2019
DOI: 10.1180/clm.2019.49
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Mineralogical study of clays from Dobrodo, Serbia, for use in ceramics

Abstract: This study focuses on the mineralogical characterization of four raw clay samples from Dobrodo deposit, Serbia. Several analytical methods were applied to determine the chemical and mineralogical composition, morphology and physical properties (colour, plasticity, specific surface area, particle size and cation-exchange capacity) of the clay samples. Kaolinite, smectite and illite are the predominant phases in all of the samples studied that contain between 60.2 and 87.1 wt.% of clay. Quartz, feldspars, parago… Show more

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Cited by 7 publications
(19 citation statements)
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“…The thermal events at ∼350°C and ∼450°C are indicative of iron minerals (goethite and limonite) and halloysite, which are present in smaller amounts (Norton, 1939;Grim & Rowland, 1944). The broad endothermic event at between 550°C and 650°C represents dehydroxylation of kaolinite and halloysite and transformation to amorphous metakaolinite and metahalloysite, but it could also be indicative of illite minerals (Norton, 1939;Speil et al, 1945;Földvári, 2011;Milošević et al, 2019a). The presence of these phases was confirmed by XRPD and SEM analysis.…”
Section: Mineralogymentioning
confidence: 99%
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“…The thermal events at ∼350°C and ∼450°C are indicative of iron minerals (goethite and limonite) and halloysite, which are present in smaller amounts (Norton, 1939;Grim & Rowland, 1944). The broad endothermic event at between 550°C and 650°C represents dehydroxylation of kaolinite and halloysite and transformation to amorphous metakaolinite and metahalloysite, but it could also be indicative of illite minerals (Norton, 1939;Speil et al, 1945;Földvári, 2011;Milošević et al, 2019a). The presence of these phases was confirmed by XRPD and SEM analysis.…”
Section: Mineralogymentioning
confidence: 99%
“…The clay in the Dobrodo deposit does not have a uniform appearance and chemical composition. It is layered with clays of various colours and shades, from yellow to dark grey, due to differences in mineralogy (Milošević et al , 2019a).
Fig.
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Section: Locality and Materialsmentioning
confidence: 99%
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