Thermal behaviour of libethenite from room temperature up to dehydration

The structural modifications with temperature of libethenite, Cu (sub 2) (PO (sub 4) )(OH), were determined by single-crystal X-ray diffraction up to dehydration and consequent decomposition of the crystal under investigation. In the temperature range 25-475 degrees C, libethenite shows positive and linear expansion. The axial thermal expansion coefficients, determined over this temperature range, are: alpha (sub a) =6.6(1).10 (super -6) K (super -1) , alpha (sub b) =1.21(2).10 (super -5) K (super -1) , alpha (sub c) =9.0(2).10 (super -6) K (super -1) , alpha (sub V) =2.78(3).10 (super -5) K (super -1) . Axial expansion is then anisotropic with alpha (sub a) :alpha (sub b) :alpha (sub c) =1:1.83:1.33. Structure refinements of X-ray diffraction data collected at different temperatures allowed us to characterize the mechanisms by which the libethenite structure accommodates variations in temperature. Increasing temperature induces expansion of both Cu polyhedra and no significant variation of the PO (sub 4) tetrahedron, which acts as a rigid unit. Cu(1) octahedra expand mostly as a consequence of the increase of the axial bonds, and become more distorted. Starting from T=500 degrees C, precursor signs of incoming dehydration are visible: two adjacent OH groups approach each other and cause dramatic changes in the whole structure. Concomitantly, the libethenite crystal begins to deteriorate and, at T=600 degrees C, broad and weak diffraction effects of polycrystalline material are observed.