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Deterioration of Pre-Hispanic Stucco Masks from the Archaeological Mayan Site of Edzna, Campeche, Mexico

机译:墨西哥坎佩切州埃兹纳考古玛雅遗址的西班牙裔前灰泥面具的恶化

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This contribution shows the results of a study carried out in order to determinate the deterioration mechanisms suffered by stucco masks from the important archaeological Mayan site of Edzna, Campeche, Mexico; due to their long exposition to the tropical environment of the zone. Stratigraphic analysis of fragments from the masks containing pigments and surface neoformation products, were analyzed by optical microscopy and scanning electron microscopy coupled to a secondary X-ray emission system. Crystalized salts mineral composition were characterized by X-ray diffraction. Also, during the study, environmental parameter like temperature and relative humidity were monitored in site. Results indicate that stuccos mineral matrix is formed by calcareous materials, covered by films with variable proportions of ferrous materials (red, ochre and yellow colors) and rich carbon content (black color). Compounds were associated to blue and green colors. Al these materials showed a high level of deterioration because of differential forces caused by stucco and deposits of environmental soluble salts during dissolution crystallization cycles caused by humidity differences between stucco and environmental as a consequence of their particular exposure conditions.
机译:这一贡献显示了一项研究结果,目的是确定墨西哥坎佩切州埃兹纳重要考古玛雅遗址上的灰泥面具遭受的破坏机理;由于它们长期暴露于该地区的热带环境中。通过光学显微镜和扫描电子显微镜与二次X射线发射系统耦合,分析了含有颜料和表面新形成产物的口罩中碎片的地层分析。通过X射线衍射表征结晶的盐矿物组成。此外,在研究过程中,现场监测了诸如温度和相对湿度等环境参数。结果表明,灰泥矿物基质是由钙质材料形成的,覆盖着具有可变比例的含铁材料(红色,o色和黄色)和富含碳含量(黑色)的薄膜。化合物与蓝色和绿色相关。所有这些材料都显示出高水平的劣化,这是由于由灰泥引起的力差以及在溶解结晶周期中由于灰泥与环境之间的湿度差异(由于其特定的暴露条件)而导致的环境可溶性盐的沉积。

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