Duilong River

Duilong River

Sketch map of the Duilong River and Doilungdêqên District
Country Tibet
Location Damxung County, Doilungdêqên District, Lhasa
Basin
River mouth 29°37′11″N 91°00′39″E / 29.619711°N 91.010815°E / 29.619711; 91.010815Coordinates: 29°37′11″N 91°00′39″E / 29.619711°N 91.010815°E / 29.619711; 91.010815
River system Lhasa River
Basin size 4,988 km2 (1,926 sq mi)
Physical characteristics
Length 137 km (85 mi)

The Duilong River, or Duilong Qu (Tibetan: Toelung; Chinese: 堆龙), is a right tributary of the Lhasa River, which it enters just below the city of Lhasa, Tibet, China. The river is about 137 kilometres (85 mi) in length. Water quality may be compromised by dissolved substances including arsenic from geothermal springs.

Course

The Duilong is the largest tributary of the Lhasa River, with a length of 137 kilometres (85 mi) and a basin area of 4,988 square kilometres (1,926 sq mi).[1] The valley of the Duilong River leads south to the Lhasa River, and is contained by two ridges of the Nianqing Tanggula Mountains. The Duilong has hydro-electrical power generation capacity of 4,000  KW.[2] The non-monsoon season lasts from October to May each year, and the monsoon season from June to October. 80% of the precipitation is in the monsoon season, when warm and moist air is transported to the Tibet Plateau from the south Indian Ocean.[3]

The Qinghai–Tibet Railway approaches Lhasa from the northwest. It descends from the Amdo grasslands to Nagchu and Damshung, and then follows the Toelung River from Yangpachen through Toelung Dechen county into west Lhasa. A new railway bridge was built over the Lhasa river to link the station in Liuwu township on the south side of the river to central Lhasa on the north side.[4]

Water quality

The southern Tibetan Plateau is tectonically active, and contains many geothermal springs. Although rivers in Tibet are generally considered to be clean, the water of the Duilong is affected by these springs. A 2015 study reported that during the non-monsoon season the levels of arsenic in the river, at 205.6 μg/L were higher than the WHO guideline of 10 μg/L for drinking water.[5] The source of the pollution seems to be untreated water from the Yangbajain Geothermal Field power station. It can be detected 90 kilometres (56 mi) downstream from this site.[6]

Yangjinshi Reservoir

A 1995 paper concluded that proposed Yangjinshi Reservoir would provide a good balance between the conflicting demands for irrigation and hydroelectric power generation. It could not be built in the lower reaches, where the river is paralleled by the Qinghai-Xizang Road, or in the middle reach where it would cover the Yangbajain geothermal field. The chosen location was therefore upstream, controlling a catchment area of 1,580 square kilometres (610 sq mi) with an annual normal runoff of 394,000,000 cubic metres (1.39×1010 cu ft). If the water level were maintained at 4,360 metres (14,300 ft) above sea level, the reservoir would have a capacity of 81,000,000 cubic metres (2.9×109 cu ft) including available storage of 19,000,000 cubic metres (670,000,000 cu ft). The project would include a 4500 kW power station.[7]

References

    1. ↑ Ye, Duan & Zang 2010, p. 226.
    2. ↑ Ge & Li 1996, p. 35.
    3. ↑ Li 2013, p. 4144.
    4. ↑ China Strives to Complete Gormo-Lhasa railroad...
    5. ↑ Li 2013, p. 4143.
    6. ↑ Zhang & Huang 1997.
    7. ↑ Shen 1995, p. 155.

    Sources

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