Source of aeolian dune sands on the northern margin of Qarhan Salt Lake, Qaidam Basin, NW China

2019 ◽  
Vol 55 (5) ◽  
pp. 3643-3653 ◽  
Author(s):  
Jiyan Li ◽  
Ling Zhou ◽  
Jialiang Yan ◽  
Xujia Cui ◽  
Yingying Cai
2013 ◽  
Vol 40 (2) ◽  
pp. 170-182 ◽  
Author(s):  
Xiaorong LUO ◽  
Ying SUN ◽  
Liqun WANG ◽  
Ancheng XIAO ◽  
Lixie MA ◽  
...  

2016 ◽  
Vol 8 (5) ◽  
pp. 670-680 ◽  
Author(s):  
Jiyan Li ◽  
Zhibao Dong ◽  
Guangqiang Qian ◽  
Zhengcai Zhang ◽  
Wanyin Luo ◽  
...  

1998 ◽  
Vol 43 (20) ◽  
pp. 1755-1760 ◽  
Author(s):  
Jingsui Yang ◽  
Zhiqin Xu ◽  
Haibing Li ◽  
Cailai Wu ◽  
Junwen Cui ◽  
...  

Minerals ◽  
2019 ◽  
Vol 9 (11) ◽  
pp. 655 ◽  
Author(s):  
Zhang ◽  
Fan ◽  
Li ◽  
Du ◽  
Qin ◽  
...  

Potash plays an important role in agricultural production. The Qaidam Basin (QB) in western China is a typical inland evaporite basin, which contains an abundance of K-rich brines, including shallow brines (i.e., surface brines and intercrystalline brines) in salt lakes and deep brines (i.e., pore brines and oilfield brines) in the strata. Significant studies on these brines have been reported; however, the integrated studies on sources of K, its distribution, and the sedimentary pattern of the two brine types are still inadequate. In this study, the K+ concentrations of sixty-four intercrystalline brines from the Qarhan Salt Lake (QSL), the largest playa in the QB, are presented. After combining those results with the major ionic compositions of river waters and deep K-rich brines, and the K+ concentrations of shallow brines in the QB, we concluded that: (1) The K of brines in the QSL is mainly from the high–flux K input by rivers which gain K from silicate weathering, while the “ancient Qaidam Lake” contributed little K to the QSL; (2) the large K flux supplied by rivers, the appropriate concentration degree, and the mixing of river waters and spring waters, cooperatively account for the highest K concentrations of brines in the QSL in the QB. The different river K recharges in different sections and isolated depressions are responsible for uneven K+ concentrations of brines in the QSL. (3) The deep brines are mainly distributed in the western QB. The K source of pore brines is from the interaction of pore water with the overlying evaporite layer. While the K in oilfield brines may be meteoric water, salt dissolution, the mixing of hydrothermal fluids, and the conversion of clay minerals to K-feldspar may consume K in the oilfield brines.


2019 ◽  
Vol 98 ◽  
pp. 12025
Author(s):  
Yong Xiao ◽  
Qichen Hao ◽  
Yinfei Luo ◽  
Shengbin Wang ◽  
Xueya Dang ◽  
...  

Lake Qarhan is the largest salt lake and potassium salt resource mining base in china. Understanding the origin of brines and the contribution of modern water circulation is extremely important to the sustainable development of the salt lake. Comprehensive tools including isotope, hydrochemistry and numerical simulation had been performed. Results suggest that brine groundwater in the salt lake area is the result of ancient brines migrated from the western Qaidam Basin due to the uplift of the western basin in the geological past. Shallow phreatic aquifers in the salt lake area are also recharged by the modern surface water in the flood period. The contribution of modern groundwater circulation to the salt lake area is very limited with only 3% of the total quantity of groundwater discharge for the watershed.


2015 ◽  
Vol 7 (4) ◽  
pp. 438-449 ◽  
Author(s):  
Jiyan Li ◽  
Zhibao Dong ◽  
Zhengcai Zhang ◽  
Guangqiang Qian ◽  
Wanyin Luo ◽  
...  

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