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Wu River (Yangtze tributary)

Coordinates: 29°43′00″N 107°24′00″E / 29.7167°N 107.4000°E / 29.7167; 107.4000
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Wu River
Sancha, Yachi
Wu River
Wujiang drainage basin
EtymologyNamed for 12 peaks of Wu Mountain
Native nameWu Jiang (Chinese)
Location
CountryChina
StateGuizhou
DistrictChongqing
CitiesWushan, Badong, Zigui, Fuling
Physical characteristics
SourceSancha
 • locationWestern Guizhou
MouthYangtze River
 • location
Fuling, Eastern Chongqing Municipality
Length1,150 km (710 mi)
Basin size80,300 km2 (31,000 sq mi)
Discharge 
 • locationGongtan[1]
 • average1,108 m3/s (39,100 cu ft/s)[2]
 • minimum272 m3/s (9,600 cu ft/s)
 • maximum3,340 m3/s (118,000 cu ft/s)
Basin features
River systemYangtze River system
Tributaries 
 • leftLiuchong River, Furong River
 • rightNanming River, Yu River (Hubei), Ya River

The Wu River (Chinese: 乌江; pinyin: Wū Jiāng) is the largest southern tributary of the Yangtze River. Nearly its entire length of 1,150 kilometres (710 mi) runs within the isolated, mountainous and ethnically diverse province of Guizhou. The river takes drainage from a 80,300-square-kilometre (31,000 sq mi) watershed.

The river flows through the Liupanshui, Anshun, Guiyang (the capital), Qiannan, and Zunyi Districts of Guizhou. All nine regions of the province have at least partial drainage to the river.

Course

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Fuling where Yangtze River and Wu River converge

The river begins as the Sancha in western Guizhou and flows eastwards about 350 km (220 mi). It then bends north, west and south in a 300 km (190 mi) reach called the Yachi, and receives the Nanming River from the right. After the Yachi reach, the Wu makes a broad arc northeast through central Guizhou, picking up fifteen major tributaries including the Yu, Furong and Ya Rivers and flowing through several large hydroelectric dams. It then crosses the border into the provincial-level municipality of Chongqing, flows past Wushan, Badong and Zigui, and empties into the Yangtze River at Fuling, some 50 miles (80 km) east-northeast of Chongqing, in the Wu Gorge of the Three Gorges of the Yangtze. Part of the lower course of the river is flooded by the reservoir of Three Gorges Dam.[3]

History

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Many small river towns along the Wu, such as Gongtan, date back to as early as 200 A.D. Fuling is regarded as the first major town to be built on the river. The city was the capital of the ancient Ba state in the Sichuan area. During the Qin dynasty, the region was brought under Chinese control.

The Wu Gorge is also known as "Golden Helmet and Silver Armor Gorge". The name originates from a helmet-shaped rock formation above the river and a silver-colored cliff of slate. Another name for Wu Gorge is "Iron Coffin Gorge".

River modifications

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The Wu River has been extensively developed for hydroelectricity generation. As of 2010, dams along the river had a combined capacity of 8,500 megawatts (MW).[4] Much of this development is extremely recent, as power generation in 2010 was over four times of that in 2005. Most dams on the river were constructed and owned by the Wujiang Hydropower Corporation. The largest dam, the 232-metre (761 ft) Goupitan Dam, was completed in 2011.[5] Aside from producing power, dams on the Wu River also provide flood control and hydraulic head for irrigation operations.[6]

The lower reaches of the river are heavily polluted because of poor sewage systems and dumping of agricultural waste – so much that it is not even considered suitable for irrigation and industrial purposes.[7]

About 40 kilometres (25 mi) of the river's lower course forms an arm of the Wu Gorge (Big Gorge or Second Gorge) of the Three Gorges, now submerged in up to 30 metres (100 ft) of water from Three Gorges Reservoir. In late 2008, geological instabilities caused landslides with volumes of 20,000 and 50,000 cubic metres (26,000 and 65,000 cu yd). It is speculated that the former slide is part of a larger unstable slope with as much as 100,000 cubic metres (130,000 cu yd). The latter slide caused a wave that swamped boats up to 2 kilometres (1.2 mi) away.[8]

The 10 dams on the river that are either completed, under construction or planned, as of March 2014, are listed below from downstream to upstream.[9][10]

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In the 1950s, local governments began an ambitious project to increase the navigability of the Wu River. The lower 480 kilometres (300 mi) of the river were dredged of sediment and hundreds of sets of rapids were destroyed by explosive charges. Navigation on the upper river, in contrast, reflects the difficulty of traversing the Yangtze in the Three Gorges region before the construction of Three Gorges Dam. With the creation of the reservoir behind this dam, navigation on the lower reaches of the Wu has increased significantly.

Bridges

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The Zunyi Bridge over the Wu River

There are many spectacular bridges along the course of the Wu River. These include (from mouth heading upstream):

See also

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References

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  1. ^ "Wujiang discharge at Gongtan". Center for Sustainability and the Global Environment. River Discharge Database. 1980–1982. Retrieved 2010-08-20.
  2. ^ "Wujiang discharge at Gongtan". Center for Sustainability and the Global Environment. River Discharge Database. 1980–1982. Retrieved 2010-08-20.
  3. ^ "Wu River system (river system, China)". Encyclopædia Britannica Online. Retrieved 2009-03-16.
  4. ^ "Hydropower development on Wu River to reach over 8.5 mln kW of installed capacity by 2010". China Business News. 2006-01-12.
  5. ^ "Wu River dammed at Goupitan Hydropower Station". China Business News. 2004-11-17.
  6. ^ "Goupitan Hydropower Project" (PDF). Chinese National Committee on Large Dams. Archived from the original (PDF) on 2011-07-07. Retrieved 2009-11-30.
  7. ^ "Chongqing Wastewater Project, Three Gorges Dam, China". water-technology.net. Retrieved 2009-11-30.
  8. ^ "Major landslides hit Three Gorges region". Xinhuanet. PROBE international. 2008-12-01. Retrieved 2009-11-30.
  9. ^ Dong, Luan. "INTERACTIVE: Mapping China's "Dam Rush"". Wilson Center. Retrieved 15 June 2014.
  10. ^ "The Last Report on China's Rivers". China's Rivers Report. March 2014. Retrieved 15 June 2014.

29°43′00″N 107°24′00″E / 29.7167°N 107.4000°E / 29.7167; 107.4000