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Reversible and Selective O2 Chemisorption in a Porous Metal–Organic Host Material

by: Peter D. Southon, David J. Price, Pia K. Nielsen, Christine J. McKenzie, Cameron J. Kepert
J. Am. Chem. Soc. In Journal of the American Chemical Society, Vol. 133, No. 28. (3 June 2011), pp. 10885-10891, doi:10.1021/ja202228v  Key: citeulike:11895448

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Abstract

The metal?organic host material [CoIII2(bpbp)(O2)2bdc](PF6)4 (1·2O2; bpbp? = 2,6-bis(N,N-bis(2-pyridylmethyl)aminomethyl)-4-tert-butylphenolato; bdc2? = 1,4-benzenedicarboxylato) displays reversible chemisorptive desorption and resorption of dioxygen through conversion to the deoxygenated Co(II) form [CoII2(bpbp)2bdc](PF6)4 (1). Single crystal X-ray diffraction analysis indicates that the host lattice 1·2O2, achieved through desorption of included water guests from the as-synthesized phase 1·2O2·3H2O, consists of an ionic lattice containing discrete tetranuclear complexes, between which lie void regions that allow the migration of dioxygen and other guests. Powder X-ray diffraction analyses indicate that the host material retains crystallinity through the dioxygen desorption/chemisorption processes. Dioxygen chemisorption measurements on 1 show near-stoichiometric uptake of dioxygen at 5 mbar and 25 °C, and this capacity is largely retained at temperatures above 100 °C. Gas adsorption isotherms of major atmospheric gases on both 1 and 1·2O2 indicate the potential suitability of this material for air separation, with a O2/N2 selectivity factor of 38 at 1 atm. Comparison of oxygen binding in solution and in the solid state indicates a dramatic increase in binding affinity to the complex when it is incorporated in a porous solid. The metal?organic host material [CoIII2(bpbp)(O2)2bdc](PF6)4 (1·2O2; bpbp? = 2,6-bis(N,N-bis(2-pyridylmethyl)aminomethyl)-4-tert-butylphenolato; bdc2? = 1,4-benzenedicarboxylato) displays reversible chemisorptive desorption and resorption of dioxygen through conversion to the deoxygenated Co(II) form [CoII2(bpbp)2bdc](PF6)4 (1). Single crystal X-ray diffraction analysis indicates that the host lattice 1·2O2, achieved through desorption of included water guests from the as-synthesized phase 1·2O2·3H2O, consists of an ionic lattice containing discrete tetranuclear complexes, between which lie void regions that allow the migration of dioxygen and other guests. Powder X-ray diffraction analyses indicate that the host material retains crystallinity through the dioxygen desorption/chemisorption processes. Dioxygen chemisorption measurements on 1 show near-stoichiometric uptake of dioxygen at 5 mbar and 25 °C, and this capacity is largely retained at temperatures above 100 °C. Gas adsorption isotherms of major atmospheric gases on both 1 and 1·2O2 indicate the potential suitability of this material for air separation, with a O2/N2 selectivity factor of 38 at 1 atm. Comparison of oxygen binding in solution and in the solid state indicates a dramatic increase in binding affinity to the complex when it is incorporated in a porous solid.


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