Pierre Picot , Tobias Lange , Fabienne Testard , Frederic Gobeaux , Antoine Thill
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Evidence and importance of intermediate nanostructures in the journey from molecular precursors to allophane and imogolite nanocrystals
Nanoparticles often-called proto-imogolites have been identified as an intermediate in the formation process of imogolite nanotubes as early as 1979. Their composition and structure are now well documented in the case of synthetic imogolite. One specific characteristic of proto-imogolite is that they have a curved shape with a local structure close to the one of imogolite. During a growth stage, they evolve toward nanocrystals (allophane, imogolite). Their thorough characterization has so far been difficult. Using synchrotron Small Angle X-ray Scattering coupled with Raman spectroscopy, we observe that proto-imogolites form during the initial stage of the co-precipitation of aluminum and silicon molecular precursors thanks to a reorganization process. The shape of the initial proto-imogolites, before the growth stage, depends on the synthesis conditions and controls the characteristics of the final product. We show using cryo-TEM images that, at the end of the growth stage, non-tubular nanostructures continue to coexist with nanotubes. Protocols to quantify remaining non-tubular nano-objects and purify the samples are discussed.
期刊介绍:
Applied Clay Science aims to be an international journal attracting high quality scientific papers on clays and clay minerals, including research papers, reviews, and technical notes. The journal covers typical subjects of Fundamental and Applied Clay Science such as:
• Synthesis and purification
• Structural, crystallographic and mineralogical properties of clays and clay minerals
• Thermal properties of clays and clay minerals
• Physico-chemical properties including i) surface and interface properties; ii) thermodynamic properties; iii) mechanical properties
• Interaction with water, with polar and apolar molecules
• Colloidal properties and rheology
• Adsorption, Intercalation, Ionic exchange
• Genesis and deposits of clay minerals
• Geology and geochemistry of clays
• Modification of clays and clay minerals properties by thermal and physical treatments
• Modification by chemical treatments with organic and inorganic molecules(organoclays, pillared clays)
• Modification by biological microorganisms. etc...