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Guest-mediated phase transitions in a flexible pillared-layered metal–organic framework under high-pressure
Authors:Gemma F. Turner  Scott C. McKellar  David R. Allan  Anthony K. Cheetham  Sebastian Henke  Stephen A. Moggach
Affiliation:School of Molecular Sciences, University of Western Australia, Perth 6009 Western Australia Australia.; EastChem School of Chemistry, University of Edinburgh, Edinburgh EH9 3JW UK ; Diamond Light Source, Harwell Science and Innovation Campus, Didcot O11 ODE UK ; Materials Research Laboratory, University of California, Santa Barbara CA 93106 USA ; Fakultät für Chemie und Chemische Biologie, Technische Universität Dortmund, Dortmund 44227 Germany,
Abstract:The guest-dependent flexibility of the pillared-layered metal–organic framework (MOF), Zn2bdc2dabco·X(guest), where guest = EtOH, DMF or benzene, has been examined by high-pressure single crystal X-ray diffraction. A pressure-induced structural phase transition is found for the EtOH- and DMF-included frameworks during compression in a hydrostatic medium of the guest species, which is dependent upon the nature and quantity of the guest in the channels. The EtOH-included material undergoes a phase transition from P4/mmm to C2/m at 0.69 GPa, which is accompanied by a change in the pore shape from square to rhombus via super-filling of the pores. The DMF-included material undergoes a guest-mediated phase transition from I4/mcm to P4/mmm at 0.33 GPa via disordering of the DMF guest. In contrast, the benzene-included framework features a structure with rhombus-shaped channels at ambient pressure and shows direct compression under hydrostatic pressure. These results demonstrate the large influence of guest molecules on the high-pressure phase behavior of flexible MOFs. Guest-mediated framework flexibility is useful for engineering MOFs with bespoke pore shapes and compressibility.

The guest-dependent flexibility of the pillared-layered metal–organic framework (MOF), Zn2bdc2dabco·X(guest), where guest = EtOH, DMF or benzene, has been examined by high-pressure single crystal X-ray diffraction.
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