柴达木盆地马海盐湖低品位固体钾盐矿物组成对溶液采矿过程中钾提取和锂分布的影响

IF 2.2 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Geological Journal Pub Date : 2025-01-12 DOI:10.1002/gj.5115
Pengyu Long, Xianfu Zhao, Yanjun Zhao, Ik Woo, Jiangmin Du, Zhaoxu Wang, Yufei Hu
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引用次数: 0

摘要

随着高品位钾肥资源的日益稀缺,锂作为一种重要的伴生物被人们所认识,柴达木盆地马海盐湖低品位固体钾肥已成为日益重要的钾肥资源开发目标。然而,从这些低品位矿石中释放钾的效率低下,限制了它们在工业上的经济可行性。本研究利用x射线衍射仪(XRD)、扫描电镜-能谱仪(SEM-EDS)和观测井眼监测数据,系统分析了这些矿石的矿物学特征及其对固液转化过程中钾离子释放的影响。结果表明,光卤石、钾盐和多盐石是主要的钾矿物,其空间差异显著,直接影响钾离子的释放和迁移。浅层中的钾盐和光卤石与溶剂的反应性更强,有利于钾离子的快速释放,而多卤石则寄存于岩盐的晶间碎屑物质中,其孔隙连通性有限,导致释放速度较慢。监测井眼数据表明,溶剂注入量的变化会引起水位和钾离子浓度的显著波动,从而影响钾的溶解速率。随着溶液开采的进行,高锂区逐渐扩大,卤水中锂浓度可达120.4 mg/L,一般在20 ~ 70 mg/L之间。钾和锂分布的空间相关性表明,锂可以作为副产物有效回收。根据矿物分布和监测数据,调整溶剂注入速率和浓度,对于优化生产过程中钾和锂的溶解效率至关重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Influence of Low-Grade Solid Potash Mineral Composition on Potassium Extraction and Lithium Distribution During Solution Mining in Mahai Salt Lake, Qaidam Basin

Influence of Low-Grade Solid Potash Mineral Composition on Potassium Extraction and Lithium Distribution During Solution Mining in Mahai Salt Lake, Qaidam Basin

As high-grade potash resources become increasingly scarce and lithium is recognised as a valuable co-product, the low-grade solid potash deposits in the Mahai Salt Lake, Qaidam Basin, have become increasingly significant targets for potash resource development. However, the inefficient release of potassium from these low-grade ores constrains their economic feasibility for industrial use. This study addresses this challenge by employing x-ray diffraction (XRD), scanning electron microscopy coupled with energy dispersive spectroscopy (SEM-EDS), and observational borehole monitoring data to systematically analyse the mineralogical characteristics of these ores and their influence on potassium ion release during solid–liquid conversion. The results identify carnallite, sylvite, and polyhalite as the primary potash minerals, with a significant spatial variations across the study area that directly impact potassium ion release and migration. Sylvite and carnallite in shallow strata are more reactive with solvents, facilitating rapid potassium ion release, whereas polyhalite, hosted within the intercrystalline clastic materials of halite, demonstrates limited pore connectivity, resulting in a slower release rate. Monitoring borehole data indicate that variations in solvent injection volumes cause significant fluctuations in water levels and potassium ion concentrations, thereby affecting potash dissolution rates. As solution mining progresses, high-lithium areas gradually expand, with lithium concentrations in brine reaching up to 120.4 mg/L and generally ranging from 20 to 70 mg/L. The spatial correlation between potassium and lithium distribution suggests that lithium can be effectively recovered as a co-product. Adjustments in solvent injection rates and concentrations, based on mineral distribution and monitoring data, are essential for optimising the dissolution efficiency of both potassium and lithium during production.

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来源期刊
Geological Journal
Geological Journal 地学-地球科学综合
CiteScore
4.20
自引率
11.10%
发文量
269
审稿时长
3 months
期刊介绍: In recent years there has been a growth of specialist journals within geological sciences. Nevertheless, there is an important role for a journal of an interdisciplinary kind. Traditionally, GEOLOGICAL JOURNAL has been such a journal and continues in its aim of promoting interest in all branches of the Geological Sciences, through publication of original research papers and review articles. The journal publishes Special Issues with a common theme or regional coverage e.g. Chinese Dinosaurs; Tectonics of the Eastern Mediterranean, Triassic basins of the Central and North Atlantic Borderlands). These are extensively cited. The Journal has a particular interest in publishing papers on regional case studies from any global locality which have conclusions of general interest. Such papers may emphasize aspects across the full spectrum of geological sciences.
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