Comprehensive Investigation of Neolithic Ceramic Samples: Firing Technology and Age Insights

IF 1 Q3 PHYSICS, MULTIDISCIPLINARY
Sahib Mammadov, Aybeniz Ahadova
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 TL glow-curve intensity at 325°C was measured to estimate the historical dose of the sample, which was found to be 22.19±1.36 Gy. The concentration of U, Th, and K were 2.24±0.20 ppm , 8.31±0.80 ppm, 2.39±0.23% respectively. Dose rate and age calculation were conducted using the DRAC, version 1.2 and output results are as follows: Environmental dose rate: 3.46±0.19 mGy/a; Age of the sample: 4.400±530 BC years which are in line with the stratigraphically estimated age of this area and with the radiocarbon age (4270±160 BC) reported in our previous work. The results obtained from this multidisciplinary approach provide insights into the firing technology and age of the ceramic samples.
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Abstract

Thermogravimetric (TG/DTG), thermoluminescence (TL), and X-ray powder diffraction (XRD) techniques were applied to characterize samples collected from the archaeological site of Polutepe in Azerbaijan, dating to the Neolithic period, and gave new information on the firing technology. The thermogravimetric analysis of ceramic shards from Polutepe revealed that the firing temperature of the samples was in the range of 700°C, based on the presence of calcite in the sample. XRD analysis confirmed the presence of quartz, feldspar, and clay minerals in the ceramic samples. According to XTD analysis the mineral composition of the ceramic sample from Polutepe site was as follows: Quartz-33.8 mass%, Feldspar (albite)-21.7 mass%, Muscovite- 33.6 mass%, and Calcite- 10.9 mass%. TL glow-curve intensity at 325°C was measured to estimate the historical dose of the sample, which was found to be 22.19±1.36 Gy. The concentration of U, Th, and K were 2.24±0.20 ppm , 8.31±0.80 ppm, 2.39±0.23% respectively. Dose rate and age calculation were conducted using the DRAC, version 1.2 and output results are as follows: Environmental dose rate: 3.46±0.19 mGy/a; Age of the sample: 4.400±530 BC years which are in line with the stratigraphically estimated age of this area and with the radiocarbon age (4270±160 BC) reported in our previous work. The results obtained from this multidisciplinary approach provide insights into the firing technology and age of the ceramic samples.
新石器时代陶瓷样品的综合调查:烧制技术和时代洞察
采用热重(TG/DTG)、热释光(TL)和x射线粉末衍射(XRD)技术对阿塞拜疆新石器时代Polutepe考古遗址的样品进行了表征,并为烧制技术提供了新的信息。对来自Polutepe的陶瓷碎片的热重分析表明,基于样品中方解石的存在,样品的烧成温度在700°C范围内。XRD分析证实了陶瓷样品中存在石英、长石和粘土矿物。根据XTD分析,Polutepe遗址陶瓷样品的矿物组成为:石英-33.8质量%,长石(钠长石)-21.7质量%,白云母- 33.6质量%,方解石- 10.9质量%。测定325°C时的TL发光曲线强度,估计样品的历史剂量为22.19±1.36 Gy。U、Th、K的浓度分别为2.24±0.20 ppm、8.31±0.80 ppm、2.39±0.23%。使用DRAC 1.2版本进行剂量率和年龄计算,输出结果如下:环境剂量率:3.46±0.19 mGy/a;样品年龄:4400±530 BC,与本区地层估算年龄和前人报告的放射性碳年龄(4270±160 BC)一致。通过这种多学科方法获得的结果为陶瓷样品的烧制技术和年龄提供了见解。
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来源期刊
East European Journal of Physics
East European Journal of Physics PHYSICS, MULTIDISCIPLINARY-
CiteScore
1.10
自引率
25.00%
发文量
58
审稿时长
8 weeks
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