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In allen Fällen gleich: Eine stabile, reversible und amorphe Phase (siehe Strukturmodell) wurde jeweils durch Tempern der vier zeolithischen Imidazolatgerüste ZIF‐1, ‐3, ‐4 und Co‐ZIF‐4 erhalten. Aus Nanoindentationsexperimenten, Dichtemessungen und Röntgenbeugungsdaten wird gefolgert, dass die Strukturen in allen vier Fällen äquivalent sind. Eine Amorphisierung wurde nur bei ZIFs mit nichtsubstituierten...
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