Encyclopedia of Crystallographic Prototypes

AFLOW Prototype: AB3C4_cP8_215_a_c_e-001

This structure originally had the label AB3C4_cP8_215_a_c_e. Calls to that address will be redirected here.

If you are using this page, please cite:
M. J. Mehl, D. Hicks, C. Toher, O. Levy, R. M. Hanson, G. L. W. Hart, and S. Curtarolo, The AFLOW Library of Crystallographic Prototypes: Part 1, Comp. Mat. Sci. 136, S1-S828 (2017). (doi=10.1016/j.commatsci.2017.01.017)

Links to this page

https://aflow.org/p/31D9
or https://aflow.org/p/AB3C4_cP8_215_a_c_e-001
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Cubic Lazarevićite (AsCu$_{3}$S$_{4}$) Structure: AB3C4_cP8_215_a_c_e-001

Picture of Structure; Click for Big Picture
Prototype AsCu$_{3}$S$_{4}$
AFLOW prototype label AB3C4_cP8_215_a_c_e-001
Mineral name lazarevićite
ICSD 42516
Pearson symbol cP8
Space group number 215
Space group symbol $P\overline{4}3m$
AFLOW prototype command aflow --proto=AB3C4_cP8_215_a_c_e-001
--params=$a, \allowbreak x_{3}$

  • This structure is very similar to sulvanite ($H2_{4}$), except that in this case the copper atoms are on the cubic faces [the (3c) sites] rather than the cubic edges [the (3d) sites]. The actual composition of the sample under study is Cu$_{3}$(As$_{0.65}$Cu$_{0.20}$Fe$_{0.13}$)S$_{4}$. We will ignore the alloying on the arsenic site here.
  • (Sclar, 1960) set $x_{3} = 1/4$, but that is not required by symmetry and there is undoubtedly some relaxation.
  • After much searching we finally obtained the original article for this structure from the Internet Archive. We thank them for making these documents available.

\[ \begin{array}{ccc} \mathbf{a_{1}}&=&a \,\mathbf{\hat{x}}\\\mathbf{a_{2}}&=&a \,\mathbf{\hat{y}}\\\mathbf{a_{3}}&=&a \,\mathbf{\hat{z}} \end{array}\]

Basis vectors

Lattice coordinates Cartesian coordinates Wyckoff position Atom type
$\mathbf{B_{1}}$ = $0$ = $0$ (1a) As I
$\mathbf{B_{2}}$ = $\frac{1}{2} \, \mathbf{a}_{2}+\frac{1}{2} \, \mathbf{a}_{3}$ = $\frac{1}{2}a \,\mathbf{\hat{y}}+\frac{1}{2}a \,\mathbf{\hat{z}}$ (3c) Cu I
$\mathbf{B_{3}}$ = $\frac{1}{2} \, \mathbf{a}_{1}+\frac{1}{2} \, \mathbf{a}_{3}$ = $\frac{1}{2}a \,\mathbf{\hat{x}}+\frac{1}{2}a \,\mathbf{\hat{z}}$ (3c) Cu I
$\mathbf{B_{4}}$ = $\frac{1}{2} \, \mathbf{a}_{1}+\frac{1}{2} \, \mathbf{a}_{2}$ = $\frac{1}{2}a \,\mathbf{\hat{x}}+\frac{1}{2}a \,\mathbf{\hat{y}}$ (3c) Cu I
$\mathbf{B_{5}}$ = $x_{3} \, \mathbf{a}_{1}+x_{3} \, \mathbf{a}_{2}+x_{3} \, \mathbf{a}_{3}$ = $a x_{3} \,\mathbf{\hat{x}}+a x_{3} \,\mathbf{\hat{y}}+a x_{3} \,\mathbf{\hat{z}}$ (4e) S I
$\mathbf{B_{6}}$ = $- x_{3} \, \mathbf{a}_{1}- x_{3} \, \mathbf{a}_{2}+x_{3} \, \mathbf{a}_{3}$ = $- a x_{3} \,\mathbf{\hat{x}}- a x_{3} \,\mathbf{\hat{y}}+a x_{3} \,\mathbf{\hat{z}}$ (4e) S I
$\mathbf{B_{7}}$ = $- x_{3} \, \mathbf{a}_{1}+x_{3} \, \mathbf{a}_{2}- x_{3} \, \mathbf{a}_{3}$ = $- a x_{3} \,\mathbf{\hat{x}}+a x_{3} \,\mathbf{\hat{y}}- a x_{3} \,\mathbf{\hat{z}}$ (4e) S I
$\mathbf{B_{8}}$ = $x_{3} \, \mathbf{a}_{1}- x_{3} \, \mathbf{a}_{2}- x_{3} \, \mathbf{a}_{3}$ = $a x_{3} \,\mathbf{\hat{x}}- a x_{3} \,\mathbf{\hat{y}}- a x_{3} \,\mathbf{\hat{z}}$ (4e) S I

References

  • C. B. Sclar and M. Drovenik, Lazarevićite, A New Cubic Copper-Arsenic Sulfied from Bor, Jugoslavia, Bull. Geo. Soc. Am. 71, 1970 (1960).
  • M. Fleischer, New Mineral Names, Am. Mineral. 46, 464–468 (1961).
  • P. Villars, K. Cenzual, J. Daams, R. Gladyshevskii, O. Shcherban, V. Dubenskyy, N. Melnichenko-Koblyuk, O. Pavlyuk, S. Stoiko, and L. Sysa, Structure Types. Part 2: Space Groups (218) P-43n - (195) P23 $\cdot$ Cu$_{3}$AsS$_{4}$ (2005), doi:10.1007/10920473_223. Springer-Verlag Berlin Heidelberg.

Found in

  • P. Villars and L. Calvert, Pearson's Handbook of Crystallographic Data for Intermetallic Phases (ASM International, Materials Park, OH, 1991), 2nd edn.

Prototype Generator

aflow --proto=AB3C4_cP8_215_a_c_e --params=$a,x_{3}$

Species:

Running:

Output: