Dabusun Lake | |
---|---|
Location | Golmud City Haixi Prefecture Qinghai Province China |
Coordinates | 37°01′27″N95°08′20″E / 37.024081°N 95.1389253°E |
Type | Endorheic saline lake |
Primary inflows | Golmud River |
Basin countries | China |
Max. length | 30 km (19 mi) |
Max. width | 4–7.5 km (2–5 mi) |
Surface area | 184–334 km2 (71–129 sq mi) |
Average depth | 0.5–1.02 m (1 ft 8 in – 3 ft 4 in) |
Max. depth | 1.72 m (5 ft 8 in) |
Surface elevation | 2,675 m (8,776 ft) |
Dabusun Lake | |||||||||
---|---|---|---|---|---|---|---|---|---|
Chinese name | |||||||||
Traditional Chinese | 達布遜 鹽湖 | ||||||||
Simplified Chinese | 达布逊 盐湖 | ||||||||
Postal | Dabasun Nor | ||||||||
Literal meaning | Dabusun Salt Lake | ||||||||
| |||||||||
Mongolian name | |||||||||
Mongolian script | (ᠵᠡᠭᠦᠨ) ᠳᠠᠪᠤᠰᠤᠨ ᠨᠠᠭᠤᠷ | ||||||||
|
Former names | |||||
---|---|---|---|---|---|
Mongolian name | |||||
Mongolian script | ᠳᠠᠯᠠᠢ ᠳᠠᠪᠤᠰᠤᠨ | ||||
|
Dabusun or Dabuxun Lake, alternately known as Dabasun Nor, is a lake beside the town Qarhan,just north of Golmud in the Haixi Prefecture of Qinghai Province in northwestern China. Fed by the main course of the Golmud River,it is the largest present-day lake in the Qarhan Playa. Like the other lakes of the surrounding Qaidam Basin,it is extremely saline,with 307–338 grams of salt per liter of water (2.5 lb/gallon).
Dabusun [1] [2] or Dabasun Nor [3] [4] is a romanization of its Mongolian name,which means simply "Salt Lake". [5] In Mongolian,the name is sometimes designated "eastern",to distinguish it from West Dabusun Lake. [5] It is sometimes misspelled Dabsun [6] or Dabsan. [7] [8] It was formerly known as the Dalai Dabasun, [9] meaning "Sea" or "Ocean of Salt".
Dabuxun [6] is the pinyin romanization of the Chinese name 達布遜 (Dábùxùn),a transcription into characters of the Mongolian name.
Dabusun lies in the Dabusun subbasin in the central Qarhan Playa. [10] It is one of the many saltwater lakes in the endorheic Qaidam Basin, [6] bound by the Qilian Mountains to the north,the Altun to the west,and the Kunlun to the south. [11] Lying at an elevation of 2,675 m (8,776 ft) above sea level,it has a mean annual temperature of 0.1 °C (32.2 °F) despite lying on the same latitude as Greece,Algeria,and Virginia in the United States. [7] Dabasun is the largest present lake in the Qarhan Playa. [6] It is fed by the main course of the Golmud River from the south and,to a lesser extent,by mineral springs [2] from the north. [12] In Qaidam's hyperarid climate,there is generally only 28–40 mm (1–2 in) of annual rainfall but about 3,000 mm (120 in) of annual evaporation. [7] Its area is thus variable by season and year, [13] usually 184–334 km2 (71–129 sq mi) but increasing in the wetter winter and spring and decreasing through the summer and fall. The lake is elongated,stretching from the northwest to the southeast. Its length is usually about 30 km (19 mi) east to west,and its width is usually about 4–7.5 km (2–5 mi) north to south. The maximum depth is 1.72 m (5 ft 8 in),and the average depth varies from 0.5 to 1.02 m (1 ft 8 in to 3 ft 4 in).
