Syr Darya Explained

Syr Darya
Name Other:Jaxartes
Map:Aral_Sea_watershed.png
Subdivision Type1:Country
Subdivision Name1:Kyrgyzstan, Uzbekistan, Tajikistan, Kazakhstan
Subdivision Type5:Cities
Subdivision Name5:Khujand, TJ, Tashkent, UZ, Turkestan, KZ, Kyzylorda, KZ, Baikonur, KZ
Length:2256.25km (1,401.97miles)
Discharge1 Min:170m3/s
Discharge1 Avg:1180m3/s[1]
Discharge1 Max:3900m3/s
Source1:Confluence of Naryn and Kara Darya
Source1 Location:Fergana Valley, Uzbekistan
Source1 Coordinates:40.9008°N 71.7575°W
Source1 Elevation:400m (1,300feet)
Mouth:North Aral Sea
Mouth Location:Kazaly, Kazakhstan
Mouth Coordinates:46.1542°N 60.8736°W
Mouth Elevation:42m (138feet)
Basin Size:402760km2
Tributaries Left:Kara
Tributaries Right:Naryn, Chirciq, Arys, Sarysu
Custom Label:Protection status
Extra:
Wikidata:yes
Zoom:4
Stroke-Width:1.5

The Syr Darya (in Persian pronounced as /siːɾ dæɾˈjɒː/), historically known as the Jaxartes (Greek, Ancient (to 1453);: Ἰαξάρτης), is a river in Central Asia. The name, which is Persian, literally means Syr Sea or Syr River. It originates in the Tian Shan Mountains in Kyrgyzstan and eastern Uzbekistan and flows for 2256.25km (1,401.97miles) west and north-west through Uzbekistan, Sughd province of Tajikistan, and southern Kazakhstan to the northern remnants of the Aral Sea. It is the northern and eastern of the two main rivers in the endorheic basin of the Aral Sea, the other being the Amu Darya (Jayhun, also known by its classical name the Oxus).

In the Soviet era, extensive irrigation projects were constructed around both rivers, diverting their water into farmland and causing, during the post-Soviet era, the virtual disappearance of the Aral Sea, once the world's fourth-largest lake. The point at which the river flows from Tajikistan into Uzbekistan is, at 300m (1,000feet) above sea level, the lowest elevation in Tajikistan.[2] [3] [4]

Name

The second part of the name (Persian: darya,) means "lake" or "sea" in Persian and "river" in the Central-Asian Persian. The current name dates only from the 18th century.

The earliest recorded name was Jaxartes or Iaxartes (Greek, Ancient (to 1453);: Ἰαξάρτης) in Ancient Greek, consist of two morpheme Iaxa and artes, found in several sources, including those relating to Alexander the Great. The Greek name hearkens back to the Old Persian name Yakhsha Arta ("True Pearl"), perhaps a reference to the color of its glacially-fed water.[5] More evidence for the Persian etymology comes from the river's Turkic name up to the time of the Arab conquest, the Yinçü, or "Pearl river", from Middle Chinese 眞珠 *t͡ɕiɪn-t͡ɕɨo.[6] [7] Tang Chinese also recorded this name as Yaosha River 藥殺水 (MC: *jɨɐk-ʃˠɛt) and later Ye River 葉河 (MC: *jiɛp).

The current local name of the river, Syr (Sïr), does not appear before the 16th century. In the 17th century, Abu al-Ghazi Bahadur Khan, historian and ruler of Khiva, called the Aral Sea the "Sea of Sïr," or Sïr Tengizi.

The important evidence is the etymology of the name of the Syr-Darya River mentioned by the Ancient authors – '''Yaksart''', established by V. A. Livshits (2003: 10). It means ‘'''flowing’, ‘streaming’.''' The word belongs to the Sogdian dialect that had emerged from the Saka language group.[8]

History

When the Macedonian army of Alexander the Great reached the Jaxartes in 329 BC, after travelling through Bactria and Sogdia without encountering any opposition, they met with the first instances of native resistance to their presence. In October 329 BC the Macedonians fought the Battle of Jaxartes against the Saka, killing some 1,200 combatants including the leader of the nomads. Alexander was forced to retire south to deal with a revolt in Sogdia. Alexander was wounded in the fighting that ensued and the native tribes took to attacking the Macedonian garrisons stationed in their towns. As the revolt against Alexander intensified it spread through Sogdia, plunging it into two years of warfare, the intensity of which surpassed any other conflict of the Anabasis Alexandri.[9]

On the shores of the Syr Darya, Alexander placed a garrison in the City of Cyrus (Cyropolis in Greek), which he then renamed after himself Alexandria Eschate—"Alexandria the furthest"—in 329 BC. For most of its history since at least the Muslim conquest of Central Asia in the 7th to 8th centuries AD, the name of this city (in present-day Tajikistan) has been Khujand.

In the mid-19th century, during the Russian conquest of Turkestan, the Russian Empire introduced steam navigation to the Syr Darya, initially from Fort Raim[10] but with an important river port at Kazalinsk (Kazaly) from 1847 to 1882, when service ceased.

