TY  - CONF
AU  - Knežević, Petar
AU  - Vuković, Nikola
AU  - Mihajlović, Katarina
AU  - Vujaković, Marko
AU  - Pantović-Spajić, Katarina
AU  - Radosavljević-Mihajlović, Ana
PY  - 2023
UR  - https://ritnms.itnms.ac.rs/handle/123456789/1197
AB  - One 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.
PB  - Belgrade : Serbian Ceramic Society
C3  - The Eleventh Serbian Ceramic Society Conference »Advanced Ceramics and Application«
T1  - Diatomic earth: Structure and modification
EP  - 49
SP  - 49
ER  - 

@conference{
author = "Knežević, Petar and Vuković, Nikola and Mihajlović, Katarina and Vujaković, Marko and Pantović-Spajić, Katarina and Radosavljević-Mihajlović, Ana",
year = "2023",
abstract = "One 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.",
publisher = "Belgrade : Serbian Ceramic Society",
journal = "The Eleventh Serbian Ceramic Society Conference »Advanced Ceramics and Application«",
title = "Diatomic earth: Structure and modification",
pages = "49-49"
}

Knežević, P., Vuković, N., Mihajlović, K., Vujaković, M., Pantović-Spajić, K.,& Radosavljević-Mihajlović, A.. (2023). Diatomic earth: Structure and modification. in The Eleventh Serbian Ceramic Society Conference »Advanced Ceramics and Application«
Belgrade : Serbian Ceramic Society., 49-49.

Knežević P, Vuković N, Mihajlović K, Vujaković M, Pantović-Spajić K, Radosavljević-Mihajlović A. Diatomic earth: Structure and modification. in The Eleventh Serbian Ceramic Society Conference »Advanced Ceramics and Application«. 2023;:49-49..

Knežević, Petar, Vuković, Nikola, Mihajlović, Katarina, Vujaković, Marko, Pantović-Spajić, Katarina, Radosavljević-Mihajlović, Ana, "Diatomic earth: Structure and modification" in The Eleventh Serbian Ceramic Society Conference »Advanced Ceramics and Application« (2023):49-49.