Although the northern springs contribute much less volume,their waters carry far greater concentrations of solutes and are important to the chemical composition of the lake. [14] Below,the alternating beds of mud and halite extend at least 40 m (130 ft) in some places. [6] In addition to common salt,it also has an abundance of carnallite [1] (potassium magnesium chloride) in an area of 2 km × 35 km (1 mi × 22 mi) and magnesium sulfate. The known beds are exposed at the surface or buried by 3–4 m (10–13 ft) of sedimentation. [6]
Paleoclimatologists believe that between 770,000 and 30,000 years ago Dabusun formed part of a much larger Qarhan Lake,which alternated nine times between being a fresh- and saltwater lake. [15] Pollen studies suggest that the area of the lake bed which now underlies Dabusun was raised around 700 m (2,300 ft) in just the last 500,000 years. [16] Tectonic activity also varied sedimentation in the lake by shifting its tributaries and basins,although it remained in the Qarhan Playa during this period. [17] At around 30,000 years ago,this great freshwater lake spread over at least 25,000 km2 (9,700 sq mi) with a surface 50–60 m (160–200 ft) above the present levels of its successors. It was cut off and became saline again around 30,000 years ago and began precipitating salts about 25,000 years ago. [18] It has been shrinking in size by evaporation for most of that time, [9] although it was only about 42 km (26 mi) in circumference in the mid-19th century,when it was visited by the Polono-Russian explorer Przhevalsky. [9] [lower-alpha 1]
Until the recent commercial exploitation of the salts and other minerals,the district has remained largely unpopulated,as the salt deposits made it difficult for the nomads of northwestern China to use the area for their herds. [9] The area's potassium deposits were accidentally discovered in 1957 [20] and exploratory wells found the Yanhu Gas Field north of the lake the next year. [21]
The lake lies just west of the G3011 Liuge Expressway. It is also serviced by the Dabusun and Qarhan railway stations on the Qingzang Railway.
Qinghai Lake or Ch'inghai Lake, also known by other names, is the largest lake in China. Located in an endorheic basin in Qinghai Province, to which it gave its name, Qinghai Lake is classified as an alkaline salt lake. The lake has fluctuated in size, shrinking over much of the 20th century but increasing since 2004. It had a surface area of 4,317 km2 (1,667 sq mi), an average depth of 21 m (69 ft), and a maximum depth of 25.5 m (84 ft) in 2008.
Golmud, also known by various other romanizations, is a county-level city in the Haixi Mongol and Tibetan Autonomous Prefecture of Qinghai Province, China. It is now the second-largest city in Qinghai and the third largest in the Tibetan Plateau. The population in 2020 is 221,863.
Carnallite (also carnalite) is an evaporite mineral, a hydrated potassium magnesium chloride with formula KCl.MgCl2·6(H2O). It is variably colored yellow to white, reddish, and sometimes colorless or blue. It is usually massive to fibrous with rare pseudohexagonal orthorhombic crystals. The mineral is deliquescent (absorbs moisture from the surrounding air) and specimens must be stored in an airtight container.
Altyn-Tagh is a mountain range in Northwestern China that separates the Eastern Tarim Basin from the Tibetan Plateau. The western third is in Xinjiang while the eastern part forms the border between Qinghai to the south and Xinjiang and Gansu to the north.
The Qaidam, Tsaidam, or Chaidamu Basin is a hyperarid basin that occupies a large part of Haixi Prefecture in Qinghai Province, China. The basin covers an area of approximately 120,000 km2 (46,000 sq mi), one-fourth of which is covered by saline lakes and playas. Around one third of the basin, about 35,000 km2 (14,000 sq mi), is desert.
Da Qaidam is a county-level administrative zone in Haixi Prefecture in northwestern Qinghai province, China. It borders Gansu province to the north.
The Qarhan or Cha'erhan railway station is a station on the Qingzang Railway at Qarhan in Golmud County, Haixi Prefecture, Qinghai Province, China.
The Prairie Evaporite Formation, also known as the Prairie Formation, is a geologic formation of Middle Devonian (Givetian) age that consists primarily of halite and other evaporite minerals. It is present beneath the plains of northern and eastern Alberta, southern Saskatchewan and southwestern Manitoba in Canada, and it extends into northwestern North Dakota and northeastern Montana in the United States.
