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德化窑遗址出土南宋白瓷的劣化研究OACHSSCD

Study on the deterioration of Southern Song white porcelain unearthed from the Dehua kiln site

中文摘要英文摘要

德化窑是中国南方著名民窑,在窑址出土的南宋白瓷中,釉面局部被黄色硬结层附着是较为普遍的现象.本工作针对一件附着黄色硬结层的南宋德化窑白瓷标本,采用光学显微镜观察(OM)、能量色散X射线荧光光谱分析(EDXRF)、微区拉曼光谱分析(μ-Raman)和扫描电子显微镜-能谱分析(SEM-EDS)等方法分别对标本本体和黄色硬结层进行分析,探讨德化地区土壤环境下釉的劣化机理和硬结层的形成原因.研究表明,南宋德化白瓷釉为透明钙碱釉,在酸性土壤环境中主要发生离子交换和网络溶解反应,释放的硅在釉面缩聚形成硅凝胶,局部微环境的酸碱度差异导致硅凝胶产生两种特殊的显微结构.黄色硬结层由硅凝胶和土壤无机胶体通过静电引力、分子间作用力等凝聚而成.

Dehua kiln was a famous folk kiln in Southern China with a long history.The surfaces of Dehua white porcelain unearthed from the kiln site are generally attached with yellow induration.Based on a comprehensive analysis of a Southern Song white porcelain sample with yellow induration,this study investigated the deterioration mechanism of the glaze and the formation of induration deposits in the soil environment of Dehua.The analytical methods used include optical microscopy(OM),energy dispersive X-ray fluorescence(EDXRF)spectrometry,micro-Raman(μ-Raman)spectrometry and scanning electron microscopy-energy dispersive spectrometry(SEM-EDS).The results indicate that the Southern Song Dehua glaze is a transparent calcium-alkali glaze.The main degradation processes in an acidic soil environment include ion exchange and network dissolution.Silicon released during network dissolution subsequently condensed to form silica gel on the glaze surface,and variations in local pH led to the development of two special microstructures of silica gel.The yellow induration layer was formed through the condensation of silica gel and inorganic soil colloids via electrostatic attraction and intermolecular force.

丁娆;李伟东;徐嫦松

中国科学院上海硅酸盐研究所,上海 201899||中国科学院大学,北京 100049||古陶瓷科学研究国家文物局重点科研基地(中国科学院上海硅酸盐研究所),上海 201899中国科学院上海硅酸盐研究所,上海 201899||中国科学院大学,北京 100049||古陶瓷科学研究国家文物局重点科研基地(中国科学院上海硅酸盐研究所),上海 201899中国科学院上海硅酸盐研究所,上海 201899||中国科学院大学,北京 100049||古陶瓷科学研究国家文物局重点科研基地(中国科学院上海硅酸盐研究所),上海 201899

社会科学

德化窑南宋白瓷黄色硬结层土壤环境硅凝胶

Dehua kilnSouthern Song white porcelainYellow indurationSoil environmentSilica gel

《文物保护与考古科学》 2026 (1)

52-62,11

国家重点研发计划项目(2023YFF0905803)资助

10.16334/j.cnki.cn31-1652/k.20241103401

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