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dc.contributorObradović, Nina
dc.contributorMančić, Lidija
dc.creatorKnežević, Petar
dc.creatorVuković, Nikola
dc.creatorMihajlović, Katarina
dc.creatorVujaković, Marko
dc.creatorPantović-Spajić, Katarina
dc.creatorRadosavljević-Mihajlović, Ana
dc.date.accessioned2023-12-18T10:17:33Z
dc.date.available2023-12-18T10:17:33Z
dc.date.issued2023
dc.identifier.isbn978-86-905714-0-6
dc.identifier.urihttps://ritnms.itnms.ac.rs/handle/123456789/1197
dc.description.abstractOne of the most interesting secondary raw materials within the Kolubara Basin is diatomaceous earth or diatomite, with reserves of 308.670 t in fields B and C. Chemical and mineralogical tests were performed on diatomaceous earth samples. The results of these tests are presented in this paper. Diatomite is a soft sedimentary rock formed by the deposition of cell walls (frustulae) of single-celled algae-diatoms at the bottom of sea and lake basen. Diatom frustules consist of two parts that lie on top of each other and represent a highly porous skeleton of amorphous hydrated silica. Diatom frustule size ranges from 1 μm to 1 mm, usually 10-200 μm.The specific area (SBET (m2/g)) is 47.6. The SEM/EDS, BET and FTIR methods were used for characterization. Based on the presented results, diatomaceous earth can be used in the pharmaceutical, ceramic and food industries.sr
dc.language.isoensr
dc.publisherBelgrade : Serbian Ceramic Societysr
dc.relationinfo:eu-repo/grantAgreement/MESTD/inst-2020/200023/RS//sr
dc.rightsopenAccesssr
dc.sourceThe Eleventh Serbian Ceramic Society Conference »Advanced Ceramics and Application«sr
dc.titleDiatomic earth: Structure and modificationsr
dc.typeconferenceObjectsr
dc.rights.licenseARRsr
dc.citation.epage49
dc.citation.spage49
dc.identifier.fulltexthttp://ritnms.itnms.ac.rs/bitstream/id/2750/bitstream_2750.pdf
dc.type.versionpublishedVersionsr


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