M. Botoshansky et al., PYRIDINIUM PICRATE - THE STRUCTURES OF PHASE-I AND PHASE-II - CORRECTION OF PREVIOUS REPORT FOR PHASE-I - STUDY OF THE PHASE-TRANSFORMATION, Acta crystallographica. Section B, Structural science, 50, 1994, pp. 191-200
Pyridinium picrate, C5H6N+.C6H2N3O7, was reported [Kofler (1944). Z. E
lektrochem. 50, 200-207] to exist in two crystalline phases, one (I) b
eing stable below 343 K and the other (II) between 343 K and the melti
ng point (approximately 438 K). The room-temperature structure of phas
e I, studied by two-dimensional methods, has been reported [Talukdar &
Chaudhuri (1976). Acta Cryst. B32, 803-808]. We were led to reinvesti
gate the system by a number of unusual features in Kofler's descriptio
n of the phase behaviour. Single crystals of phase I were grown from s
olution and those of phase II from the melt. We have determined the st
ructure of both phases, including analysis of the thermal motion of th
e picrate ions, which was found to be appreciably larger in phase II t
han in phase I. The reported structure of phase I was found to be inco
rrect, although there were no warning signs; the error was caused by c
onfusion between a centre and twofold screw axis in projection down [0
10]. The packing units in the two phases are nearly identical and cons
ist of hydrogen-bonded cation-anion pairs. These are packed in stacks,
with the ion-pairs superimposed in parallel array in phase I whereas
those in phase II are antiparallel; the transition between the two pha
ses, therefore, cannot be expected to be single crystal to single crys
tal, as indeed it is not. Differential scanning calorimetry (DSC) and
variable-temperature powder X-ray diffraction photography show that th
e transition occurs at 383 K. Kofler appears to have been misled by a
colour change in the phase I crystals at 343 K, which we have also obs
erved but cannot explain. The DSC measurements give DELTAH(trans) = 6.
8 kJ mol-1 and DELTAH(fus) = 31.2 kJ mol-1. The transition has proved
not to be reversible under our experimental conditions; for example, p
hase II crystals remain unchanged after 24 h at 353 K. This suggests t
hat the temperature at which the crystalline phases are in thermodynam
ic equilibrium is appreciably below 383 K; we have not been able to de
termine the transition temperature. The details of the structure deter
minations (both at 298 K) are as follows: phase I, M(r) = 308.22, lamb
da(Mo Kalpha) = 0.71069 angstrom, F(000) = 632, yellow laths, monoclin
ic, mu(Mo Kalpha) = 0.95 cm-1, P2(1/c), a = 12.122 (2), b = 3.783 (1),
c = 26.621 (3) angstrom, beta = 92.56 (5)-degrees, V = 1219.6 angstro
m3, Z = 4, D(m) = 1.62 (flotation at 298 K), D(x) = 1.67 g cm-3, R(int
) = 0.0167 (based on 25 pairs of equivalent reflections), R(F) = 0.043
6, wR = 0.0492 [based on 1645 independent reflections with F > 3sigma(
F)], refinement on F; phase II, M(r) = 308.22, lambda(Mo Kalpha) = 0.7
1069 angstrom, F(000) = 316, yellow prisms, triclinic, mu(Mo Kalpha) =
0.90 cm-1, P1BAR, a = 10.156 (2), b = 8.984 (2), c = 7.230 (1) angstr
om, alpha = 86.38 (5), beta = 80.10 (5), gamma = 89.97 (5)-degrees, V
= 648.6 angstrom3, Z = 2, D(m) = 1.60 (flotation at 298 K), D(x) = 1.5
8 g cm-3, R(F) = 0.0716, wR = 0.0694 [based on 1478 independent reflec
tions with F > 3sigma(F)], refinement on F. Cell dimensions have been
measured as a function of temperature for both phases.