scholarly journals Lithostratigraphy, mineralogy and the boron-bearing brine evolution of DaQaidam Salt Lake in Qaidam Basin since Holocene period, northern Qinghai-Tibet Plateau

2020 ◽  
Vol 198 ◽  
pp. 04038
Author(s):  
Chunliang Gao ◽  
Junqing Yu ◽  
Xiuyun Min ◽  
Aiying Cheng

Little attention has been paid to the study of sedimentary records from DaQaidam Salt Lake regarding brine evolution and hydro-climate change. Here we report the results of AMS 14C dating and mineralogical investigation on a sediment profile D4 from the south central of perennial saline water-body. The result revealed that pinnoite deposit in the lakebed was formed in early Holocene, the lake underwent three stages of lake-level and brine evolution in Holocene period, which were determined mainly by precipitation-controlled catchment inflow. The mineralogical records also depicted fluctuations in lake level and hydrochemistry on decadal and centennial scales.

2017 ◽  
Vol 430 ◽  
pp. 12-20 ◽  
Author(s):  
QiuFang Chang ◽  
ZhongPing Lai ◽  
FuYuan An ◽  
HaiLei Wang ◽  
YanBin Lei ◽  
...  

2002 ◽  
Vol 10 (1) ◽  
pp. 38-43
Author(s):  
CAO Hong ◽  
XU Mu-Qi ◽  
JIA Qin-Xian ◽  
GAO Yu-Rong ◽  
CHEN Sheng-Gui ◽  
...  

2019 ◽  
Vol 8 (10) ◽  
Author(s):  
Rui Xing ◽  
Qing‐bo Gao ◽  
Fa‐qi Zhang ◽  
Jiu‐li Wang ◽  
Shi‐long Chen

2019 ◽  
Vol 98 ◽  
pp. 07011
Author(s):  
Shu-ya Hu ◽  
Quan-sheng Zhao ◽  
Jian-wei Zhang ◽  
Jian-lei Chen

The objective of this study was to contribute to the understanding of the hydrochemical processes and evolution of brine in the Qaidam basin, in order to provide a theoretical basis for the application of brine resources in the region. The hydrochemical characteristics and evolutionary stages of brine in Mahai Salt Lake were investigated using factor analysis on brine chemistry data from 109 sampling points. Our results showed that the centre of the Salt Lake has the highest concentration of total dissolved solids (TDS), and the hydrochemical type of brine is chloride-magnesium. The brine at the centre of the lake is at the later stages of mirabilite precipitation, and the content of K+ is relatively stable. Comparatively, the hydrochemical type of brine in the slope area of the Salt Lake is Cl-Na-Mg, and is at the early stages of brine evolution. It is of guiding significance to further develop and utilize brine resources, especially to evaluate its resource development potential.


2016 ◽  
Vol 8 (6) ◽  
pp. 446 ◽  
Author(s):  
Cheinway Hwang ◽  
Yung-Sheng Cheng ◽  
Jiancheng Han ◽  
Ricky Kao ◽  
Chi-Yun Huang ◽  
...  

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