In single crystals of the beryllium silicate Be 2 SiO 4 with trigonal symmetry R3, known also as the mineral phenakite, χ (3) -nonlinear lasing by stimulated Raman scattering (SRS) is investigated. All observed Stokes and anti-Stokes lasing components are identified and ascribed to a single SRS-promoting vibration mode with ω SRS ≈876 cm −1 . With picosecond singlewavelength pumping at one micrometer the generation of an octave-spanning Stokes and anti-Stokes comb is observed.Al 2 [F 1-x (OH) x ] 2 SiO 4 four different SRS-promoting modes were observed, two of which are combined modes. These occurring differences in nonlinear-lasing characteristics motivated the present study of SRS in Be 2 SiO 4 (phenakite). The crystal structure of phenakite gives a simple example of an intermediate link between neso-silicates and tectosilicates, since all (mutually separated) [SiO 4 ] groups of the structure are strongly bonded by tetrahedral [BeO 4 ] structural units to form a three-dimensional framework [7-10].
CrystallographyBeryllium silicate, Be 2 SiO 4 , also known as the (rare) mineral phenakite, is a member of a family of isostructural trigonal compounds of general composition M 2 XO 4 , which crystallize with space group symmetry R3 (Nr. 148). In this structural family representatives are known with M II and X IV (e.g. Be ) and with M III and X II (e.g. Al 2 CdO 4 ). Coupled substitution of 2M II → M I + M III (with X IV ) or 2M II → M I + M II (with X V ) allows C