During the Soviet era, a resource-sharing system was instituted in which Kyrgyzstan and Tajikistan shared water originating from the Amu Darya and Syr Darya rivers with Kazakhstan, Turkmenistan, and Uzbekistan in summer. In return, Kyrgyzstan and Tajikistan received Kazakh, Turkmen, and Uzbek coal, gas, and electricity in winter. After the 1991 fall of the Soviet Union, this system disintegrated and the Central Asian nations have failed to reinstate it. Inadequate infrastructure, poor water-management, and outdated irrigation methods all exacerbate the issue.[11]

In 2012, the Syrdarya–Turkestan State Regional Natural Park was opened in the Kazakhstan, in hopes of protecting the river plain ecosystems, archaeological sites, and historical-cultural monuments, as well as plants and animal species, some of which are rare or endangered.[12]

Geography

The river rises in two headstreams in the Tian Shan Mountains in Kyrgyzstan and eastern Uzbekistan—the Naryn River and the Kara Darya which come together in the Uzbek part of the Fergana Valley—and flows for some 2212km (1,374miles) west and north-west through Uzbekistan and southern Kazakhstan to the remains of the Aral Sea. The Syr Darya drains an area of over 800000km2, but no more than 200000km2 actually contribute significant flow to the river: indeed, two of the largest rivers in its basin, the Talas and the Chu, dry up before reaching it. Its annual flow is a very modest 37km3 per year—half that of its sister river, the Amu Darya.

Along its course, the Syr Darya irrigates the most productive agricultural regions in all of Central Asia, together with the towns of Kokand, Khujand, Kyzylorda and Turkestan.

Various local governments throughout history have built and maintained an extensive system of canals.[6] These canals are of central importance in this arid region. Many fell into disuse in the 17th and early 18th century, but the Khanate of Kokand rebuilt many in the 19th century, primarily along the Upper and Middle Syr Darya.

Ecological damage

Massive expansion of irrigation canals in Middle and Lower Syr Darya during the Soviet period to water cotton and rice fields caused ecological damage to the area. The amount of water taken from the river was such that in some periods of the year, no water at all reached the Aral Sea. The Amu Darya in Uzbekistan and Turkmenistan faced a similar situation.

See main article: Northern river reversal.

The uranium concentration of the stream water is increased in Tajikistan with values of 43 μg/L and 12 μg/L; the WHO guideline value for drinking water of 30 μg/L is partly exceeded. The main input of uranium occurs upstream in Uzbekistan and Kyrgyzstan.[13]

See also

External links

Notes and References

  1. Web site: Cooperative Management of Transboundary Water Resources in Central Asia . Daene C. McKinney . Ce.utexas.edu . 2014-02-07.
  2. Web site: Tajikistan . The World Factbook. 30 January 2020 . lowest point: Syr Darya (Sirdaryo) 300 m .
  3. Web site: Territorial and border issues . . 1 March 2010 . 31 January 2020 . The lowest spot of the country is on the height of 300 meters and the highest spot is on the height of 7495 meters above sea level. .
  4. Web site: General information about Tajikistan . 31 January 2020 . Tajikistan is a typical mountainous country with absolute heights from 300 to 7495 m. . .
  5. "Sïr Daryā." Encyclopaedia of Islam, Second Edition. Edited by: P. Bearman, Th. Bianquis, C.E. Bosworth, E. van Donzel, W.P. Heinrichs. Brill Online, 2014.
  6. В. В. Бартольд. К истории орошения Туркестана. (On the history of Irrigation in Turkestan) in Работы по исторической географии (Works on Historical Geography). Moscow: Vostochnaia Literatura, 2002. Pages 210-231
  7. Tekin. Talat. Notes on Some Chinese Loanwords in Old Turkic. Türk Dilleri Araştırmaları. 7. 1997. 165–173.
  8. Koryakova, Ludmila . 2008-06-01 . Review at Cambridge Core- Elena E. Kuzmina (edited by J.P. Mallory): The Origins of the Indo-Iranians. xviii+762 pages, 132 figures. 2007. Leiden: Brill; 978-90-04-16054-5 hardback. . Antiquity Publications . 82 . 316 . 457 . 10.1017/s0003598x00097076 . 0003-598X.
  9. Book: Holt . Frank Lee . Alexander the Great and Bactria: The Formation of a Greek Frontier in Central Asia . 1989 . Brill . 53 . 9004086129 . 31 March 2019.
  10. Gucheval-Claugny . M. . l'Asie Centrale Et Le Réveil De La Question D'Orient . Revue des Deux Mondes (1829-1971) . 1877 . 21 . 2 . 409 . 44751873 . 0035-1962.
  11. International Crisis Group. "Water Pressures in Central Asia", CrisisGroup.org. 11 September 2014. Retrieved 6 October 2014.
  12. Web site: Сырдарья-Туркестанский государственный региональный природный парк . Syrdarya-Turkestan State Regional Natural Park, The History of the Creation of the Regional Park . 2022-11-01 . Биологический Институт . . ru.
  13. P. . Zoriy . M. . Schläger . K. . Murtazaev . J. . Pillath . M. . Zoriy . B. . Heuel-Fabianek . 2018 . Monitoring of uranium concentrations in water samples collected near potentially hazardous objects in North-West Tajikistan . Journal of Environmental Radioactivity . 181 . 109–117 . 10.1016/j.jenvrad.2017.11.010 . 29136519 .