to climate change and human activities. Therefore, estimation of the climatic and hydrological changes and the quantification of the impacts of climate change and human activities on river runoff are of great concern and important for regional water resources management. The long-term trends of hydrological time series from the selected 11 hydrological stations in the Syr Darya River Basin were examined by non-parametric methods, including the Pettitt change point test and Mann-Kendall trend tests.
    [Show full text]
  • CBD Third National Report
    MINISTRY OF ENVIRONMENTAL PROTECTION OF THE REPUBLIC OF KAZAKHSTAN THIRD NATIONAL REPORT ON PROGRESS IN IMPLEMENTATION OF THE CONVENTION ON BIOLOGICAL DIVERSITY Astana 2005 1 CONTENTS A. REPORTING PARTY .......................................................................................................................... 3 Information on the preparation of the report ..................................................................3 B. PRIORITY SETTING, TARGETS AND OBSTACLES .............................................................................. 5 Priority Setting .........................................................................................................5 Challenges and Obstacles to Implementation .................................................................6 2010 Target .............................................................................................................9 Global Strategy for Plant Conservation (GSPC) ............................................................. 44 Ecosystem Approach................................................................................................ 55 C. ARTICLES OF THE CONVENTION.................................................................................................... 57 Article 5 – Cooperation............................................................................................. 57 Article 6 - General measures for conservation and sustainable use................................... 60 Article 7 - Identification and monitoring .....................................................................
    [Show full text]
  • 3 the States of the Oghuz, the Kimek and the Kïpchak
    ISBN 978-92-3-103467-1 The Oghuz 3 THE STATES OF THE OGHUZ, THE KIMEK AND THE KÏPCHAK* S. G. Agajanov Contents The Oghuz ........................................ 66 The Kimek ....................................... 74 The Kïpchak ....................................... 77 The Oghuz During the ninth and tenth centuries, the nomadic Turkic Oghuz tribes formed a principal- ity on the middle and lower reaches of the Syr Darya (Jaxartes), in the Aral Sea region and the area of the northern Caspian. There are a number of obscure points in the history of the formation of the Oghuz people and principality in western Central Asia and Kazakhstan. The late S. P. Tolstov considered the home of the Oghuz to be the deserts and steppes of the Aral Sea region. In his view, they had lived there in ancient times before migrating from western to eastern Central Asia.1 In spite of its originality, however, this viewpoint did not gain general acceptance. Research in recent decades points to the conclusion that the Oghuz in western Central Asia originally came from the eastern T’ien Shan region. Oghuz historical tales relate that the headquarters of their supreme ruler or leader was at one time situated on the shores of Lake Issyk-kül. According to different versions of this legend, there was strife among the Oghuz caused by the hostile relations between their ruler and his son, Oghuz Khan. In his * See Maps 1 and 2. 1 Tolstov, 1948. 66 ISBN 978-92-3-103467-1 The Oghuz account of this old legend, the Persian historian Rash¯ıd al-D¯ın, who lived at the end of the thirteenth and the beginning of the fourteenth century, wrote that after a lengthy struggle, Oghuz Khan seized his father’s lands in the district of Talas.
