Heulandite molecular sieves with a Si/Al ratio of 3.2 similar to 3.8 h
ave been, synthesized hydrothermally in the presence of the alkali cat
ions Li+; Li+, K+; and Na+, K+ at 190 degrees C at autogenous pressure
. They have been characterized by X-ray powder diffraction and scannin
g electron micrographs. Heulandites can be formed in the Li+ and Na+,
K+ cation systems only with similar to 10 wt% seed crystals. But heula
ndite can be synthesized in the presence of Li+, K+ cations without se
ed crystals. The formation of heulandite-type zeolites occurs over a n
arrow crystallization field and depends on the Si/Al ratio, the OH-/Si
ratio, and on the presence of seed crystals. Scanning electron microg
raphs show a thin-plate topology for the crystals. Heulandite is therm
ally unstable for calcination beyond 350 similar to 450 degrees C. (C)
Elsevier Science Inc. 1997.