2011
DOI: 10.1021/ja202132h
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MOF-5: Enthalpy of Formation and Energy Landscape of Porous Materials

Abstract: The first experimental thermodynamic analysis of a metal-organic framework (MOF) has been performed. Measurement of the enthalpy of formation of MOF-5 from the dense components zinc oxide (ZnO), 1,4-benzenedicarboxylic acid (H(2)BDC), and occluded N,N-diethylformamide (DEF) (if any) gave values of 78.64 ± 2.95 and 99.47 ± 3.62 kJ·[mol of Zn(4)O(BDC)(3)·xDEF](-1) for the as-made form and the desolvated structure, respectively. These as-made and desolvated enthalpies correspond to the values 19.66 ± 0.74 and 24.… Show more

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Cited by 59 publications
(77 citation statements)
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References 31 publications
(23 reference statements)
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“…However, an increasing body of work suggests that crystalline porous materials with empty pores are metastable with respect to their dense phases (Figure 1). [16][17][18][19][20][21] The dense phase is a hypothetical assemblage of the same constituent atoms, ions, or ligands, but carries negligible porosity. For an all-silica zeolite, the dense phase is easily envisaged as nonporous amorphous silica, which can be accessed via simple heating.…”
Section: The Energetic Penalty For Porositymentioning
confidence: 99%
“…However, an increasing body of work suggests that crystalline porous materials with empty pores are metastable with respect to their dense phases (Figure 1). [16][17][18][19][20][21] The dense phase is a hypothetical assemblage of the same constituent atoms, ions, or ligands, but carries negligible porosity. For an all-silica zeolite, the dense phase is easily envisaged as nonporous amorphous silica, which can be accessed via simple heating.…”
Section: The Energetic Penalty For Porositymentioning
confidence: 99%
“…For reference, the formation enthalpies for all materials examined here are comparable to the formation enthalpy of other metastable materials (e.g., MOF-5). 31 …”
Section: Structural Stabilitymentioning
confidence: 99%
“…for zeolites but the conclusion of this investigation is that at least some structures of low energy, lying on the observed plateau, probably exist for very high porosity. A rich energy landscape of structures with similar energies (on the plateau) suggests that preference among configurations and/or structures which have comparable energies is controlled by kinetic factors rather than by thermodynamics . These small energetic differences permit a diversity of synthesized frameworks …”
Section: Figurementioning
confidence: 99%