Electronic structure and flotability of gold-bearing pyrite: A density functional theory study

Dan Liu , Yi-jie Wang , Yong-jun Xian , Shu-ming Wen

Journal of Central South University ›› 2017, Vol. 24 ›› Issue (10) : 2288 -2293.

PDF
Journal of Central South University ›› 2017, Vol. 24 ›› Issue (10) : 2288 -2293. DOI: 10.1007/s11771-017-3640-4
Article

Electronic structure and flotability of gold-bearing pyrite: A density functional theory study

Author information +
History +
PDF

Abstract

Various incorporation of Au in pyrite and its effects on the geometrical structure, electronic structure and flotability of pyrite were theoretically investigated and fully discussed by performing density functional theory (DFT). The calculated incorporation energy shows that gold would most likely exist in pyrite via incorporating into interstitial lattice sites in the absence of As impurity. As a result of incorporated Au, the covalence levels of the S—Fe and S—S bonds are changed, and the tonicity of Au—S bonds and antibonding of Au—Fe bonds are found to form in the pyrite, which would change the natural flotability of pyrite. The Au impurity energy levels are introduced into the energy band and result in the transformation of pyrite semiconductivity type. The calculated band-gap value suggests that the incorporated Au significantly decreases pyrite semiconductivity level, which enhances the formation and the adsorption stability of dixanthogen during pyrite flotation. The DOS results reveal that the stability and depression difficulty level of pyrites increases in the following order: Fe32S63As < Fe32S64 < Fe32S63AsAu < Fe32S64Au.

Keywords

pyrite / gold / density functional theory / electronic structure / flotability

Cite this article

Download citation ▾
Dan Liu, Yi-jie Wang, Yong-jun Xian, Shu-ming Wen. Electronic structure and flotability of gold-bearing pyrite: A density functional theory study. Journal of Central South University, 2017, 24(10): 2288-2293 DOI:10.1007/s11771-017-3640-4

登录浏览全文

4963

注册一个新账户 忘记密码

References

[1]

GaoZ-m, YangZ-s, LiH-y, LuoT-y, YaoL-b, RaoW-bo. Genesis and characteristics of gold hosted by pyrite [J]. Geol J China Univ, 2000, 6(2): 156-162

[2]

SuW-c, XiaB, ZhangH-t, ZhangX-c, HuR-zhong. Visible gold in arsenian pyrite at the Shuiyindong Carlin-type gold deposit, Guizhou, China: Implications for the environment and processes of ore formation [J]. Ore Geology Reviews, 2008, 33(3): 667-679

[3]

HazarikaP, MishraB, ChinnasamyS S, BernhardtH J. Multi-stage growth and invisible gold distribution in pyrite from the Kundarkocha sediment-hosted gold deposit, eastern India [J]. Ore Geology Reviews, 2013, 55(4): 134-145

[4]

JhaV, SinghS, VenkateshA S. Invisible gold occurrence within the quartz reef pyrite of Babaikundi area, North Singhbhum fold-and-thrust belt, Eastern Indian Shield: Evidence from petrographic, SEM and EPMA studies [J]. Ore Geology Reviews, 2015, 65: 426-432

[5]

MillsS E, TomkinsA G, WeinbergR F, FanH-rui. Implications of pyrite geochemistry for gold mineralisation and remobilisation in the Jiaodong gold district, northeast China [J]. Ore Geology Reviews, 2015, 71: 150-168

[6]

DeditiusA P, UtsunomiyaS, ReichM, KeslerS E, EwingR C, HoughR, WelsheJ. Trace metal nanoparticles in pyrite [J]. Ore Geology Reviews, 2011, 42(1): 32-46

[7]

HoughR, ReichM. Noble metal nanoparticles in ore systems [J]. Ore Geology Reviews, 2011, 42: 55-60

[8]

PalenikC S, UtsunomiyaS, ReichM, KeslerS E, WangL M, EwingR C. “Invisible” gold revealed: Direct imaging of gold nanoparticles in a Carlin-type deposit [J]. Am Mineral, 2004, 89(10): 1359-1366

[9]

WeiJ-h, TanW-j, GuoD-z, TanJ, LiY-h, YanY-fei. Isotope systematics and metallogenetic age of Zhuanghe gold deposit, Liaoning province [J]. Journal of Central South University of Technology, 2007, 14(1): 104-110

[10]

SunZ-m, SunC-b, WangJ-z, YinW-zhong. Optimization and mechanism of gold-bearing sulfide flotation [J]. Rare Metals, 2014, 33(3): 363-368

[11]

PakT H, SunT-c, XuC-y, JoY H. Flotation and surface modification characteristics of galena, sphalerite and pyrite in collecting-depressing-reactivating system [J]. Journal of Central South University of Technology, 2012, 19(6): 1702-1710

