Recharge processes limit the resource elements of Qarhan Salt Lake in western China and analogues in the evaporite basins

Hualing SONG; Qishun FAN; Qingkuan LI; Tianyuan CHEN; Haotian YANG; Chunmei HAN

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Recharge processes limit the resource elements of Qarhan Salt Lake in western China and analogues in the evaporite basins

Special Section on Salt Lake Research | Updated：2024-10-14

- Recharge processes limit the resource elements of Qarhan Salt Lake in western China and analogues in the evaporite basins
- Journal of Oceanology and Limnology Vol. 41, Issue 4, Pages: 1226-1242(2023)
- Affiliations：
  
  1. Key Laboratory of Comprehensive and Highly Efficient Utilization of Salt Lake Resources, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China
  2. Qinghai Provincial Key Laboratory of Geology and Environment of Salt Lakes, Xining 810008, China
  3. University of Chinese Academy of Sciences, Beijing 100049, China
- Author bio：
  
  qsfan@isl.ac.cn
- Funds：
- DOI：
  CLC：
- Received：22 June 2022，
  
  Accepted：31 August 2022，
  
  Online First：02 November 2022，
  
  Published：01 July 2023
- Accepted：
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SONG Hualing,FAN Qishun,LI Qingkuan,et al.Recharge processes limit the resource elements of Qarhan Salt Lake in western China and analogues in the evaporite basins[J].Journal of Oceanology and Limnology,2023,41(04):1226-1242.
DOI：

SONG Hualing,FAN Qishun,LI Qingkuan,et al.Recharge processes limit the resource elements of Qarhan Salt Lake in western China and analogues in the evaporite basins[J].Journal of Oceanology and Limnology,2023,41(04):1226-1242. DOI：

摘要

Abstract

The Qarhan Salt Lake (QSL) in western China is K-Sr-Li-B-Br-Rb multi-resource coexisting Quaternary brine deposits. Significant research efforts have been directed to the origin of K-Li resources and evolutionary history of the QSL. However

the study on the different sources

recharge processes

and differential distribution patterns for these resource elements in brine deposits is still inadequate. Therefore

we measured Li-B concentrations and H-O-Sr-B isotopic compositions of different waters (river

spring

and brine) from the QSL

combined with the reported K-Sr contents and multiple isotopes of waters

to discuss the recharge

source of K-Sr-Li-B and their spatial distributions

by analogy with other evaporite basins in the world. The results show that: (1) the K-Li-B-Sr elemental concentrations of brines and their spatial distribution in the QSL are diverse; (2) high K and Sr values are distributed in Dabuxun and Qarhan sections

respectively

which are controlled by Ca-Cl springs in the northern QSL; on the contrary

Li and B values are enriched in the Bieletan section and are charged by thermal springs in the Kunlun Mountains; (3) the formation and evolution of Ca-Cl and thermal springs constrain fundamentally on the recharge processes of K-Sr and Li-B elements in the terminal salt lakes of the Qaidam Basin (QB); (4) some analogues of recharge processes limit the resource elements of the QSL and other salt lakes (Da Qaidam

Lop Nur

Zhabuye

Atacama

and Guayatayoc) in the world provides a reference for the resource exploration in deep formation waters in the evaporite basins.

关键词

Keywords

references

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Hualing SONG

Chunmei HAN

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University of Chinese Academy of Sciences

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