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Metal-organic frameworks (MOFs) are a class of crystalline materials with a structure of inorganic nodes connected by organic ligands. There are currently more than 60,000 known MOFs, and they are being investigated as promising materials for gas storage, including CO2 sequestration, and hydrogen storage, and can even be used to harvest water in the desert.
Metal-organic frameworks (MOFs) are fast becoming dominant in research into new materials. These three-dimensional structures are formed from the self-assembly of inorganic nodes, and organic bridging ligands, into highly ordered networks with exceptionally high internal surface areas (>7000 m2 g-1). These ‘molecular sponges’ possess huge, record-breaking porosities; in some cases, the internal surface area of 1 g of a MOF is the same as one-and-a-half football fields. Many applications have therefore been proposed for MOFs, including, for example, H2, CO2, and CH4 gas storage and separations, ion conduction, catalysis, and water harvesting1. Commercial (crystalline) MOF products available include those for the prevention of fruit ripening, and the storage of toxic gases in the semiconductor industry.
High temperature reactions between mixtures of some specific MOFs, namely ZIF-4 [M(Im)2] and ZIF-62 [Zn(Im)1.75(bIm)0.25] (M = Co2+, Zn2+, Im: C3H3N2−, bIm: C7H5N2−), were investigated (Fig. 1). Previously, it had been observed that, upon heating, both ZIF-4-Zn and ZIF-4-Co undergo a transition to a high-density amorphous phase, and then to a dense crystal upon heating to 300 °C and 450 °C, respectively. The dense zinc framework melts at 550 °C, unlike the dense cobalt crystal, which remains intact until thermal decomposition at ca. 570 °C. ZIF-62 remains in the room temperature crystalline structure until it melts at 410 °C4.
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