2018
DOI: 10.1016/j.seppur.2018.06.012
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Effect of coexisting ions on recovering lithium from high Mg2+/Li+ ratio brines by selective-electrodialysis

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Cited by 105 publications
(33 citation statements)
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“…Electrodialysis equipped with monovalent selective ion exchange membranes (IEM), called selective-electrodialysis (S-ED), has recently been proposed to overcome the aforementioned issues via direct lithium extraction without the use of any extractants or adsorbents. 35–37 Monovalent cations (Li + , Na + , K + ) preferentially migrate through the monovalent selective cation exchange membranes while divalent cations (Mg 2+ , Ca 2+ ) are blocked, allowing selective lithium recovery from high Mg 2+ /Li + ratio brines. S-ED is regarded as a very promising emerging technology due to its high energy efficiency, applicability to high-salinity brine, and eco-friendliness.…”
Section: Introductionmentioning
confidence: 99%
“…Electrodialysis equipped with monovalent selective ion exchange membranes (IEM), called selective-electrodialysis (S-ED), has recently been proposed to overcome the aforementioned issues via direct lithium extraction without the use of any extractants or adsorbents. 35–37 Monovalent cations (Li + , Na + , K + ) preferentially migrate through the monovalent selective cation exchange membranes while divalent cations (Mg 2+ , Ca 2+ ) are blocked, allowing selective lithium recovery from high Mg 2+ /Li + ratio brines. S-ED is regarded as a very promising emerging technology due to its high energy efficiency, applicability to high-salinity brine, and eco-friendliness.…”
Section: Introductionmentioning
confidence: 99%
“…Lithium resources can be divided into either primary or secondary sources. Primary sources include mineral rocks [ 3 ], saline lakes [ 4 ], brines [ 5 ], sea water [ 6 ], underground water [ 7 ], and groundwater [ 8 ], while secondary sources are typically lithium obtained from recycling lithium-containing devices and components, such as batteries, capacitors [ 9 ], or general e-wastes [ 10 ]. The world’s primary reserves of lithium are estimated at over 250 billion tons [ 1 ], of which 230 billion tons are present within oceans, while the remaining amount exists as ores or continental brines.…”
Section: Introductionmentioning
confidence: 99%
“…The recovery of lithium from a different kind of natural brines such as geothermal brine is complicated by high water salinity 200–500 g/L and the presence of hardness ions, especially magnesium ions [ 13 , 14 ]. Li + and Mg 2+ ions have very similar size of 0.076 and 0.075 nm, respectively, which requires additional efforts and processing steps in the case of a high Mg 2+ /Li + ratio [ 15 , 16 ]. Among different methods of lithium recovery (e.g., extraction, crystallization, precipitation, ion-exchange adsorption, electrodialysis), extraction and ionic adsorption are most widely used due to their high selectivity [ 10 , 17 , 18 , 19 , 20 , 21 , 22 , 23 , 24 ].…”
Section: Introductionmentioning
confidence: 99%