Abstract
In situ time-resolved synchrotron X-ray and neutron powder diffraction studies indicate that the negative thermal expansion and 'trap door' cation relocations observed in zeolite rho result from water-mediated chemical changes that occur during dehydration.
| Original language | English |
|---|---|
| Pages (from-to) | 2221-2222 |
| Number of pages | 2 |
| Journal | Chemical Communications |
| Issue number | 22 |
| DOIs | |
| State | Published - Nov 21 2000 |
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