Abstract
References
- Bilgici Cengiz G. (20189. Transfer factors of 226Ra, 232Th and 40K from soil to pasture‑grass in the northeastern of Turkey. Journal of Radioanalytical and Nuclear Chemistry 329(1); 83-89 Chataigner, C.; Işıklı, M.; Gratuze, B.; Çil, V. (2014). Obsidian Sources in the Regions of Erzurum and Kars (North-East Turkey): New Data. Archaeometry 56(3), 351-374. Chiozzi P., De Felice P., Fazio A., Pasquale V., Verdoya M., (2000). Laboratory application of NaI(Tl) γ-ray spectrometry to studies of natural radioactivity in geophysics. Applied Radiation and Isotopes 53; 127-132. Çolak, A., Aygün H., (2011) Sarıkamış (Kars) civarı obsidiyenleri bilgi notu. MTA. Maden Etüt ve Arama Dairesi Başkanlığı SERKA Raporu. Kars. El-Farrash A.H., Yousef H.A., Hafez A.F., (2012). Activity concentrations of 238U and 232Th in some soil and fertilizer samples using passive and active techniques. Radiation Measurements 47; 644-648 Tzortzis, M., Tsertos, H., Christofides, S., George Christodoulides, G., (2003).Gamma-ray measurements of naturally occuring radioactive samples from Cyprus characteristic geological rocks. Radiation Measurements 37; 221-229. United Nations Scientific Committee on the Effect of Atomic Radiation (2000) Report to the general assembly, Effects and risks of ionizing radiations. United Nations, New York.
Abstract
Obsidian
is a naturally occurring volcanic glass formed as an igneous rock. It is a kind
of alumino-silicate glass containing iron impurities and some tiny particles
(particle-dispersed glasses). It can be found in black, gray, brown, blue, and
green colors in nature. In recent work, the obsidian specimens in black and
brown colors were collected from Sarıkamış which is a small town in Kars
province located at the north-east part of Turkey. The obtained specimens were
then cut and polished to obtain two parallel surfaces to perform optical
measurements. The optical absorption spectra of the samples were collected
under ambient environment. The natural radioactivity levels of the specimens
were also measured using a gamma spectrometer whıch uses a NaI(Tl)
scintillation detector for the determination of the radioactivity.
References
- Bilgici Cengiz G. (20189. Transfer factors of 226Ra, 232Th and 40K from soil to pasture‑grass in the northeastern of Turkey. Journal of Radioanalytical and Nuclear Chemistry 329(1); 83-89 Chataigner, C.; Işıklı, M.; Gratuze, B.; Çil, V. (2014). Obsidian Sources in the Regions of Erzurum and Kars (North-East Turkey): New Data. Archaeometry 56(3), 351-374. Chiozzi P., De Felice P., Fazio A., Pasquale V., Verdoya M., (2000). Laboratory application of NaI(Tl) γ-ray spectrometry to studies of natural radioactivity in geophysics. Applied Radiation and Isotopes 53; 127-132. Çolak, A., Aygün H., (2011) Sarıkamış (Kars) civarı obsidiyenleri bilgi notu. MTA. Maden Etüt ve Arama Dairesi Başkanlığı SERKA Raporu. Kars. El-Farrash A.H., Yousef H.A., Hafez A.F., (2012). Activity concentrations of 238U and 232Th in some soil and fertilizer samples using passive and active techniques. Radiation Measurements 47; 644-648 Tzortzis, M., Tsertos, H., Christofides, S., George Christodoulides, G., (2003).Gamma-ray measurements of naturally occuring radioactive samples from Cyprus characteristic geological rocks. Radiation Measurements 37; 221-229. United Nations Scientific Committee on the Effect of Atomic Radiation (2000) Report to the general assembly, Effects and risks of ionizing radiations. United Nations, New York.
Details
| Primary Language | English |
|---|---|
| Subjects | Engineering |
| Journal Section | Articles |
| Authors | |
| Publication Date | July 25, 2019 |
| Published in Issue | Year 2019Volume: 6 |
