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