首页> 外文会议>2nd International FEZA (Federation of the European Zeolite Associations) Conference, Sep 1-5, 2002, Taormina, Italy >Microtopographic features and dissolution behavior of natural zeolite surfaces studied by Atomic Force Microscopy (AFM)
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Microtopographic features and dissolution behavior of natural zeolite surfaces studied by Atomic Force Microscopy (AFM)

机译:原子力显微镜(AFM)研究天然沸石表面的微观形貌特征和溶解行为

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摘要

Atomic Force Microscopy (AFM) has been used to observe surface features at the micrometer scale in several zeolite samples. In zeolites exhibiting tabular habit, such as heulandite, yugawaralite, and stilbite, the AFM investigation of the well developed {010} form allowed direct mapping of the elementary steps visible on freshly cleaved surfaces. The steps have a thickness invariably corresponding to half-unit cell and they are commonly involved in growth spirals. Dissolution experiments using diluited acidic solutions have also been performed, both under in-situ and ex-situ conditions, in order to observe the structure and/or defect-controlled formation of dissolution pits. Regularly shaped etch pits have been observed on laumontite (both on the {110} prism and on the {-201} pinacoid) and in chabazite, whereas heulandite shows very irregular dissolution figures. In situ dissolution experiments on yugawaralite and chabazite showed anomalous surface swelling and deformation in proximity of structural defects prior to intensive fracturing of the surface layers.
机译:原子力显微镜(AFM)已用于以微米尺度观察几种沸石样品中的表面特征。在表现出片状习性的沸石中,例如赤铁矿,汤河铝榴石和闪锌矿,对发达的{010}形态进行原子力显微镜研究可直接绘制在新近分裂的表面上可见的基本台阶。台阶的厚度始终对应于半晶胞,它们通常参与生长螺旋。为了观察溶蚀坑的结构和/或缺陷控制的形成,还已经在原位和异位条件下使用稀释的酸性溶液进行了溶出实验。在月桂石(在{110}棱镜和{-201}针形上)和菱沸石中均观察到规则形状的蚀刻坑,而辉石显示出非常不规则的溶出度。在Yugawaralite和菱沸石上进行的原位溶解实验表明,在表面层进行强烈压裂之前,结构缺陷附近的表面异常膨胀和变形。

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