data_global _chemical_name_mineral 'Plumbogummite' loop_ _publ_author_name 'Kolitsch U' 'Tiekink E R T' 'Slade P G' 'Taylor M R' 'Pring A' _journal_name_full 'European Journal of Mineralogy' _journal_volume 11 _journal_year 1999 _journal_page_first 513 _journal_page_last 520 _publ_section_title ; Hinsdalite and plumbogummite, their atomic arrangements and disordered lead sites ; _database_code_amcsd 0006790 _chemical_formula_sum 'Pb Al3 (P1.9 As.1) O14 H6' _cell_length_a 7.039 _cell_length_b 7.039 _cell_length_c 16.761 _cell_angle_alpha 90 _cell_angle_beta 90 _cell_angle_gamma 120 _cell_volume 719.205 _exptl_crystal_density_diffrn 4.049 _symmetry_space_group_name_H-M 'R -3 m' loop_ _space_group_symop_operation_xyz 'x,y,z' '2/3+x,1/3+y,1/3+z' '1/3+x,2/3+y,2/3+z' 'x,x-y,z' '2/3+x,1/3+x-y,1/3+z' '1/3+x,2/3+x-y,2/3+z' 'y,x,-z' '2/3+y,1/3+x,1/3-z' '1/3+y,2/3+x,2/3-z' '-x+y,y,z' '2/3-x+y,1/3+y,1/3+z' '1/3-x+y,2/3+y,2/3+z' '-x,-x+y,-z' '2/3-x,1/3-x+y,1/3-z' '1/3-x,2/3-x+y,2/3-z' '-y,-x,z' '2/3-y,1/3-x,1/3+z' '1/3-y,2/3-x,2/3+z' 'x-y,-y,-z' '2/3+x-y,1/3-y,1/3-z' '1/3+x-y,2/3-y,2/3-z' 'y,-x+y,-z' '2/3+y,1/3-x+y,1/3-z' '1/3+y,2/3-x+y,2/3-z' '-x+y,-x,z' '2/3-x+y,1/3-x,1/3+z' '1/3-x+y,2/3-x,2/3+z' '-x,-y,-z' '2/3-x,1/3-y,1/3-z' '1/3-x,2/3-y,2/3-z' '-y,x-y,z' '2/3-y,1/3+x-y,1/3+z' '1/3-y,2/3+x-y,2/3+z' 'x-y,x,-z' '2/3+x-y,1/3+x,1/3-z' '1/3+x-y,2/3+x,2/3-z' loop_ _atom_site_label _atom_site_fract_x _atom_site_fract_y _atom_site_fract_z _atom_site_occupancy _atom_site_U_iso_or_equiv Pb 0.04090 0.04090 0.00000 0.16667 0.02530 Al 0.50000 0.00000 0.50000 1.00000 0.00730 P 0.00000 0.00000 0.31002 0.95000 0.01180 As 0.00000 0.00000 0.31002 0.05000 0.01180 O1 0.00000 0.00000 0.59830 1.00000 0.01700 O2 0.21420 -0.21420 -0.05740 1.00000 0.01640 O-H3 0.12600 -0.12600 0.13753 1.00000 0.01300 loop_ _atom_site_aniso_label _atom_site_aniso_U_11 _atom_site_aniso_U_22 _atom_site_aniso_U_33 _atom_site_aniso_U_12 _atom_site_aniso_U_13 _atom_site_aniso_U_23 Pb 0.03110 0.03110 0.02010 0.02040 -0.00180 0.00180 Al 0.00500 0.00540 0.01170 0.00270 0.00020 0.00030 P 0.01030 0.01030 0.01490 0.00510 0.00000 0.00000 As 0.01030 0.01030 0.01490 0.00510 0.00000 0.00000