التفاصيل البيبلوغرافية
| العنوان: |
宋代黑釉茶盏油滴的 飞行时间二次离子质谱表征. (Chinese) |
| Alternate Title: |
Characterization of Oil Spots on Black-Glazed Teabowl Made in Song Dynasty by Time-of-Flight Secondary Ion Mass Spectrometry. (English) |
| المؤلفون: |
徐子琪, 赵煊赫, 梁汉东, 李展平, 铁偲 |
| المصدر: |
Journal of Chinese Mass Spectrometry Society; Jan2023, Vol. 44 Issue 1, p25-33, 9p |
| مصطلحات موضوعية: |
SECONDARY ion mass spectrometry, MINERALS, HEMATITE crystals, GLAZES, DEPTH profiling, SONG dynasty, China, 960-1279, CATIONS |
| مصطلحات جغرافية: |
CHINA |
| Abstract (English): |
The ancient porcelain is the treasure of Chinese civilization. In this paper, multiple surface analysis tools were applied to characterize the attractive silvery bright spots on the glaze of black-glazed tea bowl fragment. The raindrop-shaped silver flecks covering the surface were symbols of North China oil spots. High-resolution time of flight-secondary ion mass spectrometry（TOF-SIMS） data confirmed the main component of the oil spot was iron oxide. Positive ions were Fe+（m/z 55.93）, FeO+（m/z 71.93）, Fe2O+（m/z 127.86）, and negative ions were FeO-（m/z 71.93）, FeO-2（m/z 87.92）. A series of peaks were detected by micro-Raman spectroscopy, such as 230, 294, 412, 502, 611, 1 337 cm-1. This suggested existence of hematite（α-Fe2O3） in the spot. Secondary ion imaging of TOF-SIMS indicated the oil spots（～120 μm） was formed by self-organization and dispersion of hundreds hexagonal hematite crystal（～2-10 μm）. Hematite was spatially complementary to alkaline calcareous glaze that contains silicon, aluminum, calcium, and sodium. TOF-SIMS depth profiling of the spot suggested a more than 5 μm continuous hematite layer on the glaze of black-glazed tea bowl. The main mineral of α-Fe2O3 crystals was hematite, which was ochre usually. Specular hematite, a subspecies of hematite with silver or black color, was believed to play critical role in the formation of the oil spot. With the optical microscope observations, we believed that the silvery material on the surface of the oil spots should be a thin layer of specular hematite and the lower ochre layer was hematite. In fact, the oil spot appeared silvery-white and reflective when viewed from 15° to 165°, while it appeared ochre when the angles of gaze was not greater than 15° from the glazed surface of the specimen. The extraordinary visual property of color changing with different angle of gaze formed the charm of Song dynasty oil spot tea bowls. With these results, a hypothesis for the formation of the North China oil spots was enlightened. The molten phase of Fe-rich soy-black glaze gradually formed micron-sized hematite particulates at sealed kiln of high temperature（1 250 ℃）. When the kiln was unsealed, the hot porcelain was exposed to cold air immediately. A thin layer of specular hematite was generated on top of hematite particulates. [ABSTRACT FROM AUTHOR] |
| Abstract (Chinese): |
本研究利用飞行时间二次离子质谱 (TOF-SIMS) 表征典型黑釉茶盏釉面上银色反光斑纹, 即华北油滴. 高分辨质谱测定油滴的主要成分是氧化铁, 由显微拉曼光谱确定其矿物形式是赤铁矿 (α-Fe2O3). 二次离子质谱 (SIMS) 离子成像进一步揭示: 该赤铁矿呈六方柱晶体 (约2～10μm); 近百余枚这样的晶体自组织分散排列构成类似雨滴状的斑纹 (约120μm); 与其形貌互补的是含硅、铝、钙、钠等元素的碱性石灰质釉质. SIMS深度剖析发现, α-Fe2O3晶体的连续深度不小于5μm. 基于SIMS表征结果, 还探讨了赤铁矿沉积薄膜状镜铁矿 (α-Fe2O3) 引起华北油滴呈银色与镜面反射现象的原理, 以及TOF-SIMS在表征和研究古瓷方面的潜力和局限. [ABSTRACT FROM AUTHOR] |
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| قاعدة البيانات: |
Complementary Index |