TY - JOUR
T1 - Radiation effects on TL and EPR of sodalite and application to dosimetry
AU - Cano, N. F.
AU - Watanabe, S.
AU - Blak, A. R.
AU - Mosqueira Yauri, Jessica
PY - 2010
Y1 - 2010
N2 - Sodalite, Na8Al6Si6O24Cl 2, a natural silicate mineral, has been investigated concerning its thermoluminescence (TL) and electron paramagnetic resonance (EPR) properties. Samples, both natural and heat treated at 500°C for 30min, present an EPR signal at g=2.01132. The irradiation induces two signals at g=2.0008 and a group of 11 lines due to an O- ion in an intermediate position with respect to two adjacent Al nuclei, that are superimposed on the signal at g=2.0008. An annealing at 500 °C/30min produces a broad signal around g∼2.0, probably due to Fe3+ magnetic dipole interactions. The samples were annealed at 500 °C/30min and then irradiated with gamma-ray doses varying from 1 Gy to 20 kGy. All the samples have shown TL peaks at 110, 230 and 270 °C. Similar results were obtained for natural samples. The accumulated dose (AD) was determined to be AD∼2.5 kGy and the annual dose of (0.5950.001) mGy/year was obtained from the concentration of U, Th, and K 2O in the sample. Therefore, the age obtained for natural sodalite was (4.20.2)106 years.
AB - Sodalite, Na8Al6Si6O24Cl 2, a natural silicate mineral, has been investigated concerning its thermoluminescence (TL) and electron paramagnetic resonance (EPR) properties. Samples, both natural and heat treated at 500°C for 30min, present an EPR signal at g=2.01132. The irradiation induces two signals at g=2.0008 and a group of 11 lines due to an O- ion in an intermediate position with respect to two adjacent Al nuclei, that are superimposed on the signal at g=2.0008. An annealing at 500 °C/30min produces a broad signal around g∼2.0, probably due to Fe3+ magnetic dipole interactions. The samples were annealed at 500 °C/30min and then irradiated with gamma-ray doses varying from 1 Gy to 20 kGy. All the samples have shown TL peaks at 110, 230 and 270 °C. Similar results were obtained for natural samples. The accumulated dose (AD) was determined to be AD∼2.5 kGy and the annual dose of (0.5950.001) mGy/year was obtained from the concentration of U, Th, and K 2O in the sample. Therefore, the age obtained for natural sodalite was (4.20.2)106 years.
UR - http://www.scopus.com/inward/record.url?scp=78651109332&partnerID=8YFLogxK
U2 - 10.1088/1742-6596/249/1/012022
DO - 10.1088/1742-6596/249/1/012022
M3 - Artículo
AN - SCOPUS:78651109332
SN - 1742-6588
VL - 249
JO - Journal of Physics: Conference Series
JF - Journal of Physics: Conference Series
M1 - 012022
ER -