Undifferentiated Inorganics in Coal Fly Ash and Bottom Ash: Calcispheres, Magnesiacalcispheres, and Magnesiaspheres

During a study aiming to recover strategic elements and minerals from coal fly ash and bottom ash (RAREASH and CHARPHITE projects funded, respectively, by the 2nd ERA-MIN and 3rd ERA-MIN Programs of the European Union Commission), it was found that in coal fly ash and bottom ash from Romania and Pol...

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Bibliographic Details
Published in:Minerals (Basel) 2018-04, Vol.8 (4), p.140
Main Authors: Valentim, Bruno, Białecka, Barbara, Gonçalves, Paula, Guedes, Alexandra, Guimarães, Renato, Cruceru, Mihai, Całus-Moszko, Joanna, Popescu, Luminiţa, Predeanu, Georgeta, Santos, Ana
Format: Article
Language:English
Subjects:
Airborne particulates
Amorphous materials
Bottom ash
Coal
Electron microscopy
Fly ash
Iron
Light microscopy
Magnesium oxide
Microscopes
Microscopy
Minerals
Nodules
Nomenclature
Optical microscopy
Periclase
Scanning electron microscopy
Silicates
Surveying
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Summary:During a study aiming to recover strategic elements and minerals from coal fly ash and bottom ash (RAREASH and CHARPHITE projects funded, respectively, by the 2nd ERA-MIN and 3rd ERA-MIN Programs of the European Union Commission), it was found that in coal fly ash and bottom ash from Romania and Poland, several morphotypes did not fit into the general fly ash classifications, unless grouped together as “undifferentiated inorganics”. However, the combination of reflected light optical microscopy under oil immersion, scanning electron microscopy, and X-ray microanalysis (SEM/EDS) showed that many of these morphotypes not only have distinctive petrographic patterns but are also characterized by a chemical assemblage dominated by Ca, Mg, and P. In this paper, a survey of the literature is presented together with several detailed studies of samples from the RAREASH and CHARPHITE projects from which the following nomenclature are proposed: “calcispheres” for spongy Ca-rich morphotypes, “calcimagnesiaspheres” for (Ca + Mg)-rich morphotypes with visible MgO nodules and/or periclase (MgO) exsolved from Ca aluminate-silicate glass, and “magnesiaspheres” divided into “magnesiaferrospheres” for (Mg + Fe)-rich morphotypes with magnesioferrite, and “magnesiaoxyspheres” for magnesiaspheres mainly composed of (Mg + Fe)-rich amorphous material with visible MgO nodules and/or periclase.
ISSN:2075-163X
2075-163X
DOI:10.3390/min8040140