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Hydrogen storage in ion-exchanged zeolites

机译:离子交换沸石中的氢存储

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摘要

The hydrogen storage properties of zeolites X, Y, A and Rho containing various exchangeable cations have been investigated. All hydrogen storage capacities were measured at a temperature of -196 deg C and a pressure range of 0-15 bar, using a constant pressure thermogravimetric analyser. The results show that, zeolites exhibit diverse behaviour with respect to hydrogen uptake, dependent on both the framework structure and the nature of the cations present. A major factor influencing uptake is the available void space: in zeolites A and Rho pore blocking by large extraframework cations is a major factor restricting hydrogen uptake, but in zeolites X and Y, blocking does not occur. This study also suggests that cations may act as binding sites for hydrogen molecules. For zeolites X and Y, hydrogen uptake relates closely to the measured BET surface area. The highest gravimetric storage capacity of 2.19 wt. percent was obtained for CaX. Volumetric storage densities of up to 31.0 kg H_2/m~3 (143 H_2 molecules/unit cell) and 30.2kg H_2/m~3 (144 H_2 molecules/unit cell) were achieved for CaX and KX, respectively.
机译:已经研究了含有各种可交换阳离子的X,Y,A和Rho沸石的储氢性能。使用恒压热重分析仪在-196℃的温度和0-15 bar的压力范围内测量所有储氢容量。结果表明,沸石对氢的吸收表现出不同的行为,这取决于所存在的阳离子的骨架结构和性质。影响吸收的主要因素是可用的空隙空间:在沸石A和Rho中,大的骨架外阳离子对孔的阻塞是限制氢吸收的主要因素,但在沸石X和Y中,不会发生阻塞。这项研究还表明,阳离子可能充当氢分子的结合位点。对于沸石X和Y,氢的吸收与所测BET表面积密切相关。最高重量存储容量为2.19 wt。对于CaX,获得了50%。 CaX和KX分别达到31.0 kg H_2 / m〜3(143 H_2分子/单位细胞)和30.2kg H_2 / m〜3(144 H_2分子/单位细胞)的体积存储密度。

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