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The presence of calcite in archeological ceramics

机译:方解石在考古陶瓷中的存在

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摘要

The present work describes the methods for detecting and classifying calcite in archeological ceramics, the forms of calcite and their interpretation in archeometric terms. Calcite appears in form of coarse granules and fine particles, and its origin can be primary or secondary. Coarse granules can be polycrystalline or mono-crystals of calcite. Fragments of shells, fossils or microfossils are also found. Primary calcite is the initial calcite preserved in low-fired pottery. Secondary calcite, formed after the ceramic firing, may be reformed (re-carbonated) calcite, precipitated calcite or calcite from alteration. The firing can cause the formation of a 'reaction rim' around coarse granules of calcite, while strong decomposition of coarse calcite causes the formation of 'calcite ghosts'. The identification of the forms of calcite gives information on raw materials, the firing temperature and the manufacturing technology of the pottery.
机译:本工作描述了考古陶瓷中方解石的检测和分类方法,方解石的形式及其在考古学上的解释。方解石以粗颗粒和细颗粒的形式出现,其起源可以是主要的或次要的。粗粒可以是方解石的多晶或单晶。还发现了贝壳,化石或微化石的碎片。主要方解石是保存在低烧陶器中的初始方解石。陶瓷烧成后形成的次级方解石可以重整(重新碳化)方解石,沉淀的方解石或因改变而产生的方解石。烧成会导致方解石粗粒周围形成“反应边缘”,而粗方解石的强分解会导致“方解石鬼影”的形成。方解石形式的鉴定给出了有关原材料,烧成温度和陶器制造技术的信息。

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