Dabusun or Dabasun Nor is a romanization of its Mongolian name, which means simply "Salt Lake". In Mongolian, the name is sometimes designated "eastern", to distinguish it from West Dabusun Lake. It is sometimes misspelled Dabsun or Dabsan. It was formerly known as the Dalai Dabasun, meaning "Sea" or "Ocean of Salt". Dabuxun is the pinyin romanization of the Chinese name , a transcription into characters of the Mongolian name.
Geography
Dabusun lies in the Dabusun subbasin in the central Qarhan Playa. It is one of the many saltwater lakes in the endorheic Qaidam Basin, bound by the Qilian Mountains to the north, the Altun to the west, and the Kunlun to the south. Lying at an elevation of above sea level, it has a mean annual temperature of despite lying on the same latitude as Greece, Algeria, and Virginia in the United States. Dabasun is the largest present lake in the Qarhan Playa. It is fed by the main course of the Golmud River from the south and, to a lesser extent, by mineral springsfrom the north. In Qaidam's hyperarid climate, there is generally only of annual rainfall but about of annual evaporation. Its area is thus variable by season and year, usually 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 east to west, and its width is usually about north to south. The maximum depth is, and the average depth varies from.
Geology
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. Below, the alternating beds of mud and halite extend at least in some places. In addition to common salt, it also has an abundance of carnallite in an area of and magnesium sulfate. The known beds are exposed at the surface or buried by of sedimentation.
History
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. Pollen studies suggest that the area of the lake bed which now underlies Dabusun was raised around in just the last 500,000 years. Tectonic activity also varied sedimentation in the lake by shifting its tributaries and basins, although it remained in the Qarhan Playa during this period. At around 30,000 years ago, this great freshwater lake spread over at least with a surface 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. It has been shrinking in size by evaporation for most of that time, although it was only about in circumference in the mid-19th century, when it was visited by the Polono-Russian explorer Przhevalsky. 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. The area's potassium deposits were accidentally discovered in 1957 and exploratory wells found the Yanhu Gas Field north of the lake the next year.
