E. Stuckenschmidt et al., NATROLITE .1. REFINEMENT OF HIGH-ORDER DATA, SEPARATION OF INTERNAL AND EXTERNAL VIBRATIONAL AMPLITUDES FROM DISPLACEMENT PARAMETERS, Physics and chemistry of minerals, 19(8), 1993, pp. 562-570
A single crystal of natrolite, Na2Al2Si3O10.2H2O, was studied by X-ray
diffraction methods at room temperature. The intensities were measure
d with MoKalpha radiation (lambda = 0.7107 angstrom) in a complete sph
ere of reflection up to sin theta/lambda = 0.903 angstrom-1. The struc
ture was refined in the orthorhombic space group Fdd2 with a = 18.2929
(7) angstrom, b = 18.6407(9) angstrom, c = 6.5871(6) angstrom, V = 224
6 angstrom3, Z = 8. A refinement of high-order diffraction data yielde
d reliability factors of R(F) = 0.9%, R(W)(F) = 0.8%, GoF = 1.40 for 1
856 high-angle reflections (0.7 less-than-or-equal-to sin theta/lambda
less-than-or-equal-to 0.903 angstrom-1) and R(F) = 1.0%, R(W)(F) = 1.
2 %, GoF = 3.07 for all 3471 independent reflections in the complete s
phere of reflection. The T - O distances as well as the T - O - T angl
es were found to be strongly influenced by the different bond strength
s received by the individual oxygen atoms. The T - O distances calcula
ted using Baur's extended valence rule agree on average within 0.003 a
ngstrom with the observed values. An analysis of the mean square displ
acement amplitudes allowed a separation of the external and internal v
ibrational amplitudes along the T - O bonds as well as along the Na -
O and H2O - O bond directions and the calculation of force constants.
The internal vibrational amplitudes (DELTAU) of the T - O vibrations a
re in the range of 5 to 11 x 10(-4) angstrom2, that is about one order
of magnitude smaller than the mean square displacement amplitudes of
the external vibrations. The corresponding force constants are F = 354
to 824 Nm-1. The values of the force constants of the motion of the N
a-ion and the water molecule against the framework oxygen atoms lie in
the range between F = 57 and 293 Nm-1. This is the first instance whe
re displacement amplitudes from a zeolite structure refinement could b
e apportioned between contributions from internal and external vibrati
ons for individual bonds.