The kinetics of hydrothermal crystallisation of sodium zeolites from a natu
ral mixture of halloysite and amorphous silica with Si/Al approximate to 4
was investigated. The sample collected at Scarpara (Tuscania, Italy) is the
final product of an intense hydrothermal alteration process on the pre-exi
sting leucitic tufities. In order to enhance its reactivity in the NaOH sol
ution, the sample was thermally activated at 600 degreesC for 1 h. The hydr
othermal crystallisation sequence of zeolites formed in the range 90-150 de
greesC has been followed using real-time synchrotron powder diffraction. Th
e reaction kinetics of Na-X. Na-P and analcime were analysed using a model
developed for the study of the kinetic data from X-ray diffraction experime
nts. Na-X and Na-P cocrystallize with an autocatalytic nucleation at lower
isothermal temperatures and with a heterogeneous nucleation at higher isoth
ermal temperatures. Na-X tends to dissolve before Na-P, which in turn trans
forms into analcime. This work is part of a general project on the kinetics
of formation of zeolites from clay precursors which is important for eithe
r engineering and production of valuable industrial materials and for the i
nterpretation of poorly understood processes of formation of zeolites in na
tural hydrothermal environments.