Electronic structure and flotation behavior of monoclinic and hexagonal pyrrhotite
Electronic structures of monoclinic and hexagonal pyrrhotite were studied using density functional theory method, together with their flotation behavior. The main contribution of monoclinic pyrrhotite is mainly from Fe 3d, while that of hexagonal pyrrhotite is from Fe 3d, Fe 3p and S 3s. The hexagon...
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| Published in | Journal of Central South University Vol. 22; no. 2; pp. 466 - 471 |
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| Main Authors | , , |
| Format | Journal Article |
| Language | English |
| Published |
Heidelberg
Central South University
01.02.2015
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| Subjects | |
| Online Access | Get full text |
| ISSN | 2095-2899 2227-5223 |
| DOI | 10.1007/s11771-015-2544-4 |
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| Abstract | Electronic structures of monoclinic and hexagonal pyrrhotite were studied using density functional theory method, together with their flotation behavior. The main contribution of monoclinic pyrrhotite is mainly from Fe 3d, while that of hexagonal pyrrhotite is from Fe 3d, Fe 3p and S 3s. The hexagonal pyrrhotite is more reactive than monoclinic pyrrhotite because of large density of states near the Fermi level. The hexagonal pyrrhotite shows antiferromagnetism. S—Fe bonds mainly exist in monoclinic pyrrhotite as the covalent bonds, while hexagonal pyrrhotite has no covalency. The main contributions of higest occupied molecular orbital (HOMO) and lowest unoccupied molecular obital (LUMO) for monoclinic pyrrhotite come from S and Fe. The main contribution of HOMO for hexagonal pyrrhotite comes from Fe, while that of LUMO comes from S. The coefficient of Fe atom is much larger than that of S atom of HOMO for hexagonal pyrrhotite, which contributes to the adsorption of CaOH
+
on the surface of hexagonal pyrrhotite when there is lime. As a result, lime has the inhibitory effect on the floatation of hexagonal pyrrhotite and the coefficient of Fe is very close to that of S for monoclinic pyrrhotite. Therefore, the existence of S prevents the adsorption of CaOH
+
on the surface of monoclinic pyrrhotite, which leads to less inhibitory effect on the flotation of monoclinic pyrrhotite. |
|---|---|
| AbstractList | Electronic structures of monoclinic and hexagonal pyrrhotite were studied using density functional theory method, together with their flotation behavior. The main contribution of monoclinic pyrrhotite is mainly from Fe 3d, while that of hexagonal pyrrhotite is from Fe 3d, Fe 3p and S 3s. The hexagonal pyrrhotite is more reactive than monoclinic pyrrhotite because of large density of states near the Fermi level. The hexagonal pyrrhotite shows antiferromagnetism. S—Fe bonds mainly exist in monoclinic pyrrhotite as the covalent bonds, while hexagonal pyrrhotite has no covalency. The main contributions of higest occupied molecular orbital (HOMO) and lowest unoccupied molecular obital (LUMO) for monoclinic pyrrhotite come from S and Fe. The main contribution of HOMO for hexagonal pyrrhotite comes from Fe, while that of LUMO comes from S. The coefficient of Fe atom is much larger than that of S atom of HOMO for hexagonal pyrrhotite, which contributes to the adsorption of CaOH
+
on the surface of hexagonal pyrrhotite when there is lime. As a result, lime has the inhibitory effect on the floatation of hexagonal pyrrhotite and the coefficient of Fe is very close to that of S for monoclinic pyrrhotite. Therefore, the existence of S prevents the adsorption of CaOH
+
on the surface of monoclinic pyrrhotite, which leads to less inhibitory effect on the flotation of monoclinic pyrrhotite. |
| Author | Zhao, Cui-hua Wu, Bo-zeng Chen, Jian-hua |
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| Cites_doi | 10.1127/ejm/2/4/0525 10.1016/S0016-7037(00)00503-2 10.1179/000844311X552269 10.1103/RevModPhys.64.1045 10.1016/S0016-7037(99)00421-4 10.1016/S0892-6875(00)00098-4 10.1103/PhysRevB.45.13244 10.1103/PhysRevB.41.7892 10.1016/S0039-6028(97)00370-1 |
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| Keywords | monoclinic pyrrhotite flotation behavior hexagonal pyrrhotite electronic structure density functional theory |
