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硫酸亚铁煅烧温度对中国古代传统铁红釉上彩呈色影响的研究

Study on the Influence of Calcination Temperature of Iron Vitriol on the Coloration of Ancient Chinese Traditional Iron Red Overglaze Color.

作者信息

Li Qijiang, Wu Anjian, Zhang Maolin, Li Jinwei, Cao Jianwen, Li Haorui, Jiang Yimei

机构信息

Research Center of Ancient Ceramic, Jingdezhen Ceramic University, Jingdezhen 333001, China.

Jiangxi Ceramic Heritage Conservation and Imperial Kiln Research Collaborative Innovation Center, Jingdezhen 333001, China.

出版信息

Materials (Basel). 2024 Jun 7;17(12):2800. doi: 10.3390/ma17122800.

DOI:10.3390/ma17122800
PMID:38930171
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11204637/
Abstract

Iron red, a traditional Jingdezhen overglaze color, is primarily colored with iron oxide (FeO). In traditional processes, the main ingredient for the iron red overglaze color, raw iron red, is produced by calcining iron vitriol (FeSO·7HO). Analysis of ancient iron red porcelain samples indicates that the coloration is unstable, ranging from bright red to dark red and occasionally to black. Addressing this, the present study, from a ceramic technology standpoint, conducts a series of calcination experiments on industrial iron vitriol at varying temperatures. Utilizing methodologies such as differential scanning calorimetry-thermogravimetry (DSC-TG), Raman spectroscopy, X-ray diffraction (XRD), scanning electron microscopy with X-ray energy dispersive spectrometry (SEM-EDS), and optical microscopy (OM), this research scientifically explores the impact of iron vitriol's calcination temperature on the coloration of traditional Jingdezhen iron red overglaze color. The findings indicate that from room temperature to 550 °C, the dehydration of iron vitriol resulted in the formation of Fe(SO) and a minimal amount of α-FeO, rendering the iron red overglaze color a yellowish-red shade. At 650 °C, the coexistence of Fe(SO) and α-FeO imparted a brick-red color to the iron red. As the temperature was elevated to 700 °C, the desulfurization of Fe(SO) produced α-FeO, transitioning the iron red to an orange red. With further temperature increase to 750 °C, the particle size of α-FeO grew and the crystal reflectivity decreased, resulting in a purplish-red hue. Throughout this stage, the powder remained in a single α-FeO phase. Upon further heating to 800 °C, the crystallinity of α-FeO enhanced, giving the iron red overglaze color a dark red or even black appearance.

摘要

铁红是一种传统的景德镇釉上彩,主要由氧化铁(FeO)着色。在传统工艺中,铁红釉上彩的主要原料生铁红是通过煅烧绿矾(FeSO·7HO)制成的。对古代铁红瓷器样本的分析表明,其颜色不稳定,从鲜红色到深红色,偶尔还会变成黑色。针对这一问题,本研究从陶瓷工艺的角度,对工业绿矾在不同温度下进行了一系列煅烧实验。利用差示扫描量热-热重分析法(DSC-TG)、拉曼光谱、X射线衍射(XRD)、扫描电子显微镜-能谱仪(SEM-EDS)和光学显微镜(OM)等方法,本研究科学地探究了绿矾煅烧温度对传统景德镇铁红釉上彩颜色的影响。研究结果表明,从室温到550℃,绿矾脱水生成Fe(SO)和少量α-FeO,使铁红釉上彩呈现出黄红色调。在650℃时,Fe(SO)和α-FeO共存,使铁红呈现砖红色。当温度升高到700℃时,Fe(SO)脱硫生成α-FeO,铁红转变为橙红色。随着温度进一步升高到750℃,α-FeO的粒径增大,晶体反射率降低,呈现出紫红色调。在这个阶段,粉末一直处于单一的α-FeO相。进一步加热到800℃时,α-FeO的结晶度增强,使铁红釉上彩呈现出深红色甚至黑色。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fcbf/11204637/14049bd0b05f/materials-17-02800-g009a.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fcbf/11204637/aeaec9036c78/materials-17-02800-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fcbf/11204637/452dd28a7d40/materials-17-02800-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fcbf/11204637/4f342b9f5173/materials-17-02800-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fcbf/11204637/4bdcf391fa8e/materials-17-02800-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fcbf/11204637/ed017007c4a9/materials-17-02800-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fcbf/11204637/c8d4d24cd442/materials-17-02800-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fcbf/11204637/c19bd7f359a2/materials-17-02800-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fcbf/11204637/a0e210cf0691/materials-17-02800-g008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fcbf/11204637/14049bd0b05f/materials-17-02800-g009a.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fcbf/11204637/aeaec9036c78/materials-17-02800-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fcbf/11204637/452dd28a7d40/materials-17-02800-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fcbf/11204637/4f342b9f5173/materials-17-02800-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fcbf/11204637/4bdcf391fa8e/materials-17-02800-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fcbf/11204637/ed017007c4a9/materials-17-02800-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fcbf/11204637/c8d4d24cd442/materials-17-02800-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fcbf/11204637/c19bd7f359a2/materials-17-02800-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fcbf/11204637/a0e210cf0691/materials-17-02800-g008.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fcbf/11204637/14049bd0b05f/materials-17-02800-g009a.jpg

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