2022
DOI: 10.1007/s40831-022-00494-z
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Reaction Behavior of Aluminogoethite and Silica Minerals in Gibbsite Bauxite in High-Temperature Digestion

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Cited by 6 publications
(2 citation statements)
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“…The source of the Fe 2+ can be different: iron [ 19 ] and aluminum [ 20 ] that reacts with the alkaline solution with the formation of H 2 and following the reduction of Fe 3+ to Fe 2+ ; the addition of FeSO 4 [ 21 , 22 ] and the addition of organic matter [ 23 ]. The presence of Fe 2+ ions also helps to decrease the amount of Na and Al that is lost with the BR, which is connected to the formation of other desilication products [ 24 ]. However, the main disadvantage of these methods is the need of a high-pressure leaching process at T > 220 °C.…”
Section: Introductionmentioning
confidence: 99%
“…The source of the Fe 2+ can be different: iron [ 19 ] and aluminum [ 20 ] that reacts with the alkaline solution with the formation of H 2 and following the reduction of Fe 3+ to Fe 2+ ; the addition of FeSO 4 [ 21 , 22 ] and the addition of organic matter [ 23 ]. The presence of Fe 2+ ions also helps to decrease the amount of Na and Al that is lost with the BR, which is connected to the formation of other desilication products [ 24 ]. However, the main disadvantage of these methods is the need of a high-pressure leaching process at T > 220 °C.…”
Section: Introductionmentioning
confidence: 99%
“…The source of the Fe 2+ can be different: iron [19] and aluminum [20] that reacts with the alkaline solution with the formation of H 2 and following the reduction of Fe 3+ to Fe 2+ ; the addition of FeSO 4 [21,22] and the addition of organic matter [23]. The presence of Fe 2+ ions also helps to decrease the amount of Na and Al that is lost with the BR, which is connected to the formation of other desilication products [24]. However, the main disadvantage of these methods is the need of a high-pressure leaching process at T > 220…”
Section: Introductionmentioning
confidence: 99%