摘要
The zeolite analcime was synthesized, in its sodium form, from a perlite (volcanic glass) deposit at Lopburi, Thailand. Particle size analysis was used to approximate the radius of the analcime particles as 3.87脙脙10脙脙脙6m. XRD, XRF, 29Si MAS NMR and thermal analysis confirmed the product as analcime of good purity. Diffusion exchange of Cu2+, Ni2+, Pb2+ and Zn2+ for 22Na+ from the synthetic analcime was investigated in the temperature range 298脙脙脙333K. Diffusion coefficients (D) were calculated using the Barrer, Barri and Klinowski equation. Ea, 脙脙S* and 脙脙G* values showed that all the channel sites were involved in the observed diffusion processes.