This structure originally had the label A7B2C_cP40_205_bd_c_a. Calls to that address will be redirected here.
If you are using this page, please cite:
D. Hicks, M.J. Mehl, M. Esters, C. Oses, O. Levy, G.L.W. Hart, C. Toher, and S. Curtarolo, The AFLOW Library of Crystallographic Prototypes: Part 3, Comp. Mat. Sci. 199, 110450 (2021). (doi=10.1016/j.commatsci.2021.110450)
This is the high temperature form of all the structures listed. The low temperature structure depends on the composition. Below 290°C ZrP2O7 transforms to an orthorhombic structure, space group Pbca #61, with 136 unique crystallographic positions and 1080 atomic sites. See (Birkedal, 2006) and (Stinton, 2006) for more details.
G. R. Levi and G. Peyronel, Struttura Cristallografica del Gruppo Isomorfo (Si4+, Ti4+, Zr4+, Sn4+, Hf4+) P2O7, Z. Kristallogr. 92, 190–209 (1935), doi:10.1524/zkri.1935.92.1.210.
H. Birkedal, A. M. K. Andersen, A. Arakcheeva, G. Chapuis, P. Norby, and P. Pattison, The Room-Temperature Superstructure of ZrP2O7 Is Orthorhombic: There Are No Unusual 180∘ P-O-P Bond Angles, Inorg. Chem. 45, 4346–4351 (2006), doi:10.1021/ic0600174.
G. W. Stinton, M. R. Hampson, and J. S. O. Evans, The 136-Atom Structure of ZrP2O7 and HfP2O7 from Powder Diffraction Data, Inorg. Chem. 45, 4352–4358 (2006), doi:10.1021/ic060016b.
Found in
R. T. Downs and M. Hall-Wallace, The American Mineralogist Crystal Structure Database, Am. Mineral. 88, 247–250 (2003).