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Deterioration of different stones used in historical buildings within Nigde province, Cappadocia

机译:卡帕多细亚尼格德省历史建筑中使用的不同石材的变质

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The Cappadocia region hosts various historical buildings constructed by several civilisations from long in the past until more recently. Some of these are big and significant buildings and their artistic, cultural and aesthetical features are quite attention-grabbing. The stones used in most of these buildings have deteriorated due to various effects. The correct identification of the deterioration mechanisms is of fundamental importance to design retrofitting and restoration procedures. In this study we aimed to determine the engineering properties and deterioration of the stones widely used in the different historical buildings in the Nigde region that forms the southern boundary of Cappadocia. 17 block samples (2 marble, 2 travertine, 6 tuff, 5 ignimbrite and 1 andesite) were taken - in accordance with the obtained permits - from stones that had fallen from the buildings and could not be used again as part of any restoration. With the purpose ofidentifying the deterioration of the building stones due to their geological structure and external effects, chemical and petrographic analyses were conducted along with detailed field observations. To determine the geomechanical properties (dry unit weight, water absorption, effective porosity, P-wave velocity, uniaxial compressive strength, slake durability index, capillary water absorption, Bohme abrasion value and Schmidt hammer rebound value) of the stones comprehensive laboratory research was carried out. The main cause of the deterioration observed in ignimbrites (UK3) and tuffs (AK3) with low strength and high porosity was humidity, especially at the capillary level. Significant deterioration observed on some stone samples was also due to the use of stones that exhibited poorer properties than the rest, although they came from the same quarry. Adding the negative effects of ground and surface water on top of these, severe damage on the stones in the forrnof flaking, discolouration and loss of strength were observed.
机译:卡帕多细亚(Cappadocia)地区拥有各种历史建筑,这些建筑是由多个文明建造而成的,其历史可追溯至过去。其中一些是大型的重要建筑物,其艺术,文化和美学特征引人注目。由于各种影响,大多数这些建筑物中使用的石材已经变质。正确识别劣化机制对于设计翻新和修复程序至关重要。在这项研究中,我们旨在确定在卡帕多西亚南部边界的尼德地区不同历史建筑中广泛使用的石材的工程特性和劣化。根据获得的许可,从掉落在建筑物上且无法再次用作任何修复物的石头中采集了17个块状样品(2个大理石,2个钙华,6个凝灰岩,5个火成岩和1个安山岩)。为了识别建筑石材由于其地质结构和外部影响而导致的变质,进行了化学和岩石学分析以及详细的现场观察。为了确定石材的地质力学性能(干重,吸水率,有效孔隙率,P波速度,单轴抗压强度,熟料耐久性指标,毛细吸水率,布氏磨耗值和施密特锤回弹值),进行了全面的实验室研究出来。在强度低,孔隙率高的火成岩(UK3)和凝灰岩(AK3)中观察到变质的主要原因是湿度,尤其是在毛细管水平。在某些石材样品上观察到的显着劣化也是由于使用了比其他石材性能差的石材,尽管它们来自同一采石场。在这些之上加上地下水和地表水的负面影响,观察到了forrnof剥落中石头的严重损坏,变色和强度下降。

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