The crystal structure of the carnotite-type compound Ba 2 [(UO 2) 2 Ti 2 O 8 ] has been determined by ab initio methods from synchrotron X-ray and neutron powder-diffraction data. We describe the first reported structure of a uranyl titanate; it was solved in the monoclinic space-group P2 1 /c and has the lattice parameters a 6.4463(1), b 8.5999(1), c 10.2532(1) Å, b 75.936(1)°, V 551.36(1) Å 3 , D calc 6.253 g/cm 3 and Z = 4. A multiple histogram approach was used to refine the structure from synchrotron and neutron-diffraction data, giving quality factors of R B 0.032 and 0.039, R wp 0.090 and 0.063, and R p 0.070 and 0.049, respectively. The compound forms a layered structure in which sheets of uranyl pentagonal bipyramids share edges with dimers of TiO 5 square pyramids. These are separated by layers of 11-fold-coordinated barium atoms. Because of the potential presence of Ba 2 [(UO 2) 2 Ti 2 O 8 ] in ceramic waste-forms for the immobilization of radioactive wastes, the leach rate of uranium and barium were determined. The normalized rates of leaching from Ba 2 [(UO 2) 2 Ti 2 O 8 ], averaged over seven days, are 1.3 3 10-5 g/m 2 /day for uranium, a significantly lower rate than that observed from pyrochlore waste-forms, and 1 3 10-4 g/m 2 /day for barium. Keywords: Ba 2 [(UO 2) 2 Ti 2 O 8 ], crystal structure, uranyl titanate waste-form, synchrotron data, neutron-diffraction data, powder diffraction.