From thermal cracking, physical properties

If one examines the evolution of new zeolite structures over the past decade the most interesting discoveries have been made with high silica compositions. Many of these phases can be prepared in essentially all silica forms. Purists would prefer to classify such molecular sieves as organosilicates or porosils (1), in part because the physical properties differ from more classical low Si/Al ratio zeolites. In particular, the high silica zeolites tend to be more thermally stable and chemically robust. Additionally, the higher the Si/Al ratio the more hydrophobic the zeolite. These features are desirable for catalysts that may be used in catalytic processes such as cracking (3). 

The mechanical interaction between the different epitaxial layers may result in the formation of misfit dislocations. Nucleation and propagation of cracks can ensue if the mismatch in thermal expansion coefficient is relatively large. The defects significantly influence the physical properties of the thin films. Examples from different material combinations and models of how to predict the numbers for critical thicknesses are provided in Section 14.4. 

TS involves the measurement of the sound intensity emitted by a sample as a function of temperature. Sound emission originates from the release of thermal stresses in the sample, such as movement of dislocations, generation and propagation of cracks, nucleation of new phases, relaxation processes, and discontinuous changes in physical properties. For example, at a glass transition temperature, a discontinuous change in free volume generates elastic waves... 

---