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Changes in the body, glaze and enamel compositions of early Meissen porcelain, 1723-c.1740

机译:早期Meissen瓷器,1723-C.1740的身体,釉料和珐琅组合物的变化

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The evolution of early Meissen body, glaze and colorant compositions is examined using X-ray fluorescence spectroscopy (XRF) measurements on three artefacts that can be accurately dated to the period 1723-c.1740. The results are interpreted based on recipes recorded in the earliest documents of the Meissen archives. The pure Aue kaolinite contains low levels of Ti and can be distinguished from secondary clays, for example, clay from Colditz. The excess Ti in the glaze versus the body reported earlier and confirmed by the present authors is explained by the exclusive use of Colditz clay for the glaze, as described in the recipes before 1730, providing a terminus ante quem for Meissen porcelain exhibiting this particular asymmetry. After 1730, the presence of elevated Ti in the body could serve as a marker for the experimental admixture of clays to Aue kaolinite to alter its properties. Based on the detection of As, Ba and Bi, it is suggested that smalt from Erzgebirge was the colorant for blue enamels until at least 1725.
机译:使用X射线荧光光谱(XRF)测量在三个人工制品上检查早期Meissen身体,釉和着色剂组合物的演变,可以准确地日期为1723-C.1740。结果是根据梅森档案的最早文件记录的食谱来解释。纯Aue高岭石含有低水平的Ti,并且可以与来自Colditz的粘土区分开的。釉中的过度Ti与本作者提前报告的身体和本作者的确认是由Colditz Clay用于釉料的独家使用,如在1730年之前的食谱中所述,为迈森瓷器提供展示这种特殊的不对称的末端左侧标题。在1730之后,体内的升高的Ti可能用作用于粘土的实验混合物以改变其性质的粘土的标记物。基于检测为,BA和BI,建议从ErzgeBirge的Smalt是蓝色搪瓷的着色剂,直到至少1725。

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