4.5 Article

Raman study of rusty oil spotted glaze produced in Linfen kilns (Shanxi province, AD 1115-1368)

期刊

JOURNAL OF RAMAN SPECTROSCOPY
卷 53, 期 3, 页码 582-592

出版社

WILEY
DOI: 10.1002/jrs.6229

关键词

hematite; Linfen kilns; microstructure; pseudobrookite; epsilon-Fe2O3

资金

  1. China National Key RD Program [2019YFC1520202, 2019YFC1520103]
  2. Shaanxi University of Science and Technology
  3. French National Centre for Scientific Research
  4. CNRS [186116]
  5. PHC CAI YUANPEI Project [46284PB]
  6. Silicate Cultural Heritage Protection and Utilization Innovation Team of Shaanxi Province [2020TD-008]
  7. Shaanxi Natural Science Basic Research Project [2020JQ-721, 2021JZY014]
  8. China National Natural Science Foundation [51902192, 51972201]

向作者/读者索取更多资源

The Linfen kiln complex is known for its oil spotted glazed ware production, and this study used micro-Raman spectroscopy to analyze the nature of the rusty oil spot pattern. Hematite crystals were found in the glaze, with their distribution suggesting how they are carried towards the surface during firing. Additionally, the study revealed variation in band position and FWHM of the spectra due to partial substitution of Fe ions in the hematite crystals.
The Linfen kiln complex, one of the most representative of Shanxi kilns, is famous for its oil spotted glazed ware production. In this work, micro-Raman spectroscopy was applied to analyze the nature of the rusty oil spot pattern of a bowl fragment from Linfen kilns. Crystals of polygonal shape found in the spots at the glaze surface and around bubbles in the cross-section of the glaze were identified as hematite. Their distribution in the glaze suggests that nucleation seeds and small crystals are carried toward the surface by the rise of bubbles during the heating step of the firing. Raman spectra combined with energy-dispersive spectrometry (EDS) measurements also suggest that Fe ions in hematite crystals are partially substituted, causing the variation of band position and full width at half maximum (FWHM) of the spectra. Dendritic epsilon-Fe2O3 was identified in brown areas of the black glaze, as well as pseudobrookite crystals of tens of microns in the cross-section of the glaze. The degree of the glaze polymerization (A(500)/A(1000)) was calculated at 1.85, indicating a firing temperature lower than 1300 degrees C, consistent with the archaeological data.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.5
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据