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THE PHOTOREDUCTION OF METHYLVIOLOGEN VIA ELECTRON TRANSFER FROM ALUMINOSILICATE ZEOLITES

机译:铝硅酸盐沸石通过电子转移对甲基硫醇的光催化

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The photoreduction yields of methylviologen and various alkylated homologues in zeolite-X, Y and A were determined at 77 K. in the absence of any reducing counteranion. Upon irradiation at 77 K, dehydrated samples turned light blue and a single line ESR spectrum was observed with a g-factor identical to that of the methylviologen radical cation. Samples that were not dehydrated produced ESR spectra about 10% as intense as those that had the water removed. The photoreduction yield was largest in zeolite Y, less in zeolite X which has more cations and hence more crowding in the cages, and very small in zeolite A which has much smaller cages. The electron donor in these systems is believed to be the anionic aluminosilicate framework of the host zeolite.
机译:在不存在任何还原性抗衡阴离子的情况下,在77 K下测定了沸石X,Y和A中甲基紫精和各种烷基化同系物的光还原产率。在77 K照射后,脱水样品变成浅蓝色,并观察到单线ESR光谱,其g因子与甲基紫罗兰自由基阳离子相同。未脱水的样品产生的ESR光谱的强度约为去除水分后的样品的10%。沸石Y的光还原产率最大,沸石X的阳离子较少,因而具有更多的阳离子,因此笼子中的拥挤程度更高,而沸石A的笼罩小得多。这些系统中的电子给体被认为是主体沸石的阴离子硅铝酸盐骨架。

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