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The benefit of a tough skin: bullet holes, weathering, and the preservation of heritage

机译:坚韧的皮肤的好处:弹孔,风化和保护遗产

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摘要

Projectile damage to building stone is a widespread phenomenon. Sites damaged 100 years ago during First World War still see daily use, while in a more contemporary setting numerous reports show the damage to buildings in Babylon, Mosul and Palmyra. While research has been carried out on the long-term effects of conflict such as fire damage, little is known about the protracted damage sustained through the impact of bullets, shrapnel and other metal projectiles outside of the field of engineering focussed on ceramics and metals. To investigate alterations to mineral structure caused by projectile damage, impacts were created in medium grained, well compacted, meso-porous sandstone samples using .22 calibre lead bullets shot at a distance of 20m. Half these samples were treated with a surface consolidant (Wacker OH 100), to mimic natural cementation of the rock surface. These samples were then tested for changes to surface hardness and moisture movement during temperature cycles of 15 to 65°C. Petrographic thin section analysis was carried out to investigate the microscale deformation associated with high speed impact. The results surprisingly show that stress build-up behind pre-existing cementation of the surface, as found in heritage sites that have been exposed to moisture and temperature fluctuations for longer periods of time, can be alleviated with a bullet impact. However, fracture networks and alteration of the mineral matrices still form a weak point within the structure, even at a relatively low impact calibre. This initial study illustrates the need for geomorphologists, geologists, engineers and heritage specialists to work collectively to gain further insights into the long-term impact of higher calibre armed warfare on heritage deterioration.
机译:弹丸对建筑石材的破坏是普遍现象。 100年前第一次世界大战期间受损的场所仍可日常使用,而在更现代的环境中,许多报道表明巴比伦,摩苏尔和巴尔米拉的建筑物遭到了破坏。尽管已经对诸如火害之类的冲突的长期影响进行了研究,但对于以子弹,弹片和其他金属弹丸的冲击所造成的长期破坏却鲜为人知。为了研究由弹丸损坏引起的矿物结构变化,使用了在20m处发射的.22口径铅弹在中等粒度,压实的中孔砂岩样品中产生了冲击。这些样品的一半用表面固结剂(Wacker OH 100)处理,以模拟岩石表面的自然胶结作用。然后测试这些样品在15到65°C的温度循环中表面硬度和水分运动的变化。进行了岩相薄片分析以研究与高速冲击有关的微观形变。结果出乎意料地表明,在原有的表面胶结作用背后的应力积聚可以通过子弹冲击得到缓解,如在长期暴露于水分和温度波动的遗产中所发现的那样。然而,即使在相对较低的冲击口径下,断裂网络和矿物基质的变化仍会在结构内形成薄弱点。这项初步研究表明,地貌学家,地质学家,工程师和遗产专家需要共同努力,以进一步了解高水平武装战争对遗产恶化的长期影响。

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