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- W1997526114 abstract "The structures of SrY zeolite were determined in the dehydrated and in the hydrated form by X-ray powder diffractometry. The influence of the temperature on the variation of the cation location was investigated in the range of 323 K to 723 K for the hydrated forms and between 723 K and 1123 K in the dehydrated forms. For the dehydrated structures a Boltzmann-like cation distribution was observed above 823 K. With increasing temperature the cations become more and more equally distributed over the different cation sites. Below 823 K a linear variation of the cation site populations is observed, which is explained in terms of domain disorder. In the hydrated samples the cation site distribution depends on the residual water inside the zeolite cavities, which is a function of temperature." @default.
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- W1997526114 date "1987-11-01" @default.
- W1997526114 modified "2023-09-26" @default.
- W1997526114 title "Influence of the temperature on the cation distribution in dehydrated and hydrated SrY zeolites" @default.
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- W1997526114 doi "https://doi.org/10.1016/0144-2449(87)90092-3" @default.
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