The structure of yellow InCl is explained. The cubic cell contains 20 trigo
nally and 12 digonally distorted InCl6-octahedra, due to the (5s)(2)-outer
electron configuration of In+. To a good approximation the structure can be
seen as distorted rocksalt, due to three equally strong lattice modes. The
distortions of the local octahedra, of various symmetry-type, can be calcu
lated from the structure, derived from available XRD-data. It is possible f
rom these to deduce bilinear forms, which express chirality, tetrahedron fo
rming and spiral forming. Chirality is especially interesting, since there
is an optical analogue and one of the expressions for chirality resembles t
he rotational strength as described by Condon for optical rotation. The oth
er form of chirality goes beyond the Condon approximation and arises since
the size of these octahedra is about 1/3 of the wave length of the helices.
The three lattice modes induce a number of anti-ferrodistortive distributi
ons of helices, tetrahedrons and spirals. In addition, there is also one fe
rrodistortive component for chirality and one for tetrahedron forming. (C)
1998 Elsevier Science S.A. All rights reserved.