Vermiculite: Treatments, Applications, and Structural and Physico-Chemical Characteristics
A special issue of Minerals (ISSN 2075-163X). This special issue belongs to the section "Crystallography and Physical Chemistry of Minerals & Nanominerals".
Deadline for manuscript submissions: closed (10 December 2021) | Viewed by 9131
Special Issue Editor
Interests: vermiculites; environmental mineralogy; structural and physico-chemical characterization of minerals; characterization techniques (X-ray: diffraction and fluorescence; spectroscopies: Raman, Mössbauer, infrared; electron microscopies: high-resolution transmission and scanning); archeometry
Special Issue Information
Vermiculite, a phyllosilicate with appearance similar to micas at the macroscopic level, has a structure composed of two T-O-T layers joined by an inter-layer. The T-O-T layer is composed of an octahedral (O) sheet of Mg2+, located between two tetrahedral sheets (T) of Si4+. The inter-layer is formed by an octahedral sheet of Mg2+ bound to oxygens or OH- groups. In addition, it contains water. The isomorphic substitutions, especially in the tetrahedral sheets of Si4+ to Al3+, are very common. Due to the presence of water and OH- groups, vermiculite can undergo hydration–dehydration processes that depend on various factors, such as temperature, pressure, particle size, relative humidity, and chemical composition. The chemical formula of vermiculite is: X4(Y2-3)O10(OH)2M·nH2O, where X represents the tetrahedral positions (Si4+ and Al3+), Y the octahedral positions (Mg2+, Fe2+, Fe3+, Cr3+, Ti4+, etc.), and M represents the cations located in the inter-layer space (Mg2+, Ca2+, K+, Na+, etc.) to compensate the charges, as a consequence of the isomorphic substitutions.
In addition to this vermiculite, there are the so-called commercial vermiculites. These vermiculites consist of various interstratified layers of mica/vermiculite, vermiculite with different states of hydration, mixtures of mica and vermiculite, etc. The main characteristic of commercial vermiculites is their exfoliation and expansion capacity when the vermiculite is abruptly heated, and that occurs due to the loss of water molecules located between the silicate sheets.
Vermiculites can be modified by temperature, pressure, chemical treatments, and irradiation. Unmodified and modified vermiculites are characterized by their industrial and technological applications. These applications are a function of the material’s physical and chemical properties and the treatment it has undergone.
The relationship between structural changes of vermiculite and the chemical and physical treatments could contribute to predicting the environmental fate of toxic metals, and developing methods to remove these metals from contaminated waters or soils. In addition, that relationship could give light to ambiguities about their geological origin.
This Special Issue will focus on treatments and applications of vermiculites in a strict sense as well as commercial vermiculites; as well as their structural, physico-chemical characteristics.
Dr. Celia Marcos Pascual
Guest Editor
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Keywords
- vermiculite
- mixed layers
- treatments physico-chemical
- adsorption of heavy metals and organic products
- structural and physico-chemical properties
- X-ray techniques (diffraction, fluorescence, etc.)
- electron microscopy (high-resolution transmission, scanning electron)
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