Lead and Bismuth Chalcogenide Systems Hurr.Lnc Lru, Luxn L. Y. CH
American Mineralogist, Volume 79, pages 1159-l 166, 1994 Lead and bismuth chalcogenide systems Hurr.lNc Lru, Luxn L. Y. CH,c.Nc Department of Geology, University of Maryland, College Park, Maryland2O742,U-5.4. Ansrnlcr Phaserelations in the systemsof lead and bismuth chalcogenideswere examined in the temperature range of 500-900 "C. In the system PbS-PbSe-BirSr-BirSer,a complete series of solid solutions exists between PbnBioS,,(heyrovskyite) and PbnBioSe,r,whereas along the join from Pb.BiuS,,(lillanite) to PbrBiuSe,,there are two terminal solid solutions. The join PbBirSo-PbBirSeois characterizedby an extensivesolid solution basedon weibullite. Six extensive ranges of solid solution exist in the system PbSe-PbTe-BirSer-BirTer,and their compositionsfall along the joins in Pb(Se,Te):Bir(Se,Te),ratios of l:0, 2.7:1, 2:I, l:1, l:2, and0: I . New phasesand solid solutions in the systemsof lead and bismuth sulfide and telluride and selenide and telluride are all structurally related, and their structures are based on stacked layers of PbTe (two layers) and BirTe, (five layers). The total number of layers (N) in the unit cell of a phase, mPbTe'nBirTer, is expressedby the equation N : Z(2m * 5n), where Z is the number of formula units in the unit cell and can only be derived from experimental data. For the four phasesalong the galena-tetradymitejoin in the PbS- PbTe-BirSr-BirTe, system, PbrBirSrTer, PbrBioSrTeo,PbBirSrTer, -and PbBinS'Teohave N, Z, a, and c-respectively:9, l, q.2l x, and ft.j1 A;32,2,4.23 A, and 60.00A;21,3, 4.8 A.
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