Distribution of elemental compositions of zeolite quarries and calculation of radiogenic heat generation
Yazarlar (4)
Prof. Dr. Şeref TURHAN Kastamonu Üniversitesi, Türkiye
S. Tokat Kastamonu Üniversitesi, Türkiye
Prof. Dr. Aslı KURNAZ Kastamonu Üniversitesi, Türkiye
A. Altıkulaç
Muğla Sıtkı Koçman Üniversitesi, Türkiye
Muğla Sıtkı Koçman Üniversitesi, Türkiye
| Makale Türü | Özgün Makale (SSCI, AHCI, SCI, SCI-Exp dergilerinde yayınlanan tam makale) | ||
| Dergi Adı | International Journal of Environmental Analytical Chemistry (Q3) | ||
| Dergi ISSN | 0306-7319 Dergi Bilgileri (2022) | ||
| Dergi Tarandığı Indeksler | SCI-Expanded | ||
| Makale Dili | İngilizce | Basım Tarihi | 12-2022 |
| Cilt / Sayı / Sayfa | 102 / 19 / 7851–7862 | DOI | 10.1080/03067319.2020.1839439 |
| Makale Linki | https://www.tandfonline.com/doi/abs/10.1080/03067319.2020.1839439 | ||
| UAK Araştırma Alanları |
Nükleer Fizik
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| Özet |
| The effectiveness ofthe use of zeolites in different industrial processes depends on their physical-chemical properties that are distinctly connected to their geological deposits. In this study, major oxides, eco-toxic metals (Cr, Co, Ni, Cu, Zn, As, Zr, Cd and Pb), and rare earth (Y, La, Ce, Pr and Nd), radioactive (Th and U) and other trace elements contents of eighty-one zeolite samples collected from four different zeolite quarries in Gördes in Turkey were analysed by using energy dispersed X-ray fluorescence spectrometer. Also, pH values and SiO2/Al2O3 ratios were determined for zeolite samples. In addition, radiogenic heat generation (RHG) caused by radiations emitted from uranium (U), thorium (Th) and radioactive potassium (40K) in zeolite samples wereestimated.Gördes zeolite contains major oxides, on average, 75.1% SiO2, 14.1% Al2O3, 3.2% K2O, 2.4% CaO, 1.7% Fe2O3, 1.4% MgO, 1.3% Na2O. The … |
| Anahtar Kelimeler |
| eco-toxic metal | Gördes | major oxides | radiogenic heat generation | thorium | uranium | Zeolite |
BM Sürdürülebilir Kalkınma Amaçları
| Atıf Sayıları | |
| Scopus | 6 |
| Google Scholar | 10 |