“…Combined TG-DTA was mostly used to provide complementary information on the decomposition process of various organic host molecules (ions) occluded in the zeolitic framework during synthesis. Usually only qualitative information is desired on the temperature range in which the organics are removed from the precursor framework by oxidative degradation, and examples illustrating the fruitful use of DTA for this purpose are numerous: decomposition of tetra-methylammonium (TMA) ions occluded in various zeolites (Barrer & Denny, 1961;Aiello & Barrer, 1970;Wu et al, 1971;Colella et al, 1982;Whyte & Dalla Betta, 1982;Penchev et al, 1983;Sidamonidze et al, 1983;Occelli & Perrotta, 1983); decomposition of ZSM-5 containing either its classical structure-directing tetra-propylammonium (TPA) ions (Bibby et al, 1979;Chao, 1979;Bibby et al, 1980;Derouane et al, 1981b;Chao et al, 1981;Yun & Ruren, 1982;Penchev et al, 1983), or tetra-ethylammonium (TEA) ions (Parker et al, 1984), or containing various other (poly)alkylamines (Qingxia et al, 1982;Gabelica et al, 1983f;Parker et al, 1983); decomposition of ZSM-11 containing tetra-butylammonium (TBA) ions (Bibby et al, 1979;Gabelica et al, 1983f;Surin et al, 1983); decomposition of ZSM-5/11 mixed phases (intergrowths) containing tri-alkylamines (Gabelica et al, 1983f) and degradations of many other complex organic molecules incorporated in high-silica zeolites such as ZSM-39 (Bibby & Parker, 1983) or Eu-1 (Casci et al, 1983), or even decomposition of tetra-alkylammonium ions 'occluded' within amorphous silica-aluminas (Manton & Davidtz, 1979;Howden, 1982b).…”