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作 者:陈尧成[1] 张福康[1] 张筱薇[1] 蒋忠义[2] 李德金[2]
机构地区:[1]中国科学院上海硅酸盐研究所,200050 [2]中国社会科学院考古研究所,100000
出 处:《中国陶瓷》1995年第2期40-44,共5页China Ceramics
基 金:国家自然科学基金
摘 要:1990年,在扬州唐代遗址出土14片青花瓷片,经测试分析发现:(1)样品产地很可能在巩县窑。(2)所用钴料属伴生有少量铁和铜的硫钴矿或方硫钴矿着色。(3)该钴料可能来自南非、中亚、甘肃或河北某钴硫化物矿与黄铜矿伴生的矿区。In 1990,the ruins in Tang Dynasty were scientifically excavated in Yangzhou by the Institute of Archaeology,Chinese Academy of Social Sciences and other organizations-Fourteen sherds of blue and white wares were discovered in the stratum of Tang culture. One blue and white sample was scientifically investigated by means of modern instruments.It was found that (l)The sample was fired in Gungxian kiln?2)The cobalt pigment used for Tang blue and white wares is different from those for Yuan,Ming and Qing blue and white.it was a iinnaeite or cattierite mineral containing a small amount of Fe and Cu,(3)The cobalt pigment used in Tang Dynasty was not imported from Persia,two possible sources of the pigment were suggested (a)the western merchants obtained the cobalt mineral from South Africa, Central Asia or Gansu in China, and then carried to Gungxian through the Silk Road, (b)the cobalt mineral might be obtained from the mine field somewhere in Hebei Province where chalcopyrite and sulphide of cobait mineral occur together.
分 类 号:TQ174.47[化学工程—陶瓷工业] K876.3[化学工程—硅酸盐工业]
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