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Contribution to a Better Understanding of the Mechanism Causing Dishing Failures of the Carrara Marble When Used for Outside Building Facades

机译:有助于更好地理解卡拉拉大理石在建筑外立面使用时的洗碗失败机理

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The famed Carrara marble has been used as outside-exposed, thin, facade panels that have failed because of out-of-plane distortions; a phenomenon referred to as dishing, cupping, and bowing. Theories have been advanced to explain that phenomena. This paper expands the explanations, and is based upon the relationships of thermal hysteresis the stone is known to possess and stone dimensions. The marble consists of a mosaic of fine, essentially equi-axial calcite crystals devoid of defined crystal boundaries. Calcite has a known anisotropic thermal response wherein the crystal expands (as would be expected) in the direction of the 'c' crystallographic axis, but contracts (as would not be expected) in the direction of the three 'a' crystallographic axes, which are oriented normal to the 'c' axis. Very slight repositioning of the crystals result because of dislocations along crystal boundaries, which interfere with the return of the crystals to their original locations. The resulting slight increase in volume of the marble is accumulative with continued thermal cycling. When the front of panels undergo more thermal cycles and/or reach higher temperatures than the back of panels, the result is a differential volume increase front to back with the front expanding more than the back. Based upon laboratory experimental work, when the ratio of lateral dimensions of the panels to their thickness is appropriate, out-of-plane distortions reconfigure the panels in the form of a permanent slight dish. The physical effects of the thermal hysteresis on the marble causes; dishing, increased volume, increased porosity, decreased strengths because of stress along crystal boundaries and, ultimately, disintegration of the marble into sugar-like granules. Marbles having coarser grain sizes and mosaic textures do not undergo similar thermal hysteresis effects as the Carrara marble because there are fewer crystals to interact.
机译:著名的卡拉拉大理石已被用作外部暴露的,薄的外墙面板,但由于面外变形而失效。一种现象,称为凹陷,拔罐和弯曲。已经提出了理论来解释这种现象。本文扩展了解释,并基于已知的石材热滞现象与石材尺寸之间的关系。大理石由精细的,基本等轴的方解石晶体镶嵌而成,没有明确的晶界。方解石具有已知的各向异性热响应,其中晶体在“ c”晶轴的方向上膨胀(如预期的那样),但在三个“ a”晶轴的方向上收缩(如预期的那样)垂直于“ c”轴。由于沿晶体边界的位错而导致晶体的非常轻微的重新定位,这会干扰晶体返回其原始位置。随着持续的热循环,大理石的体积略有增加。当面板的前部比面板的后部经历更多的热循环和/或达到更高的温度时,结果是前到后的体积差异增大,并且前部的扩展大于后部。根据实验室的实验工作,当面板的横向尺寸与厚度的比例合适时,面外变形会以永久性的轻微碟形形式重新配置面板。热滞现象对大理石的物理影响;凹陷,体积增加,孔隙率增加,强度降低,这是由于沿晶界的应力所致,并且最终使大理石崩解成糖状颗粒。具有较小晶粒尺寸和镶嵌纹理的大理石不会像卡拉拉大理石那样经历类似的热滞后效应,因为相互作用的晶体较少。

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