The diffusion of Cs+ was measured at temperatures of between 300 and 420C (table 7), by using tracer and serial sectioning techniques. The diffusion involved a vacancy mechanism. The Cs+ ions, which were over-sized in comparison with the host Ag+ ions, produced local strains in the AgBr lattice. This led to diffusivities which were larger than those of substitutional Ag+ and partially compensated for the intrinsic curvature in the Arrhenius plot which was expected to result from the non-linear decrease in the Gibbs free energy for Frenkel defect formation with increasing temperature. The diffusivity of Cs+ in AgBr was lower than that in AgCl. This was attributed to the larger size effect in a more compact lattice.
Diffusion of Cesium in Silver Bromide: a Surprising Observation of the Strain Effect due to an Oversize Solute. P.A.Cardegna, A.L.Laskar: Physical Review B, 1985, 32[10], 7000-2
Table 8
Diffusivity of Fe2+ in AgBr
Temperature (C) | D (cm2/s) |
419.8 | 2.57 x 10-7 |
410.2 | 1.99 x 10-7 |
395.2 | 9.96 x 10-7 |
365.5 | 2.30 x 10-7 |
350.2 | 1.20 x 10-7 |
324.3 | 5.23 x 10-7 |
299.9 | 1.78 x 10-7 |
279.9 | 6.20 x 10-7 |
240.8 | 5.90 x 10-7 |