2022
DOI: 10.1016/j.mineng.2021.107322
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Application of LA-ICP-MS to process mineralogy: Gallium and germanium recovery at Kipushi copper-zinc deposit

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Cited by 8 publications
(8 citation statements)
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“…7 The Raman spectrum is split into two fundamental modes: the longitudinal optical (LO) mode at ∼349 cm −1 (the vibrations are parallel to the exciting light) and the transverse optical (TO) mode at ∼273 cm −1 (perpendicular vibrations). 7,10,11 In terms of atom bonding, the LO mode (349 cm −1 ) was assigned to the Zn-S vibration, [7][8][9][10] while the Raman lines at 298 cm −1 were assigned to the Fe─S vibration mode, both cations being in tetrahedral coordination. 21 If the LO mode is the fundamental vibration of M─S bonds, one notices that the former shifts to wavenumbers that are lower when M═Fe and higher when M═Zn.…”
Section: Information From Xrd and Raman Spectroscopymentioning
confidence: 99%
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“…7 The Raman spectrum is split into two fundamental modes: the longitudinal optical (LO) mode at ∼349 cm −1 (the vibrations are parallel to the exciting light) and the transverse optical (TO) mode at ∼273 cm −1 (perpendicular vibrations). 7,10,11 In terms of atom bonding, the LO mode (349 cm −1 ) was assigned to the Zn-S vibration, [7][8][9][10] while the Raman lines at 298 cm −1 were assigned to the Fe─S vibration mode, both cations being in tetrahedral coordination. 21 If the LO mode is the fundamental vibration of M─S bonds, one notices that the former shifts to wavenumbers that are lower when M═Fe and higher when M═Zn.…”
Section: Information From Xrd and Raman Spectroscopymentioning
confidence: 99%
“…The first series of the method involves the dissolution of the mineral under high temperature or high‐pressure conditions, which is followed by the quantification of the target element's content based on its concentration in the resulting liquid phase. Prominent techniques of this category include chemical titration, 6 atomic absorption spectrometry (AAS), 7 inductively coupled plasma mass spectrometry (ICP‐MS), 8 and inductively coupled plasma‐optical emission spectrometer (ICP‐OES) 9 . The second series of methods relies on discerning the characteristic spectral lines generated by internal electronic transitions induced by absorbed radiation energy, which facilitates direct and swift identification of the target element content in the mineral.…”
Section: Introductionmentioning
confidence: 99%
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