激光清洗对哥特兰砂岩元素组成影响的观察

Laser Chemistry Pub Date : 2006-01-10 DOI:10.1155/2006/84781
M. Jasińska, J. Bredal-Jørgensen, G. Śliwiński
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引用次数: 4

摘要

采用SEM/EDX技术研究了激光表面清洗对天然结壳历史砂岩的元素组成变化。将激光照射前后的石样数据与未结皮的参考石样进行了比较。已经观察到,由于烧蚀清洗导致的结壳去除伴随着Al, S, K, Ca和Mg元素的部分含量的减少,在未清洗的结壳覆盖的石头表面记录的初始值的60 - 80%范围内。在地壳覆盖下的岩石层中,观察到以sio2颗粒间的粒间空间为主要砂岩组分,并充填有降解黏合剂的结构。从粘结剂破坏与地壳化学成分的重合出发,推导出环境污染长期相互作用导致的石质表面破坏。激光照射后各元素的空间分布表明,除sio2外,砂岩表层元素含量下降了50%,而初始含量为4%的Fe和其他表面残留物P、Ti、Zn、cl -均低于1%,变化不明显。与文献一致的结论是,用1064 nm激光进行表面清洗不会导致铁从砂岩表面去除。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Observation of the Laser Cleaning Effect on the Gotland Sandstone Elemental Composition
Changes of the elemental composition due to laser surface cleaning of a naturally crusted historical sandstone were investigated by means of the SEM/EDX technique. Data obtained for stone samples prior to and after laser irradiation were compared with those for noncrusted, reference ones. It has been observed that the crust removal resulting from ablative cleaning was accompanied by a decrease of the partial content of elements Al, S, K, Ca, and Mg in the range of 60–80 % of their initial value recorded for the noncleaned, crust-covered stone surface. In the stone layer just under the crust coverage, a structure characterized by intergranular spaces between the SiO 2 grains being the main sandstone component filled with degraded binder was observed. From the coincidence of the binder destruction and chemical composition of the crust, the stone surface destruction due to the long-term interaction of environmental pollution was deduced. The spatial distributions of individual elements obtained by mapping after laser irradiation indicated that besides SiO 2 the content of elemental components in the sandstone surface layer decreased by 50 % , whereas for Fe with the initial content of 4 % and other surface remnants: P, Ti, Zn, and Cl—all below 1 % , insignificant changes were only revealed. It was concluded in agreement with the literature that surface cleaning by means of the 1064 nm laser does not cause removal of iron from the sandstone surface.
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