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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:在用于外部建筑物外墙外,更好地了解导致卡拉拉大理石丢失的机制的贡献

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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Carrara大理石已被用作已经因为外的平面扭曲的失败暴露外,薄,表面面板;的现象被称为碟状凹陷,拔罐,和弯曲。理论已经提出来解释的现象。本文扩大了解释,并基于热滞石已知具有和石头尺寸的关系。大理石由细的马赛克的,基本上相等的轴向方解石晶体没有确定的晶体边界。方解石在3个“A”晶轴的方向上的公知的各向异性热响应,其中,所述晶体膨胀(如所预期的)在“C”结晶轴,但合同的方向(将不被期望的),其被定向垂直于“C”轴。因为沿着晶界的位错,这与晶体的恢复到原来的位置干扰晶体的非常轻微的重新定位的结果。大理石的体积导致略有增加是累计有持续的热循环。当面板的前经历更多次热循环和/或小于面板的背面达到更高的温度,结果是一个微分容积前方与前扩大超过背背增加。基于实验室的实验工作中,当面板它们的厚度的横向尺寸的比例是合适的,出平面外扭曲重新配置面板在永久轻微碟形天线的形式。在大理石原因热滞后的物理效应;凹陷,体积增加,增加的孔隙率,和降低,因为应力的强度沿着晶界,最终大理石的崩解成糖状颗粒。有粗糙的颗粒大小和镶嵌大理石纹理不进行类似的热滞后效应的卡拉拉大理石,因为有较少的晶体进行交互。

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