Single-crystal X-ray diffraction was used to investigate the phase was referred to as the "2110" phase by Muller et al. 6 and structure of the ternary oxide of approximate formula Suzuki et al. 7 and as the "8250" phase by Hong et al. 8 Roth Bi 14 (Sr,Ca) 12 O 33 . The crystal examined was found to have et al. 1 designated this phase as Bi 14 Sr 6Ϫx Ca 6ϩx O 33 and charactera composition Bi 2 Sr 0.68 Ca 1.07 O 4.75 or Bi 16 Sr 5.44 Ca 8.56 O 38 as a ized it as a ternary oxide solid solution occurring at a composiresult of refinement. It crystallizes in the monoclinic space tion containing just over 50 mol% 1 2 Bi 2 O 3 and ranging from group (C2/m), with cell parameters a ؍ 21.764 (4) Å , b ؍ approximately 20 mol% CaO:25 mol% SrO to 40 mol% CaO: 4.3850 (13) Å , c ؍ 12.905 (3) Å ,  ؍ 102.72 (2)؇, and V 8 mol% SrO.In the quarternary oxide system Bi-Sr-Ca-Cu-O 1201.2 (5) Å 3 . Strontium and calcium ions were found to (BSCCO), this phase was found to be in equilibrium with the substitute for each other. The structure consists of a nettwo-layer 80 K high T c "2212" phase and also with the onework of alkaline-earth oxide polyhedra with broad channels layer "11905" phase. 6,9 Therefore, information on the phase parallel to the b axis, in which the bismuth ions reside. Two relationships of this solid solution series is important for mateout of four crystallographically distinct Bi ions form infinite rial characterization during processing of the superconducting
Bi-O zigzag ribbons of edge-linked Bi-O units, while each phases. of the other two form oxygen corner-shared Bi-O chainsThe unit cell and symmetry of a single crystal of one solid along b. The lone pair electrons of the Bi ions point toward solution member, approximately Bi 14 Sr 6 Ca 6 O 33 , was previously each other in the channels.obtained by Roth et al. 1 in 1990 by precession photography.The crystal system was found to be monoclinic with a space group, Cm or C2/m. However, no crystal structure was I. Introduction determined.T HE ternary oxide of approximate formula Bi 14 (Sr,Ca) 12 O 33 As crystal structure is important for phase equilibria and also in the Bi-Sr-Ca-O system was first described by Roth for understanding the physical properties of materials, the goal et al. 1,2 (Fig. 1) and also by Burton et al. 3 and Rawn et al. 4,5 This of this investigation, as part of a continuing study of the phase equilibria of the Bi-Sr-Ca-Cu-O system, is to report the structure and an estimation of the true composition of this Bi-SrRobert L. Snyder-contributing editor Ca-O phase. Also, recent studies of bismuth alkaline-earth oxide in the Bi-Sr-Ca-Cu-O system have described unusual bonding of