Abstract
The crystal structure of calcium oxalate trihydrate, grown on whitlockite by reaction with oxalic acid, was determined utilizing 697 independent reflections and converged to R = 0.034. Important parameters are triclinic space group P1, a 7.145(6), b 8.600(7), c 6.099(5), α 112.30(5), β 108.87(5), γ 89.92(5), with 2Ca(H2O)3(C2O4) in the unit cell.
The structure is based on dimers of edge-linked square antiprisms of composition where ϕ = oxygen ligand which is linked to oxalate groups or water molecules to form a sheet parallel to {100}. In weddellite, square antiprisms link to form a chain and in whewellite a related polyhedron of order 8 links to form sheet. It is not topologically possible to construct the series of structures by condensation of polyhedra alone since in each case some rearrangement of the water molecules is necessary.