A novel ultramicroporous coordination polymer, namely [Cu(F-pymo)(2)(H2O)(1.25)](n) (1, F-pymo = 5-fluoropyrimidin-2-olate), has been prepared and structurally characterized. 1 displays a zeolitic gismondine (GIS) topology, with ca. 2.9 angstrom wide helical channels which, in the thermally activated counterpart (1'), account for a 13% void volume and are responsible for the observed selective solid-gas adsorption properties toward H-2, N-2, and CO2. At 77 K 1' behaves as a molecular sieve, selectively adsorbing H-2 over N2, possibly due to size-exclusion reasons. At variance, although CO2 molecules are slightly larger than the pore size, they are readily incorporated by 1' at temperatures as high as 433 K. Variable-temperature X-ray powder diffraction (TXRPD) studies, in the temperature range 303-473 K, show that dehydration is reversible and has almost negligible effects on the network. At variance, the uptake Of CO2 occurs through a transient phase and channels expansion. While the gas storage capacity of 1' is not very high-H-2, 0.56 wt % and 0.010 kg H-2/L at 90 K and 900 Torr, and CO2, 7.6 wt % at 273 K and 900 Torr-the guest molecules achieve very high densities, comparable to that of the liquid for H-2 (0.023 vs 0.021 molecules angstrom(-3)) and to that of the solid for CO2 (0.014 vs 0.022 molecules angstrom(-3)). In addition, we have also studied the effect of the perturbation exerted by the guest molecules on its magnetic properties. The results show that while dehydration of 1 has negligible effect on its spin-canted antiferromagnetic behavior, CO2 incorporation in the pores is responsible for an increment of the transition temperature at which the weak ferromagnetic ordering takes place from 22 to 29 K.
Guest-induced modification of a magnetically active ultramicroporous, gismondine-like, copper(II) coordination network
MASCIOCCHI, NORBERTO;GALLI, SIMONA;
2008-01-01
Abstract
A novel ultramicroporous coordination polymer, namely [Cu(F-pymo)(2)(H2O)(1.25)](n) (1, F-pymo = 5-fluoropyrimidin-2-olate), has been prepared and structurally characterized. 1 displays a zeolitic gismondine (GIS) topology, with ca. 2.9 angstrom wide helical channels which, in the thermally activated counterpart (1'), account for a 13% void volume and are responsible for the observed selective solid-gas adsorption properties toward H-2, N-2, and CO2. At 77 K 1' behaves as a molecular sieve, selectively adsorbing H-2 over N2, possibly due to size-exclusion reasons. At variance, although CO2 molecules are slightly larger than the pore size, they are readily incorporated by 1' at temperatures as high as 433 K. Variable-temperature X-ray powder diffraction (TXRPD) studies, in the temperature range 303-473 K, show that dehydration is reversible and has almost negligible effects on the network. At variance, the uptake Of CO2 occurs through a transient phase and channels expansion. While the gas storage capacity of 1' is not very high-H-2, 0.56 wt % and 0.010 kg H-2/L at 90 K and 900 Torr, and CO2, 7.6 wt % at 273 K and 900 Torr-the guest molecules achieve very high densities, comparable to that of the liquid for H-2 (0.023 vs 0.021 molecules angstrom(-3)) and to that of the solid for CO2 (0.014 vs 0.022 molecules angstrom(-3)). In addition, we have also studied the effect of the perturbation exerted by the guest molecules on its magnetic properties. The results show that while dehydration of 1 has negligible effect on its spin-canted antiferromagnetic behavior, CO2 incorporation in the pores is responsible for an increment of the transition temperature at which the weak ferromagnetic ordering takes place from 22 to 29 K.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.