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Thermoluminescence response of the larimar rocks
Authors:HL Sullasi  HJ Khoury  V Barros  R Libonati  PL Guzzo  V Asfora  RE De Araujo  M Capriles  J Reyes
Institution:1. Department of Nuclear Energy – UFPE/Recife, Pernambuco, Brazil;2. Department of Mining Engineering – UFPE/Recife, Brazil;3. Department of Electronics and Systems – UFPE/Recife, Brazil;4. Department of Economic Geology – SEIC/Santo Domingo, Dominican Republic
Abstract:The aim of this paper is to evaluate the thermoluminescent (TL) response of a larimar, a variety of pectolite (NaCa2Si3O8OH]). It is a blue pectolite only found on the terrestrial crust of the province of Barahona, in the south-western region of the Dominican Republic. The larimar rock used in this study, presented a light-blue color with brown areas. X-ray powder diffractometry (XRD), showed that the light-blue portion of the rock is composed essentially by pectolite and the brown portion is composed by a mixture of minerals. Aliquots of 5 mg of light-blue portions were irradiated with gamma rays with doses from 10 to 104 Gy and the TL glow curves were obtained from 50 to 400 °C. The glow curve showed a broad peak around 150 °C and a peak near 280 °C. Different pre-heat condition were used to remove the broad peak. The TL emission of the main peak appeared in the region of 580 nm. The TL response of the main peak showed a linear behavior up to 2500 Gy and a sub-linear behavior above this dose value. Studies of the 30 day fading effects in TL signal using a pre-heating temperature around 180 °C during 15 min were carried out and fading near 25% was observed.
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