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Long term corrosion behaviour of copper in soil: A study of archaeological analogues

机译:铜在土壤中的长期腐蚀行为:考古类似物的研究

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The long term corrosion behaviour of copper in soil environment has been addressed by studying two archaeological copper samples. The microstructures of the material of construction of a Chalcolithic (2350BC-1800BC) copper chisel from Balathal and an OCP period (2650BC-800BC) Cu anthropomorphic object have been first characterized by microscopy and the features understood by stereological methods. The equiaxed grain size, coring effects in the grains and the relatively soft matrix of the OCP copper object indicated that it was manufactured by casting. The deformed grains near the surfaces and variation in the microhardness of the sample at different points suggests that the Chalcolithic copper chisel was processed by cold deformation after casting of the square cross section chisel. The surface patina on the two archaelogical copper objects has been characterized by X-ray diffraction. In the case of OCP copper, the green surface patina was analyzed as a mixture composed mainly of cuprite, and minor amounts of malachite and brochantite. In the case of Chalcolithic copper, the patina was composed of sulfates and oxysulfates in the outer layers while the inner layers were rich in copper oxides. The electrochemical behaviour of both the archaeololgical coppers has been characterized and compared with that of a modern Cu sample by potentio-dynamic polarization studies. The corrosion rate, determined by Ta-fel extrapolation technique in 3.5% NaCl solution, of Chalcolithic Cu was only marginally higher than that of modern and OCP Cu. The higher rates of corrosion in case of archaeological coppers have been attributed to the presence of second phase sulfide inclusions.
机译:通过研究两个考古铜样品,可以解决铜在土壤环境中的长期腐蚀行为。 Balathal的Chalcolithic(2350BC-1800BC)铜凿和OCP时期(2650BC-800BC)Cu拟人化物体的构造材料的微观结构首先通过显微镜进行了表征,并通过立体方法了解了特征。等轴晶粒尺寸,OCP铜物体的晶粒中的去核效应和相对较软的基体表明它是通过铸造制造的。靠近表面的变形晶粒和样品在不同点的显微硬度变化表明,在铸造方形截面凿子后,通过冷变形处理了黄铜矿铜凿。通过X射线衍射表征了两个考古铜物体上的表面铜绿。在OCP铜的情况下,分析的绿色表面铜绿是主要由铜矿以及少量孔雀石和青铜矿组成的混合物。在黄铜矿的情况下,铜绿由外层的硫酸盐和硫酸盐组成,而内层的铜氧化物丰富。通过电位动态极化研究,已表征了两种考古铜的电化学行为,并将其与现代Cu样品的电化学行为进行了比较。通过Ta-fel外推技术在3.5%NaCl溶液中测定的黄铜矿型铜的腐蚀速率仅略高于现代铜和OCP铜。在考古铜的情况下,较高的腐蚀速率归因于第二相硫化物夹杂物的存在。

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