X-Ray Diffraction Crystalline Microstructure of Minerals

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 (27 August 2021) | Viewed by 1996

Special Issue Editors


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Department of Geology, University of Valencia, 46100 Burjasot (Valencia), Spain
Interests: applied mineralogy; X-ray diffraction; microstructural analyisis; clay mineralogy; ceramics; fillers
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Guest Editor
Establecimientos Baixens S.L.Paints area. R&D Lab. Pol. Ind. Moncarra, s/n. 46230 Alginet, Valencia, Spain
Interests: X-ray diffraction; microstructural analysis; kaolinite; electronic microscopy; hydrothermal synthesis
Special Issues, Collections and Topics in MDPI journals

Special Issue Information

Dear Colleagues,

Most minerals and materials are mainly made of polycrystals. Powder X-ray diffraction analysis of their ideal crystals concerns mainly identification, quantification and structure refinements, while that of non-ideal crystals concerns the real microstructure (crystallite size, shape, strain), texture, stress and distortions. A variety of methods have been developed to analyze the microstucture by X-ray powder diffraction in order to characterize defects, composition variations and crystallite size, shape and microstrains. The X-ray line (or peak) profile analysis (LPA) used for the study of crystalline microstructures started with the investigation of the crystallite size of colloidal particles of noble metals by Scherrer in 1918. In a simplified way, it has been established that the broadening of the diffraction peaks results from two main contributions that are crystallite (the domain which can be considered as a perfect crystal) size and lattice microstrains. Line profile parameters give information about the size and shape of crystallites together with the distribution of sizes and microstrains, the nature of dislocations and the occurrence of faults or mistakes in the structure. There are different procedures to extract contributions, and the most widely used results are those concerning average crystallite sizes and crystallite size distributions, which in anisotropic crystals refer to particular diffraction directions. Observation with microscopy techniques of high resolution and magnification (HRTEM, FESEM, AFM, etc.) allows the recognition of correspondences or correlations between measured values, or possible aggregation mechanisms. Different size distributions frequently reveal different growth mechanisms. The appreciated microstructural characteristics can be applied to the discrimination of genetic processes, both in the natural and industrial production of crystalline solids. Microstructural parameters are frequenly used in the evaluation of mineral processing and in the production of materials, as well as in the characterization of geological units.

Prof. Dr. Joaquín Bastida
Dr. Pablo Rafael Pardo Ibáñez
Guest Editors

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Keywords

  • X-ray powder diffraction;
  • line profile analysis (LPA);
  • line profile fitting;
  • line profile parameters;
  • crystallite size;
  • crystallite size distribution (CSD);
  • crystalline microstructure;
  • minerals;
  • materials

Published Papers (1 paper)

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Research

18 pages, 3467 KiB  
Article
Powder XRD Study of Changes of Cd2+ Modified Clinoptilolite at Different Stages of the Ion Exchange Process
by Louiza Dimowa and Yana Tzvetanova
Minerals 2021, 11(10), 1130; https://doi.org/10.3390/min11101130 - 14 Oct 2021
Cited by 5 | Viewed by 1497
Abstract
Cadmium exchange on clinoptilolite is performed and structurally studied for different durations of the ion exchange process (2 h, 24 h, 72 h, 168 h, 12 days, 22 days) at room temperature and 90 °C. The distribution of Cd2+ ions in all [...] Read more.
Cadmium exchange on clinoptilolite is performed and structurally studied for different durations of the ion exchange process (2 h, 24 h, 72 h, 168 h, 12 days, 22 days) at room temperature and 90 °C. The distribution of Cd2+ ions in all samples is elucidated after exchange on clinoptilolite using powder XRD data processed by Rietveld structural software. Clinoptilolite is not selective for cadmium cations, but at 90 °C the exchange is ~2.5 cations per unit cell. At RT it reaches ~1.25 cations per unit cell being twice as low. The obtained maximum exchanged sample for 22 days 90 °C was structurally refined in order to find the cadmium positions in the clinoptilolite voids. The structural refinements of the occupations of the incoming and outgoing cations give an idea of how the intracrystalline diffusion is processed. A good correlation between results obtained by structural refinement of the Cd-exchanged samples and the data of the EDS measurements was achieved. Full article
(This article belongs to the Special Issue X-Ray Diffraction Crystalline Microstructure of Minerals)
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