The compressional behavior and the P-induced deformation mechanisms at the atomic scale of (Cs,K)Al 4 Be 5 B 11 O 28 (londonite, a~7.31 A and space group P43m) were investigated by in situ single-crystal synchrotron X-ray diffraction with a diamond anvil cell up to 26 GPa. No phase transition was observed within the P-range investigated: this material exhibits isotropic compression (i.e., with cubic symmetry) in response to the applied pressure. Fitting the P-V data with a Birch-Murnaghan isothermal equation of state, we obtained:) and K 0 =4.6(6). A series of structural refinements, based on the high-pressure intensity data, were performed. The stiffness of londonite (similar to that of carbides) is governed by its close-packing structure, and in particular by the very low compressibility of B-and Be-tetrahedra and the modest compressibility of the Al-octahedra. The Cs-polyhedra are the most compressible units of the structure. The effects of pressure can be accommodated by intrapolyhedral compression or deformation, leading to a modest bulk compression. The high amount of boron in londonite (B 2 O 3~5 0 wt%) makes its synthetic counterpart a potential neutron absorber. In addition, the high content of Cs makes londonite-type materials as potential hosts for nuclear waste.
K E Y W O R D Sborates, cesium/cesium compounds, elastic constants, single crystals, structure