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| References_xml | – reference: HeM FQinW QLizW ZChenY JLaiC HResearch on flotation performances of polymorphic pyrrhotite [C]24th International Mineral Processing Congress2008BeijingScience Press11531160 – reference: BeckerMBradshawDDe VilliersJThe mineralogy of pyrrhotite from Sudbury CCN and Phoenix nickel ores and its effect on flotation performance [J]Canadian Metallurgical Quarterly2011501101910.1179/000844311X552269 – reference: HongQ YTangY HWangY HLiangD YYuL XInvestigation on properties and structure of pyrrhotite and the difference of its floatability [J]Metal Mine20114016467 – reference: LawsonVKerrA NShieldsYWellsP FXuMDaiZImproving pentlandite pyrrhotite separation at INCO’s Clarabelle Mill [C]Centenary of Flotation Symposium2005Brisbane, AustraliaAusIMM Brisbane875885 – reference: WardJ CThe structure and properties of some iron sulphides [J]Rev Pur Appl Chem197020175206 – reference: BeckerUHunzA WThorntonGVaughanD JThe atomic and electronic structure of the (001) surface of monoclinic pyrrhotite (Fe7S8) as studied using STM, LEED and quantum mechanical calculations [J]Surf Sci1997389668710.1016/S0039-6028(97)00370-1 – reference: WellsP FKelebekSBurrowsM JSuarezD FFinchJ ARaoS RHolubecIPyrrhotite rejection at Falconbridge’s Strathcona Mill [C]Processing of Complex Ores: Mineral Processing and the Environment1997MontrealCIM5162 – reference: PayneM CTeterM PAllanD CAriasT AJoannopoulosJ DIterative minimization techniques for ab initio total energy calculations: molecular dynamics and conjugate gradients [J]Reviews of Modern Physics1992641045109710.1103/RevModPhys.64.1045 – reference: KalahdoozanMAdsorption and flotation characteristics of hexagonal and monoclinic pyrrhotite [D]1996Brisbane, AustraliaQueens University – reference: ThomasJ ESmartR S CSkinnerW MKinetics factors for oxidative and non-oxidative dissolution of iron sulfides [J]Min Eng200010–111149115910.1016/S0892-6875(00)00098-4 – reference: JanzenM PNicholsonR VScharerJ MPyrrhotite reaction kinetics: Reaction rates for oxidation by oxygen, ferric iron, and for nonoxidative dissolution [J]Geochim Cosmochim Acta20006491511152210.1016/S0016-7037(99)00421-4 – reference: ThomasJ ESkinnerW MSt SmartR CA mechanism to explain sudden changes in rates and products for pyrrhotite dissolution in acide solution, Geochim [J]Cosmochim Acta200165111210.1016/S0016-7037(00)00503-2 – reference: ProfsaiMDodonayIPyrrhotite superstructures: Part I. Fundamentals structures of the NC (N=2, 3, 4 and 5) type [J]Eur J Mineral1990252552810.1127/ejm/2/4/0525 – reference: PerdewJ PWangYAccurate and simple analytic representation of the electron-gas correlation energy [J]Phys Rev B199245132441324910.1103/PhysRevB.45.13244 – reference: OriovaT AStupnikowV MKrestanA LMechanism of oxidative dissolution of sulphides [J]Zhurnal Prikladnoi Khimii19896121722177 – reference: VaughanD JCraigJ RMineral chemistry of metal sulphides [M]1978Cambridge, UKCambridge University. Press493 – reference: GersonAJasieniakMThe effect of surface oxidation on the Cu activation of pentlandite and pyrrhotite [C]24th International Mineral Processing Congress2008BeijingScience Press10541063 – reference: VanderbiltDSoft self-consistent pseudopotentials in a generalized eigenvalue formalism [J]Phys Rev B1990417892789510.1103/PhysRevB.41.7892 – volume: 2 start-page: 525 year: 1990 ident: 2544_CR2 publication-title: Eur J Mineral doi: 10.1127/ejm/2/4/0525 – volume: 65 start-page: 1 issue: 1 year: 2001 ident: 2544_CR4 publication-title: Cosmochim Acta doi: 10.1016/S0016-7037(00)00503-2 – volume-title: Adsorption and flotation characteristics of hexagonal and monoclinic pyrrhotite [D] year: 1996 ident: 2544_CR10 – volume: 50 start-page: 10 issue: 1 year: 2011 ident: 2544_CR8 publication-title: Canadian Metallurgical Quarterly doi: 10.1179/000844311X552269 – volume: 20 start-page: 175 year: 1970 ident: 2544_CR18 publication-title: Rev Pur Appl Chem – volume: 64 start-page: 1045 year: 1992 ident: 2544_CR15 publication-title: Reviews of Modern Physics doi: 10.1103/RevModPhys.64.1045 – start-page: 493 volume-title: Mineral chemistry of metal sulphides [M] year: 1978 ident: 2544_CR1 – start-page: 1153 volume-title: 24th International Mineral Processing Congress year: 2008 ident: 2544_CR11 – start-page: 51 volume-title: Processing of Complex Ores: Mineral Processing and the Environment year: 1997 ident: 2544_CR13 – volume: 40 start-page: 64 issue: 1 year: 2011 ident: 2544_CR9 publication-title: Metal Mine – volume: 64 start-page: 1511 issue: 9 year: 2000 ident: 2544_CR5 publication-title: Geochim Cosmochim Acta doi: 10.1016/S0016-7037(99)00421-4 – volume: 10–11 start-page: 1149 year: 2000 ident: 2544_CR3 publication-title: Min Eng doi: 10.1016/S0892-6875(00)00098-4 – volume: 61 start-page: 2172 year: 1989 ident: 2544_CR6 publication-title: Zhurnal Prikladnoi Khimii – volume: 45 start-page: 13244 year: 1992 ident: 2544_CR16 publication-title: Phys Rev B doi: 10.1103/PhysRevB.45.13244 – volume: 41 start-page: 7892 year: 1990 ident: 2544_CR17 publication-title: Phys Rev B doi: 10.1103/PhysRevB.41.7892 – start-page: 1054 volume-title: 24th International Mineral Processing Congress year: 2008 ident: 2544_CR14 – volume: 389 start-page: 66 year: 1997 ident: 2544_CR7 publication-title: Surf Sci doi: 10.1016/S0039-6028(97)00370-1 – start-page: 875 volume-title: Centenary of Flotation Symposium year: 2005 ident: 2544_CR12 |
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| Title | Electronic structure and flotation behavior of monoclinic and hexagonal pyrrhotite |
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