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首页> 外文期刊>Physical chemistry chemical physics: PCCP >Aluminium siting in the ZSM-5 framework by combination of high resolution ~(27)Al NMR and DFT/MM calculations
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Aluminium siting in the ZSM-5 framework by combination of high resolution ~(27)Al NMR and DFT/MM calculations

机译:结合高分辨率〜(27)Al NMR和DFT / MM计算,将ZSM-5框架中的铝选址

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摘要

The Al siting in the ZSM-5 zeolite was investigated by ~(27)Al 3Q MAS NMR spectroscopy and QM/MM calculations.It was found that the occupation of the framework T-sites by Al and the concentration of Al in these T-sites are neither random nor controlled by a simple rule.They both depend on the conditions of the zeolite synthesis.At least 12 out of the 24 distinguishable framework T-sites of ZSM-5 are occupied by Al in the set of the investigated zeolite samples.A partial identification of the Al sites is possible.The calculated ~(27)Al NMR shielding values were converted to ~(27)Al isotropic chemical shifts using the experimental isotropic chemical shift of 60.0 ppm referenced to the aqueous solution of A1(NO3)3 and the corresponding calculated NMR shielding of 490.0 ppm of a silicon rich(Si/Al 38)chabazite structure zeolite as a secondary internal standard.The observed ~(27)Al isotropic chemical shifts of 50.0 and 54.7 ppm correspond to Al atoms in the T20 and T6 sites,respectively.The pair of measured isotropic chemical shifts of 52.9 and 53.7 ppm can be assigned to the T4,T8 pair.At the low-shielding end,two assignments are plausible.The smallest deviations between the calculated and observed isotropic chemical shifts are reached for the assignment as follows:T24(64.8 ppm)is not occupied in the samples and that the observed isotropic chemical shifts 63.6,62.8,and 60.0 ppm belong to Tl,T17,and T7,respectively.It follows then that T-sites T12(60.8 ppm),T3(61.7 ppm),and T18(62.0 ppm)are most likely not occupied by Al in our ZSM-5 samples.If we assume that the calculated isotropic chemical shifts are systematically larger than the observed ones then we can assign the largest observed isotropic chemical shifts of 63.6 and 62.8 ppm to the least shielded T24 and T1 sites,respectively,and 60.0 ppm to T12.Then the sites T3(61.7 ppm),T18(62.0 ppm),and T17(62.5 ppm)would be unoccupied by Al in our ZSM-5 samples.It was further shown that there is no simple linear relationship between the observed ~(27)Al isotropic chemical shifts and the average Al-O-Si angles.
机译:通过〜(27)Al 3Q MAS NMR光谱学和QM / MM计算研究了ZSM-5沸石中的Al分布,发现Al占据了骨架T位点以及这些T-中Al的浓度ZSM-5的位点既不是随机的也不是受简单规则控制的,它们都取决于沸石的合成条件。在所研究的沸石样品中,ZSM-5的24个可区分的骨架T位中至少有12个被Al占据可以部分鉴定Al的位点。使用相对于A1(NO3)水溶液的60.0 ppm的实验各向同性化学位移,将计算出的〜(27)Al NMR屏蔽值转换为〜(27)Al各向同性化学位移)3和相应的计算得出的490.0 ppm富硅(Si / Al 38)菱沸石结构沸石作为次要内标的NMR屏蔽。观察到的50.0和54.7 ppm的〜(27)Al各向同性化学位移对应于Al原子T20和T6站点分别。可以将一对测量的各向同性化学位移分别为52.9和53.7 ppm分配给T4,T8对。在低屏蔽端,有两个分配是合理的。对于该分配,计算得出的和观察到的各向同性化学位移之间的最小偏差为样品中没有T24(64.8 ppm),并且观察到的各向同性化学位移63.6、62.8和60.0 ppm分别属于T1,T17和T7。然后是T位置T12(60.8 ppm) ,在我们的ZSM-5样品中,T3(61.7 ppm)和T18(62.0 ppm)最有可能未被Al占据。如果我们假设计算得出的各向同性化学位移大于观测到的化学位移,则可以指定最大的观测到的各向同性的化学位移分别为63.6和62.8 ppm到最小屏蔽的T24和T1位置,以及60.0 ppm到T12的位置,然后位置T3(61.7 ppm),T18(62.0 ppm)和T17(62.5 ppm)不会被占据ZSM-5样品中的Al进一步证明没有简单的线性关系观测到的〜(27)Al各向同性化学位移与平均Al-O-Si角之间的关系。

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