Suli Lake | |
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涩聂湖 (Chinese) | |
Location | Golmud County Haixi Prefecture Qinghai Province China |
Coordinates | 37°02′06″N94°18′54.5″E / 37.03500°N 94.315139°E |
Type | Endorheic saline lake |
Primary inflows | Urt Moron River |
Basin countries | China |
Surface area | 69–85 km2 (27–33 sq mi) |
Surface elevation | 2,675.6 m (8,778 ft) |
Suli Lake | |||||||||
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Traditional Chinese | 澀聶 湖 | ||||||||
Simplified Chinese | 涩聂 湖 | ||||||||
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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.
Suli [1] [2] and Sheli [2] are romanizations of the lake's Mongolian name,which derives from a word for "temples" or "sideburns". [3] (Compare Manchu ᡧᡠᠯᡠ,šulu.) Senie [a] is the pinyin romanization of the Mandarin pronunciation of the name's transcription into Chinese characters.
Suli Lake lies in the Bieletan subbasin [4] at the western edge of the Qarhan Playa at an elevation of 2,675.6 m (8,778 ft). [1] It is located north of South Suli Lake and northwest of Dabiele Lake. [5] Its area varies from 69–85 km2 (27–33 sq mi). [1] It is fed from the west by the Urt Moron or Utumeiren [6] ( t 烏圖美仁 河 , s 乌图美仁 河 ,Wūtúměirén Hé). [7] Its depth usually does not exceed 1 m (3 ft 3 in). [2]
Suli's position at the western end of the playa means that its waters are relatively less influenced by the concentrated mineral springs along the playa's northern boundary. [8] Its waters are also less saturated with potassium-rich carnallite than other southern lakes,such as Tuanjie. [9] However,the Bieletan subbasin as a whole—inclusive of S. Suli,Dabiele,and Xiaobiele —is the richest source of brine lithium in China,with an estimated store of 7.74 million metric tons (8.53 million short tons) of lithium chloride. [10] The lithium derives from hot springs located near Mount Buka Daban which now feed the Narin Gol River or Hongshui River [11] ( t 紅水 河 , s 红水 河 ,HóngshuǐHé) that flows into East Taijinar Lake. [12] In the past,however,the springs lay within the "Kunlun" paleolake which until about 30,000 years ago produced a river which flowed north into a broad alluvial fan feeding the "Qarhan" paleolake in the Sanhu area. [13] Bieletan's lithium came both from deposits directly flowing into the area at the time and continuing contributions from the Urt Moron and other rivers arising in and flowing through the former alluvial plain. [14]
North of Suli Lake,the Sebei-1 and Sebei-2 gas fields form China's 4th-largest onshore reserve of natural gas,with production capacity of 4.95 billion cubic meters (175 billion cubic feet) per year. A pipeline connects it directly to Xining and Lanzhou. [15]
During the Neogene, tectonic shifts made the bed of Suli Lake the lowest point of the Qaidam Basin, 3,200 m (10,500 ft) below its ridge. [16]
The nearby gas fields were first exploited in 1974. [15]
Natural salt pans or salt flats are flat expanses of ground covered with salt and other minerals, usually shining white under the sun. They are found in deserts and are natural formations.
A dry lake bed, also known as a playa, is a basin or depression that formerly contained a standing surface water body, which disappears when evaporation processes exceed recharge. If the floor of a dry lake is covered by deposits of alkaline compounds, it is known as an alkali flat. If covered with salt, it is known as a salt flat.
A salt lake or saline lake is a landlocked body of water that has a concentration of salts and other dissolved minerals significantly higher than most lakes. In some cases, salt lakes have a higher concentration of salt than sea water; such lakes can also be termed hypersaline lake, and may also be pink lakes on account of their color. An alkalic salt lake that has a high content of carbonate is sometimes termed a soda lake.
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.
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.
Bristol Lake is a dry lake in the Mojave Desert of San Bernardino County, California, 42 km (26 mi) northeast of Twentynine Palms.
A sabkha is a coastal, supratidal mudflat or sandflat in which evaporite-saline minerals accumulate as the result of semiarid to arid climate. Sabkhas are gradational between land and intertidal zone within restricted coastal plains just above normal high-tide level. Within a sabkha, evaporite-saline minerals sediments typically accumulate below the surface of mudflats or sandflats. Evaporite-saline minerals, tidal-flood, and aeolian deposits characterize many sabkhas found along modern coastlines. The accepted type locality for a sabkha is at the southern coast of the Persian Gulf, in the United Arab Emirates. Evidence of clastic sabkhas are found in the geological record of many areas, including the UK and Ireland. Sabkha is a phonetic transliteration of the Arabic word used to describe any form of salt flat. A sabkha is also known as a sabkhah,sebkha, or coastal sabkha.
A lake is an often naturally occurring, relatively large and fixed body of water on or near the Earth's surface. It is localized in a basin or interconnected basins surrounded by dry land. Lakes lie completely on land and are separate from the ocean, although they may be connected with the ocean by rivers. Lakes, as with other bodies of water, are part of the water cycle, the processes by which water moves around the Earth. Most lakes are fresh water and account for almost all the world's surface freshwater, but some are salt lakes with salinities even higher than that of seawater. Lakes vary significantly in surface area and volume of water.
An endorheic lake is a collection of water within an endorheic basin, or sink, with no evident outlet. Endorheic lakes are generally saline as a result of being unable to get rid of solutes left in the lake by evaporation. These lakes can be used as indicators of anthropogenic change, such as irrigation or climate change, in the areas surrounding them. Lakes with subsurface drainage are considered cryptorheic.
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).
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.
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.