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Stable Isotope and Element Geochemistry of Saline Springs in Evaporite-bearing Mengla Basin,South Yunnan,China 被引量:1
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作者 ZHANG Xiying MA Haizhou +2 位作者 GAO donglin MIAO Weiliang LI Yongshou 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2014年第S1期176-177,共2页
1 Introduction Mengla Basin is a sub-basin in southern evaporitebearing Lanping-Simao Basin.There are many salt springs in the basin.In 2012,11 spring samples were collected for analyses of chemistry and boron,hydroge... 1 Introduction Mengla Basin is a sub-basin in southern evaporitebearing Lanping-Simao Basin.There are many salt springs in the basin.In 2012,11 spring samples were collected for analyses of chemistry and boron,hydrogen and oxygen 展开更多
关键词 Mengla Basin stable isotope and element geochemistry water-rock reactions saline springs.
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Groundwater contributions in water-salt balances of the lakes in the Badain Jaran Desert,China 被引量:8
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作者 GONG Yanping WANG Xusheng +3 位作者 HU B Xiao ZHOU Yangxiao HAO Chunbo WAN Li 《Journal of Arid Land》 SCIE CSCD 2016年第5期694-706,共13页
Groundwater-fed lakes are essential for the ecology in arid and semiarid regions.As a typical arid region,the Badain Jaran Desert (BJD) is famous in the world for the presence of a large number of groundwater-fed sa... Groundwater-fed lakes are essential for the ecology in arid and semiarid regions.As a typical arid region,the Badain Jaran Desert (BJD) is famous in the world for the presence of a large number of groundwater-fed saline lakes among the mega dunes.Based on the up to date geological surveys and observations,this study analyzed the groundwater contributions in water-salt balances of the lakes in the desert.We found different types of springs,including the sublacustrine springs that indicate an upward flow of groundwater under the lakebed.A simplified water balance model was developed to analyze the seasonal variations of water level in the Sumu Barun Jaran Lake,which revealed an approximately steady groundwater discharge in the lake and explained why the amplitude of seasonal changes in lake level is less than 0.5 m.In addition,a salt balance model was developed to evaluate the salt accumulations in the groundwater-fed lakes.The relative salt accumulation time is 800–7,000 years in typical saline lakes,which were estimated from the concentration of Cl-,indicating a long history evolution for the lakes in the BJD.Further researches are recommended to provide comprehensive investigations on the interactions between the lakes and groundwater in the BJD. 展开更多
关键词 arid region groundwater-fed lake spring water level change salinity
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