A Workflow for Uncertainty Assessment in Elemental Analysis of Archaeological Ceramics: A Case Study of Neolithic Coarse Pottery from Eastern Siberia

IF 1.9 0 HUMANITIES, MULTIDISCIPLINARY Heritage Pub Date : 2023-05-20 DOI:10.3390/heritage6050234
Galina V. Pashkova, Mikhail A. Statkus, Maria M. Mukhamedova, Alexander L. Finkelshtein, Irina V. Abdrashitova, Olga Yu. Belozerova, Victor M. Chubarov, Alena A. Amosova, Artem S. Maltsev, Elena I. Demonterova, Dmitriy L. Shergin
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Abstract

In this study, the assessment of uncertainties introduced at different stages of the elemental analysis of archaeological ceramics has been described using the example of the Neolithic pottery sherds from Popovsky Lug (eastern Siberia). To evaluate the uncertainty introduced by sampling due to ceramic heterogeneity, three original sherds were cut into small subsamples. Powdered subsamples (250–350 mg) were analyzed using wavelength-dispersive X-ray fluorescence and inductively coupled plasma mass spectrometry methods, and the variations between analytical results for independent subsamples were compared with the variations introduced during the analytical process (measurement and sample preparation). It was shown that 250–350 mg of ceramic is sufficient to obtain good reproducibility (2–15%) between separate subsamples for most major and trace elements, even for the heterogeneous Neolithic ceramics included in this study. The differing behavior of concentration variations in some elements was explained by measuring the ceramic cross-sections by scanning electron microscopy and micro-X-ray fluorescence spectrometry, as well as by the theoretic modeling of the sampling error. The described workflow can be useful in finding uncertainties in elemental analysis results, which may affect the interpretation of bulk chemical composition in ceramic provenance studies.
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考古陶瓷元素分析中的不确定度评估工作流程——以东西伯利亚新石器时代粗陶为例
在本研究中,以波波夫斯基吕格(东西伯利亚)新石器时代陶器碎片为例,对考古陶瓷元素分析不同阶段引入的不确定性进行了评估。为了评估由于陶瓷非均质性而引入的采样不确定度,将三个原始碎片切割成小的子样本。采用波长色散x射线荧光法和电感耦合等离子体质谱法对250 ~ 350 mg粉末状亚样品进行了分析,并将独立亚样品的分析结果与分析过程(测量和样品制备)中引入的变化进行了比较。结果表明,250-350 mg的陶瓷足以在不同的亚样品之间获得良好的再现性(2-15%),即使是本研究中包括的异质新石器时代陶瓷。用扫描电子显微镜和微x射线荧光光谱法测量了陶瓷的横截面,并对采样误差进行了理论建模,解释了某些元素浓度变化的不同行为。所描述的工作流程可用于发现元素分析结果中的不确定性,这可能会影响陶瓷物源研究中散装化学成分的解释。
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来源期刊
Heritage
Heritage Multiple-
CiteScore
2.90
自引率
17.60%
发文量
165
审稿时长
10 weeks
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