2023
DOI: 10.1016/j.jclepro.2023.138968
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A new method for pre-enrichment of gallium and lithium based on mode of occurrence in coal gangue from Antaibao surface mine, Shanxi Province, China

Shiqi Dai,
Fengshuai Sun,
Lei Wang
et al.
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Cited by 10 publications
(3 citation statements)
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“…CG is a prevalent CSWM that generally comprises soil-like constituents, including silicates, oxides, and carbonates [51,52], in addition to substantial quantities of organic matter, N, P, and K. CG is an acidic mineral, and as the amount of CH increases, the EC and pH values decrease. The particle size of coal gangue is relatively large, so the field capacity and porosity of the AS exhibit a decline as the CG content increases.…”
Section: Discussionmentioning
confidence: 99%
“…CG is a prevalent CSWM that generally comprises soil-like constituents, including silicates, oxides, and carbonates [51,52], in addition to substantial quantities of organic matter, N, P, and K. CG is an acidic mineral, and as the amount of CH increases, the EC and pH values decrease. The particle size of coal gangue is relatively large, so the field capacity and porosity of the AS exhibit a decline as the CG content increases.…”
Section: Discussionmentioning
confidence: 99%
“…The demand for Li and Ga has been increasing dramatically in recent years with the widespread use of strategic metals, but the current supply of Li and Ga is limited due to the high cost of mining and low abundance, which has led to the need to try to recover Li and Ga from different substances. It is found that the contents of Li and Ga in CG are abnormally high; therefore, the recovery of Li and Ga from CG provides a new way for the comprehensive utilization of CG. , In order to achieve the maximum utilization of Li and Ga in the CG, the occurrence mode of Li and Ga in coal and its byproducts has been studied. The study of the coal in the Urinary Basin found that 96.6–99.4% of Li existed in the form of silicates and aluminosilicates, and it was speculated that Li may exist in Illite and kaolinite . In the coal of Pingshuo, the contents of Li and Ga in the inorganic components were significantly higher than those in the organic components, and the main contents of Li and Ga were in the silicates of coal samples .…”
Section: Introductionmentioning
confidence: 99%
“… 12 14 It is found that the contents of Li and Ga in CG are abnormally high; therefore, the recovery of Li and Ga from CG provides a new way for the comprehensive utilization of CG. 15 , 16 In order to achieve the maximum utilization of Li and Ga in the CG, the occurrence mode of Li and Ga in coal and its byproducts has been studied. 17 19 The study of the coal in the Urinary Basin found that 96.6–99.4% of Li existed in the form of silicates and aluminosilicates, and it was speculated that Li may exist in Illite and kaolinite.…”
Section: Introductionmentioning
confidence: 99%