“…Other than phillipsites and heulandite, the commercially available natural zeolites do not undergo such structural collapse (Hoss and Roy, 1960;Breck, 1974;Komarneni and Roy, 1981) and, therefore, need very high temperatures of 1200~ (Mimura and Kanno, 1980;Forberg et al, 1980) for the immobilization of Cs in crystalline phases. Heutandite, which was not investigated here, is also a potential zeolite for Cs fixation inasmuch as it undergoes structural collapse at > 360~ (Mumpton, 1960).…”