|
The Duilong River, or Duilong Qu (Tibetan: Toelung; ), is a right tributary of the Lhasa River, which it enters just below the city of Lhasa, Tibet, China. The river is about 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 and a basin area of . 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. 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. 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. 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Duilong River」の詳細全文を読む スポンサード リンク
|