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Structural and physicochemical properties of natural zeolites:clinoptilolite and mordenite

机译:天然沸石的结构和理化性质:斜发沸石和丝光沸石

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Natural,H-form and Pd-containing clinoptilolite and mordenite were characterized using adsorption,AFM,FTIR,and TG-DTA methods.The initial natural adsorbents have small specific surface area which increases significantly after their modification.FTIR spectra show the presence of the same typical bands in natural and H-form zeolites.However,the spectra of Pd-including clinoptilolite have a band of ammonia at v = 1449 cm~(-1),which can be associated with its adsorption complexes with palladium.The TG data show the presence of several types of water,and larger amounts of water desorb from H-forms of both zeolites up to 120 deg C that can be caused by stronger changes in the zeolite structure.However,the zeolite skeleton does not change after acidic processing.The changes are more visible for treated clinoptilolite.
机译:天然,H型和含Pd的斜发沸石和丝光沸石采用吸附,AFM,FTIR和TG-DTA方法进行了表征。初始天然吸附剂的比表面积小,经过改性后显着增加.FTIR光谱表明存在天然和H型沸石具有相同的典型谱带。但是,含Pd的斜发沸石的光谱在v = 1449 cm〜(-1)处具有氨谱带,这可能与其与钯的吸附配合物有关.TG数据表明存在多种类型的水,并且两种沸石的H型都能从120摄氏度以下的H型中解吸出大量水,这可能是由于沸石结构发生更强的变化所致。然而,经过酸性处理后,沸石骨架不会发生变化对于经处理的斜发沸石,该变化更明显。

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