The Qarhan Playa or Salt Plain, also misleadingly described as Qarhan Lake, is a playa in the Golmud and Dulan counties of Haixi Prefecture, Qinghai, China. Formerly a single unitary lake, it is now an expansive salt flat divided into four greater sections which contain a number of smaller salt lakes, the largest of which is Dabusun Lake. The area is heavily exploited for its valuable salt, mineral, and rare earth reserves but parts are also protected as a national park and contribute to regional tourism.
West Dabusun or Dabuxun Lake is an ephemeral lake northwest of Golmud in the Haixi Prefecture of Qinghai Province in northwestern China. Comprising a basin in the Qarhan Playa, it fills when meltwater floods the Golmud River, causing it to spill into subsidiary channels west of the main course to Dabusun Lake. Like the other lakes of the surrounding Qaidam Basin, it is extremely saline.
North or Bei Hulsan Lake, also known by other names, is a lake northeast of Golmud in Dulan County, Haixi Prefecture, Qinghai Province, China. A part of the Qarhan Playa, it is filled from the east by the Qaidam River. Like the other lakes of the surrounding Qaidam Basin, it is extremely saline.
South or Nan Hulsan Lake, also known by other names, is a lake northeast of Golmud in Dulan County, Haixi Prefecture, Qinghai Province, China. A part of the Qarhan Playa, it lies east of Tuanjie Lake and south of North Hulsan Lake. Like the other lakes of the surrounding Qaidam Basin, it is extremely saline.
Tuanjie Lake is a lake in the southeastern Qarhan Playa north of Golmud in the Haixi Prefecture of Qinghai Province in northwestern China. It is fed from the south by the Shougong River. Like the other lakes of the surrounding Qaidam Basin, it is extremely saline.
Xiezuo Lake is a lake in the northeastern Qarhan Playa north of Golmud in Dulan County, Haixi Prefecture, Qinghai Province, China. Like the other lakes of the surrounding Qaidam Basin, it is extremely saline.
Dabiele Lake, also known by other names, is an ephemeral lake in the southwestern Qarhan Playa north of Golmud in the Haixi Prefecture of Qinghai Province in northwestern China. It is fed by the Tuolahai and Qingshui Rivers from the Kunlun Mountains to the south. Like the other lakes of the surrounding Qaidam Basin, it is extremely saline; like the other lakes in the Bieletan subbasin, it is rich in lithium.
Xiaobiele Lake or Xiaobieletan is an ephemeral lake in the southwestern Qarhan Playa north of Golmud in the Haixi Prefecture of Qinghai Province in northwestern China. Like the other lakes of the surrounding Qaidam Basin, it is extremely saline; like the other lakes of the surrounding Bieletan subbasin, it is rich in lithium.
Suli or Senie Lake is a lake in the western Qarhan Playa north of Golmud in the Haixi Prefecture of Qinghai Province in northwestern China. It is fed from the west by the Urt Moron River. Like the other lakes of the surrounding Qaidam Basin, it is extremely saline; like the other lakes of the surrounding Bieletan subbasin, it is rich in lithium. Its underlying salt has also trapped one of China's largest onshore natural gas fields.
Dongling Lake is a lake in the Qarhan Playa north of Golmud in the Haixi Prefecture of Qinghai Province in northwestern China. Like the other lakes of the surrounding Qaidam Basin, it is extremely saline.
South, Little, or New Suli or Senie Lake is a small ephemeral lake in Golmud County, Haixi Prefecture, Qinghai Province, China. It lies in the southwest corner of the Qarhan Playa in the southeast Qaidam Basin. It is part of Qarhan's Bieletan subbasin, located south of Suli Lake and west of Dabiele Lake. It is principally fed from the southwest by the Zaohuo or Little Zaohuo River (小灶火河,Xiǎozàohuǒ Hé) and consists of a 1.5 km2 (0.58 sq mi) basin which gradually evaporates into three smaller ponds. As part of the Bieletan subbasin, it is rich in lithium chloride.
The Golmud or Ge'ermu River is a river in Golmud County, Haixi Prefecture, Qinghai Province, China. It flows north from the Kunlun Mountains to Dabusun and (occasionally) West Dabusun Lakes in the central Qarhan Playa in the southeastern Qaidam Basin. The county seat Golmud lies along it.