Characterization of thermoluminescence kinetic parameters of dolomite after exposure to β-radiation dose

Dolomite is a carbonate mineral of calcium and magnesium having the chemical formula CaMg(CO3)(2). It is a reservoir for significant petroleum reserves and mainly used as building and ceramic material. Thermoluminescence (TL) emission of this mineral has been examined in the literature, especially collected from Egypt, India, and Brazil. In this study, the aim is to investigate TL properties of dolomite mineral which has a wide reserve in Mersin/Turkey. Structural, morphological, and elemental analyzes were performed by X-ray Diffraction (XRD) Spectroscopy, Scanning Electron Microscope equipped with Energy Dispersive X-ray Spectrometer (SEM-EDS), and Inductively Coupled Plasma Mass Spectrometer (ICP/MS), respectively. TL measurements were carried out using a TL/OSL reader with a(90)Sr/Y-90 beta source. The natural TL (NTL) curve of the sample showed two peaks at around 255 and 345 degrees C by the wideband blue filter whereas an additional peak at 115 degrees C was observed under the beta irradiation. In addition, at high doses from 50 Gy, a shoulder at around 402 degrees C occurred. The optimum annealing temperature and duration of the sample were determined as 500 degrees C and 30 min. In order to remove the low-temperature peak, a preheating process at 200 degrees C with 23 s duration was applied before each TL readout. TL response to absorbed dose showed good linearity over the 0.1-1200 Gy dose range and the sample was observed to be reusable with only 1.7% change up to 10 cycles under a dose of 100 Gy. The kinetic parameters (activation energy E (eV), frequency factor s (s(-1)), kinetic order b) of the evident glow peaks were estimated using Peak Shape (PS), Various Heating Rate (VHR), Initial Rise (IR), and Computerized Glow Curve Deconvolution (CGCD) methods. The kinetic analysis indicated that the TL glow curve of the preheated sample consists of four individual peaks having activation energies of similar to 1.56, 1.60, 1.78, and 1.73 eV, and these peaks obey second and general-order kinetics.

Automated summary

This study investigated the thermoluminescence (TL) properties of dolomite mineral in Mersin/Turkey, analyzing its structural, morphological, and elemental characteristics, as well as conducting TL measurements and kinetic analysis. The results showed the TL response, reusability, and kinetic parameters of dolomite, providing valuable data for understanding its TL behavior.