    [Show full text]
  • DRAINAGE BASIN of the ARAL SEA and OTHER TRANSBOUNDARY SURFACE WATERS in CENTRAL ASIA Chapter 3
    68 DRAINAGE BASIN OF THE ARAL SEA AND OTHER TRANSBOUNDARY SURFACE WATERS IN CENTRAL ASIA Chapter 3 ARAL SEA AND OTHER WATERS IN CENTRAL ASIA 69 71 AMU DARYA RIVER BASIN 75 ZERAVSHAN RIVER BASIN 76 SYR DARYA RIVER BASIN 83 ARAL SEA 84 CHU-TALAS RIVER BASINS 89 ILI RIVER BASIN 91 LAKE BALQASH 91 MURGAB RIVER BASIN 91 TEJEN RIVER BASIN Chapter 3 70 ARAL SEA AND OTHER WATERS IN CENTRAL ASIA This chapter deals with major transboundary rivers in Central Asia which have a desert sink, or discharge either into one of the rivers (or their tributaries) or the Aral Sea or an another enclosed lake. It also includes lakes located within the basin of the Aral Sea. Practically all of the renewable water resources in this area are used predominantly for irrigation, and the national economies are developing under conditions of increasing freshwater shortages. TRANSBOUNDARY WATERS IN THE BASIN OF THE ARAL SEA AND OTHER TRANSBOUNDARY SURFACE WATERS IN CENTRAL ASIA1 Basin/sub-basin(s) Total area (km²) Recipient Riparian countries Lakes in the basin Amu Darya …2 Aral Sea AF, KG, TJ, UZ, TM - Surkhan Darya 13,500 Amu Darya TJ, UZ - Kafirnigan 11,590 Amu Darya TJ, UZ - Pyanj 113,500 Amu Darya AF, TJ -- Bartang … Pyanj AF, TJ -- Pamir … Pyanj AF, TJ - Vakhsh 39,100 Amu Darya KG, TJ Aral Sea Zeravshan …2 Desert sink TJ, UZ Syr Darya …2 Aral Sea KZ, KG, TJ, UZ - Naryn … Syr Darya KG, UZ - Kara Darya 28,630 Syr Darya KG, UZ - Chirchik 14,240 Syr Darya KZ, KG, UZ -Chatkal 7,110 Chirchik KG, UZ Chu 62,500 Desert sink KZ, KG Talas 52,700 Desert sink KZ, KG Assa … Desert sink KZ, KG Ili 413,000 Lake Balqash CN, KZ Lake Balqash Murgab 46,880 Desert sink AF, TM - Abikajsar … Murgab AF, TM Tejen 70,260 Desert sink AF, IR, TM 1 The assessment of water bodies in italics was not included in the present publication.
    [Show full text]
  • Integrated Water Cycle Management in Kazakhstan
    Integrated Water Cycle Management in Kazakhstan i Integrated Water Cycle Management in Kazakhstan Editors: Burghard C. Meyer Leipzig University, Germany Lian Lundy, Middlesex University, London, UK Textbook developed in the TEMPUS IV – 5th Call of Proposals on Joint Projects Almaty “Qazag university” 2014 Editors: Burghard C. Meyer & Lian Lundy, The publication should be citated as follows Meyer B. C. & L. Lundy (Eds). 2014. Integrated Water Cycle Management in Kazakhstan. Al-Farabi Kazakh National University, Publishing House, Almaty, 320 pages ISBN: 978-601-04-0900-2 Published with active contributions of the TEMPUS IV IWEB-Project partner’s institutions: Middlesex University, London, UK Al-Farabi Kazakh National University, Almaty, Kazakhstan Ahmed Yasawi International Kazak-Turkish University, Turkistan, Kazakhstan Kokshetau State University named after Shokan Ualikhanov, Kokshetau, Kazakhstan Universität Leipzig, Germany Universitat Politecnica de Valencia, Spain University of Cyprus, Nicosia, Cyprus Institute of Geography of the Republic of Kazakhstan, Almaty, Kazakhstan The Regional Environmental Centre for Central Asia, Almaty, Kazakhstan Kazakh Scientific Research Institute of Water Economy, Taraz, Kazakhstan Kazakh Research Institute of Fishery, Almaty, Kokshetau, Kazakhstan Institute of Professional Development and Retraining, Kokshetau, Kazakhstan Ministry of Education and Science Control Committee, Astana, Kazakhstan Center of Bologna process and academic mobility, Astana, Kazakhstan Fund Zhas Otan, Akmola region, Kokshetau, Kazakhstan No responsibility is assumed by the Publisher, the Editors and Authors by any injury and/or damage to persons or property of products liability, negligence or otherwise, or form any use or operation of any methods, products, instructions or ideas contained in the materials herein. The authors are responsible for the content of their chapters.
    [Show full text]