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首页> 外文期刊>Environmental earth sciences >The Estremoz marbles: an updated summary on the geological, mineralogical and rock physical characteristics
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The Estremoz marbles: an updated summary on the geological, mineralogical and rock physical characteristics

机译:Estremoz大理石:地质,矿物学和岩石物理特征的最新摘要

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摘要

Marbles have been used by human beings for the creation of buildings, monuments and art since antiquity. Impressive architecture and art all over the world are still being constructed from marble today. The Portuguese Estremoz marble is one of the important marble varieties used for these objects. The name Estremoz is used for many of the varieties, exploited and sold from this region. The present study gives an updated summary on the geological, mineralogical and rock physical characteristics with special attention to the potential physical weathering behaviour. Ten representative marble varieties extracted and sold in this region were chosen for analysis with regard to their mineralogical composition, microfabric and their thermal, thermohygric and bowing behaviour. Experimental bowing tests, carried out on selected samples, have been analysed and compared to the results measured at the State Theatre in Darmstadt. The mineralogical composition is similar for all samples, even though the colours range from white, to pinkish and dark grey. Monochromatic colours are seldom. Randomly distributed veins and spots in different colours determine the aesthetic properties. The main component is calcite (87-98%), while two samples show a lower amount of dolomite (3 and 11%). The microfabric of the studied marbles are quite different, with grain sizes ranging between 40 mu m and 2.5 mm. Distribution of grain sizes are equi-and inequigranular to seriate. The grain boundary geometry ranges from polygonal to amoeboid. All samples show a preferred orientation of the grain shape, often most pronounced in the XZ-plane. Measurements of texture showed, that the maximum c-axis densities of the marbles are similar and with 2.09-3.64 mrd moderately to strongly pronounced. In some cases, a weakly to moderate girdle-like shape of the intensity distribution could be observed. The thermal dilatation coefficient a varies between 0.16 and 12.97 x 10(-6) K-1 and shows a strong directional dependence. All samples showed an irreversible length change after repeated heating cycles under dry and wet conditions that ranges between 0.05 and 0.59 mm/m. Marble panels used for the bowing test showed a maximum bowing intensity of 0.5 mm/m. The State Theatre in Darmstadt, Germany, is one example of the exterior application of Estremoz marble. The facade is cladded with panels of 3 cm in thickness. They show weathering phenomena like fractures and concave and convex bowing. Bowing intensities have been measured up to more than 9 mm/m. Weathering phenomena are influenced by the rock physical properties which can be seen in the results of the thermal and thermohygric behaviour as well as for the bowing tests. By comparing these results, the residual permanent length change can be used as a measure of the vulnerability to thermal weathering.
机译:自上古以来,大理石就被人类用于建筑,古迹和艺术品的创作。如今,全世界仍在使用大理石建造令人印象深刻的建筑和艺术。葡萄牙Estremoz大理石是用于这些物品的重要大理石品种之一。 Estremoz这个名字用于该地区许多品种的开发和销售。本研究提供了有关地质,矿物学和岩石物理特性的最新摘要,并特别注意了潜在的物理风化行为。选择了在该地区提取并出售的十种代表性大理石品种,以对其矿物成分,微织物及其热,热湿性和弯曲性能进行分析。已对选定样品进行的实验弯曲试验进行了分析,并与在达姆施塔特国家剧院进行的测量结果进行了比较。即使颜色从白色到粉红色和深灰色,矿物成分在所有样品中都相似。单色很少。不同颜色的随机分布的静脉和斑点决定了美学特性。主要成分是方解石(87-98%),而两个样品显示的白云石含量较低(3%和11%)。所研究的大理石的微观结构差异很大,其晶粒尺寸在40微米至2.5毫米之间。晶粒尺寸的分布是等边和不等边的。晶界的几何形状范围从多边形到变形虫。所有样品均显示出晶粒形状的首选方向,通常在XZ平面上最为明显。质地的测量表明,大理石的最大c轴密度是相似的,并且以2.09-3.64 mrd中等至强烈地突出。在某些情况下,可以观察到强度分布从弱到中等的带状形状。热膨胀系数a在0.16和12.97 x 10(-6)K-1之间变化,并且显示出强烈的方向依赖性。在干燥和潮湿条件下重复加热循环后,所有样品的长度变化均不可逆,变化范围为0.05至0.59 mm / m。用于弯曲试验的大理石板显示最大弯曲强度为0.5mm / m。德国达姆施塔特的国家剧院是Estremoz大理石外部应用的一个例子。外墙覆盖着3厘米厚的面板。它们显示出风化现象,例如断裂以及凹凸弯曲。弯曲强度的测量值高达9 mm / m以上。风化现象受岩石物理性质的影响,岩石的物理性质可以从热,热湿性能以及弯曲试验的结果中看出。通过比较这些结果,可以将剩余的永久长度变化用作对热风化的脆弱性的度量。

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