[12]

GuG-h, SunX-j, LiJ-h, HuY-hua. Influences of collector DLZ on chalcopyrite and pyrite flotation [J]. Journal of Central South University of Technology, 2010, 17(2): 285-288

[13]

ZhongS-p, WuZ, HuangZ-s, RuanRenman. Oxidation kinetics reaction of gold-bearing pyrite in sulphuric acid [J]. Chin J Rare Met, 2013, 37(2): 295-301

[14]

LiuY-c, ZhuZ-s, FuJ-g, LiL-f, LinQ, LiZ-hui. Leaching gold ores by lime-sulphur-syntheticsolution with alkali-catalyzed process [J]. Chin J Rare Met, 2013, 37(1): 123-129

[15]

ReichM, KeslerS E, UtsunomiyaS, PalenikC S, ChryssoulisS L, EwingR C. Solubility of gold in arsenian pyrite [J]. Geochim Cosmochim Ac, 2005, 69(11): 2781-2796

[16]

AgangiA, HofmannA, Wohlgemuth-UeberwasserC C. Pyrite zoning as a record of mineralization in the Ventersdorp Contact Reef, Witwatersrand Basin, South Africa [J]. Econ Geol, 2013, 108(6): 1243-1272

[17]

LargeR R, MaslennikonV V, RobertF, DanyushevskyL V, ChangZ. Multistage sedimentary and metamorphic origin of pyrite and gold in the giant Sukhoi Log deposit, Lena gold province, Russia [J]. Econ Geol, 2007, 102(7): 1233-1267

[18]

LargeR R, DanyushevskyL, HollitC, MaslennikovV, MeffreS, GilbertS, BullS, ScottR, EmsboP, ThomasH. Gold and trace element zonation in pyrite using a laser imaging technique: Implications for the timing of gold in orogenic and Carlin-style sediment-hosted deposits [J]. Econ Geol, 2009, 104(5): 635-668

[19]

DeditiusA P, ReichM, KeslerS E, UtsunomiyaS, ChryssoulisS L, WalsheJ, EwingR C. The coupled geochemistry of Au and As in pyrite from hydrothermal ore deposits [J]. Geochim Cosmochim Ac, 2014, 140: 644-670

[20]

DeditiusA P, UtsunomiyaS, RenockD, EwingR C, RamanaC V, BeckerU, KeserS E. A proposed new type of arsenian pyrite: Composition, nanostructure and geological significance [J]. Geochim Cosmochim Ac, 2008, 72(12): 2919-2933

[21]

BlanchardM, AlfredssonM, BrodholtJ, WrightK, CatlowC. Arsenic incorporation into FeS2 pyrite and its influence on dissolution: A DFT study [J]. Geochim Cosmochim Ac, 2007, 71(3): 624-630

[22]

SegallM D, LindanP, ProbertM J, PickardC, HasnipP, ClarkS, PayneM C. First-principles simulation: Ideas, illustrations and the CASTEP code [J]. J Phys: Condens Matt, 2002, 14(11): 2717-2744

[23]

KresseG, JoubertD. From ultrasoft pseudopotentials to the projector augmented-wave method [J]. Phys Rev B, 1999, 59(3): 1758-1775

[24]

PerdewJ P, BurkeK, ErnzerhofM. Generalized gradient approximation made simple [J]. Phys Rev Lett, 1996, 77(18): 3865-3868

[25]

NishidateK, YoshizawaM, HasegawaM. Energetics of Mg and B adsorption on polar zinc oxide surfaces from first principles [J]. Phys Rev B, 2008, 77(3): 035330

[26]

TommY, SchieckR, EllmerK, FiechterS. Growth mechanism and electronic properties of doped pyrite (FeS2) crystals [J]. J Crys Growth, 1995, 1461271-276

[27]

ChandraA P, GersonA R. A review of the fundamental studies of the copper activation mechanisms for selective flotation of the sulfide minerals, sphalerite and pyrite [J]. Advances in Colloid & Interface Science, 2009, 145(12): 97-110

[28]

ChenJ-h, FengQ-m, LuY-ping. Energy band model of electrochemical flotation and its application: II. Energy band model of xanthate interacting with sulphide minerals [J]. Chin J Nonferrous Met, 2000, 10: 426-429

[29]

LiQ, QinW-q, SunW, QiuG-zhou. Calculation of electron structure by density function theory and electrochemical process of surface (100) of FeS2 [J]. Journal of Central South University of Technology, 2007, 14(5): 618-622

AI Summary AI Mindmap
PDF

122

Accesses

0

Citation

Detail

Sections
Recommended

AI思维导图

/