Characterization of the zeolitic tuff from the 'Igros-Vidojevici' deposit regarding geological and technological aspects

التفاصيل البيبلوغرافية
العنوان: Characterization of the zeolitic tuff from the 'Igros-Vidojevici' deposit regarding geological and technological aspects
المؤلفون: Zivko Sekulic, Slavica Mihajlović, Jovica Stojanović, Vladimir Simić, Milan Kragović, Vladan D. Kašić, Dragana Zivotic
المصدر: Hemijska Industrija, Vol 72, Iss 1, Pp 29-37 (2018)
بيانات النشر: National Library of Serbia, 2018.
سنة النشر: 2018
مصطلحات موضوعية: Physics, Zeolite, Cation-exchange capacity, General Chemical Engineering, 02 engineering and technology, General Chemistry, X-Ray powder diffraction analysis, lcsh:Chemical technology, 010402 general chemistry, 021001 nanoscience & nanotechnology, 01 natural sciences, 0104 chemical sciences, 13. Climate action, lcsh:TP1-1185, Footwall, Thermal analysis, Fourier transform Infrared spectroscopic analysis, 0210 nano-technology, Nuclear chemistry
الوصف: This study presents investigations of zeolitic tuff samples from the “Igroš- -Vidojevići” deposit. The aim of the research was to determine the quality of samples taken from all deposit parts. Thus, samples were taken from the footwall (“Zeolit 1”), and four samples from the central deposit part (“Zeolit 2”, “Zeolit 3”, “Zeolit 4” and “Zeolit 5”). Characterization of the samples included chemical analysis, determination of the adsorption coefficient for methylene blue dye and cation-exchange capacity (CEC), X-ray powder diffraction analysis (XRPD), differential thermal and thermogravimetric analysis (DTA and TGA), and Fourier transform Infrared spectroscopic analysis (FTIR). Results have shown that the footwall consists mostly of clays, whereas zeolite minerals dominate in the rest of the deposit. XRD analysis of the “Zeolit 1” sample confirmed presence of smectite and kaolinite clays, while zeolite of analcime type and quartz are present as smaller fractions. Chemical composition analysis and determination of heavy metal contents showed a significant amount (7.58%) of Fe2O3 in this sample. Therefore, further research can be pursued to find a method for removal of magnetic impurities in this deposit portion in order to utilize the clay fraction. On the other hand, according to XRD, FTIR, DTA/TGA and SEM/EDS analyses, samples which belong to the central deposit part (“Zeolit 2–5”) consist of clinoptilolite zeolite type, while clays are present in less than 10%. Thus, clays (smectites and kaolinite) accompanied with analcime and quartz are the most abundant footwall minerals while central deposit parts contain predominantly clinoptilolite accompanied with small amounts of clays. Mineragenetically, zeolites are most abundant in the “Zeolit 2” and “Zeolit 3” samples. The smallest value of CEC was determined for the “Zeolit 1” sample (46.98 mmol/100g). According to CEC values determined for “Zeolit 2” and “Zeolit 3” (141.99 and 121.01 mmol/100 g, respectively) these samples are of the best quality, and could be utilized as adsorbents of inorganic pollutants from contaminated waters. Moreover, they could be potentially used for removal of mycotoxins from cattle feed. “Zeolit 4” and “Zeolit 5” samples have shown slightly lower CEC values (89.48 and 83.75 mmol/100 g, respectively), which implies lower quality, and, therefore, could be used for soil quality improvement. Finally, determination of the external CEC has revealed a significant difference between “Zeolit 1” and “Zeolit 5” samples (17.9 and 5.31 mmol/100 g, respectively). [Project of the Serbian Ministry of Education, Science and Technological Development, Grant no. TR34013 and Grant no. TR33007]
تدمد: 2217-7426
0367-598X
الوصول الحر: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::525a1833c697752638d94fa24ccab0c0Test
https://doi.org/10.2298/hemind170428015kTest
حقوق: OPEN
رقم الانضمام: edsair.doi.dedup.....525a1833c697752638d94fa24ccab0c0
قاعدة البيانات: OpenAIRE