2007
DOI: 10.1039/b701301a
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Differentiating fundamental structural units during the dissolution of zeolite A

Abstract: In situ atomic force microscopy (AFM) is used to differentiate temporally both structure and mechanism in the removal of fundamental structural units during the dissolution of zeolite A.

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Cited by 22 publications
(18 citation statements)
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“…[23,25] All three surface terminations have been revealed in either ex situ or in situ dissolution AFM studies of aluminosilicate zeolite A. [26][27][28] Atomistic simulations on siliceous zeolite A have found these three terminations to be close in energy, with termination at the S4Rs of complete sodalite cages to be the most stable. [25,28] Simulations for zeolite A reveal the same trend.…”
Section: Resultsmentioning
confidence: 99%
“…[23,25] All three surface terminations have been revealed in either ex situ or in situ dissolution AFM studies of aluminosilicate zeolite A. [26][27][28] Atomistic simulations on siliceous zeolite A have found these three terminations to be close in energy, with termination at the S4Rs of complete sodalite cages to be the most stable. [25,28] Simulations for zeolite A reveal the same trend.…”
Section: Resultsmentioning
confidence: 99%
“…Upon dissolution, the most fragile bonds in a structure are broken so that discrete units are removed from the surface. This implies dissolution does not involve a statistical removal of arbitrary "pieces", but rather the extraction of discrete well-defined species, so that the remaining surface ideally consists of closed tiles only [4,5]. This process can be observed with 'contact-mode' Atomic Force Microscopy (AFM), revealing the relevance of NBUs in describing a zeolite crystal.…”
Section: Introductionmentioning
confidence: 99%
“…The potential of 'contact-mode' AFM for investigating the growth of zeolites was initially demonstrated by Brent et al (2008) for zeolite L [6] and by Meza et al (2007) for zeolite A [5]. Very recently, Anderson et al (2017) extended this approach and combined the information on prevailing growth patterns and features on the crystal surface with other techniques to gain deeper insight in the crystal growth.…”
mentioning
confidence: 99%
“…Surface terraces of one unit cell or a simple fraction of a unit cell are frequently observed. 5,8,11 Terrace shapes are usually consistent to a greater or lesser degree with the symmetry at the surface of the crystal. 11 These observations are consistent with certain surface structures being much preferred with lower free energies.…”
Section: Generic Model Of Crystal Growthmentioning
confidence: 97%