|
The effects of B2O3 and P2O5 on the crystallization behavior and dielectric properties of sol-
gel prepared stoichiometric cordierite and anorthite were studied. From the results, it was
found that both B2O3 and P2O5 in the cordierite would promote the formation of α- cordierite. And the addition of P2O5 could also cause the densification of cordierite. However, these additions had little influences on the dielectric constant and loss tangent of stoichiometric cordierite. Contrastingly, only the additions of B2O3 to the stoichiometric anorthite promoted the formation of the triclinic phase. Addition of P2O5 did not affect the crystallization of anorthite. Both bulk densities and the dielectric constants of sintered anorthite decreased with the increase of B2O3 and P2 O5. In addition, gel- derived cordierite glass powder with composition of MgO/Al2O3/SiO2=25/22/53 were prepared and mixed with gel-derived stoichiometric anorthite glass powder with various weight percentages and sintered to form cordierite- anorthite composites. Composites of the same compositions were also prepared by sol-gel of Ca-Mg-Al-Si four components system. In these composites, it was found that cordierite could promote the formation of the triclinic phase of anorthite and anorthite could enhance the formation of α-cordierite regardless of the preparation method. SEM and EDS analyses showed that spherical anorthite were surrounded by cordierite in the anorthite-rich samples. The wetting between anorthite and cordierite appeared to be good. This would result in good sinterability in the cordierite-anorthite system. The samples prepared by sol-gel process howshow better relationships between properties and compositions than those by powder mixing process. The densities of the cordierite-anorthite glass ceramics prepared by sol-gel process were between 2.2 and 2.7 g/ cm3, and the dielectric constants (5.4∼7.0) lineally increased with the weight percentage of the anorthite. When cordierite- anorthite glass ceramics contained 20 to 60wt% of anorthite, the samples showed low thermal expansion coefficients:4.0∼4.5×10-6/℃ at 100℃, and 2.5∼4.0×10-6/℃ at 200℃.
|