The influence of moisture on the colour characteristics of natural stone

V. Korobiichuk, R. Sobolevskyi, O. Sydorov, V. Shamrai, V. Shlapak
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Abstract

The objects of the research are the facing elements of buildings and architectural monuments. The subject of the study is the process of changing the colour of the decorative stone from moisture. To solve the problems of analyzing the appearance of the surface, it is necessary to form a digital image of the surface of the facing stone and perform its processing by means of modern computer technology. Natural stone darkens in places where there is moisture in the pores. The paper investigated the component L, which is responsible for the lightness in the Lab colour system , the study was conducted on samples with a length of 600 mm and a width of 300 mm with a thickness of 24, 25, 31, 32 mm. To determine the humidity of the samples Hydro Condtrol device was used; it is based on the dielcometric method of measuring the humidity. After 100 hours of exposure to moisture at Pokostivsky granodiorite, the reduction of component L, which is responsible for the lightness in the Lab colour system, actually stops. There is a directly proportional dependence of the height of moisture rise in the samples of natural stone on their thickness, which is associated with an increase in the number of pores that participate in the liquid transfer process. With increasing duration of exposure to moisture at Pokostivsky granodiorite the moisture of the sample surface increases, which can be predicted in the general case and for different values of the thickness of the samples using analytical expressions. Comparison of intensity of value change of components L, which is responsible for the lightness in the Lab colour system and surface moisture of the samples, allows to draw a conclusion about the absence of an explicit connection between the above-mentioned processes.
水分对天然石材颜色特性的影响
研究的对象是建筑物和建筑纪念碑的立面元素。研究的主题是改变装饰石的颜色从水分的过程。为了解决分析表面外观的问题,需要借助现代计算机技术对饰面石表面形成数字图像并进行处理。天然石材在毛孔中有水分的地方会变暗。本文研究了实验室色彩系统中负责亮度的成分L,研究对象是长度为600 mm,宽度为300 mm,厚度为24、25、31、32 mm的样品。采用液压控制装置测定样品的湿度;它是基于电介质测量湿度的方法。在Pokostivsky花岗闪长岩中暴露于湿气100小时后,负责实验室色彩系统亮度的成分L的减少实际上停止了。天然石材样品中水分上升的高度与其厚度成正比关系,这与参与液体传递过程的孔隙数量的增加有关。随着Pokostivsky花岗闪长岩受潮时间的增加,样品表面的水分增加,这可以在一般情况下和样品厚度的不同值下使用解析表达式进行预测。在实验室颜色系统中负责亮度和样品表面湿度的组分L的值变化强度的比较,可以得出上述过程之间没有明确联系的结论。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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