THE LOW-TEMPERATURE PHASE-TRANSITION SEQUENCE OF THE HALIDE PEROVSKITE TETRAMETHYLAMMONIUM TRICHLOROGERMANATE(II) AND THE STRUCTURE OF ITS INCOMMENSURATELY MODULATED DELTA-PHASE

Citation
K. Futterer et al., THE LOW-TEMPERATURE PHASE-TRANSITION SEQUENCE OF THE HALIDE PEROVSKITE TETRAMETHYLAMMONIUM TRICHLOROGERMANATE(II) AND THE STRUCTURE OF ITS INCOMMENSURATELY MODULATED DELTA-PHASE, Acta crystallographica. Section B, Structural science, 51, 1995, pp. 768-779
Citations number
25
Categorie Soggetti
Crystallography
ISSN journal
01087681
Volume
51
Year of publication
1995
Part
5
Pages
768 - 779
Database
ISI
SICI code
0108-7681(1995)51:<768:TLPSOT>2.0.ZU;2-U
Abstract
Tetramethylammonium trichlorogermanate(II), N(CH3)(4)-GeCl3, abbreviat ed as TGC, has been investigated by temperature-dependent X-ray powder and single-crystal diffraction. It is shown that TGC has a one-dimens ional incommensurately modulated phase, called the delta-phase, with p rimary modulation wavevector q approximate to 0.14 b. This phase is s table in the temperature range 170 less than or equal to T less than o r equal to 200 K and occurs between the room-temperature phase gamma a nd a lower-temperature phase epsilon. The structure of delta TGC was r efined in the (3+1)-dimensional superspace group Pnam(0 beta 0)00s. Th e average structure of delta-TGC with lattice parameters 13.083 (6) x 8.841 (4) x 9.027(4) Angstrom(3) (T = 190 K) is isomorphous to the str ucture of the normal room-temperature phase gamma. The latter is of di storted perovskite-type [Depmeier, Moller & Klaska (1980). Acta Cryst. B36, 803-807]. The modulation in the case of the delta-phase is purel y displacive, the dominant modulation wave being polarized along the c -axis and of magnitude 0.42 Angstrom. The low-temperature phase epsilo n is monoclinic with lattice parameters 13.068 (6) x 8.808 (5) x 8.962 (6)Angstrom(3), alpha = 93.9(1)degrees at T = 160 K. The intensity of the incommensurate satellite reflections vanishes at the delta-epsilon transition. The observed diffraction patterns suggest that the delta- epsilon transition at 170 K is also associated with the partial reappe arance of the orthorhombic lattice of the gamma-phase. In fact, both s ingle-crystal and powder diffraction display the super-position of a m onoclinic and an orthorhombic reciprocal lattice, which persists from T-delta-epsilon = 170 K down to at least 130 K. The intensity ratio of monoclinic to orthorhombic reflections is ca 5:1 and is essentially c onstant for T < 160 K.