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Technological study of “ghiara” mortars from the historical city centre of Catania (Eastern Sicily, Italy) and petro-chemical characterisation of raw materials

机译:来自卡塔尼亚历史悠久的市中心(意大利西西里岛,意大利)的“ ghiara”灰浆的技术研究和原材料的石油化学表征

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This paper presents new petro-chemical data on some typical mortars found in many buildings in the historic city centre of Catania (Eastern Sicily). Extensively used in the architecture of the city from the second half of the nineteenth century until the mid-twentieth century, these mortars are characterised by a particular aggregate locally known as “agghiara” or “ghiara”. This is the product of thermal transformation induced by the heating undergone by palaeo-soils, originally rich in organic matter, covered by lava flows, which change their colour to reddish nuances. The volcanic origin of ghiara is a peculiar feature of the Etnean area. Mixed with lime, it gives to mortars an intense reddish colour, as well as hydraulic properties, which are comparable with those of the historically used pozzolana. This work aimed at complete characterisation of these ghiara mortars, for providing information on several important technological aspects. In order to get information on used raw materials, sampling of some ancient underground quarries, located both in the historic city centre and at the periphery, was also performed. Results led to the complete characterisation of the selected ghiara mortars and yielded information on some technological features and the composition of both newly formed and secondary phases, these latter due to alteration processes. The hydraulic properties of mortars have been related to the occurrence of amorphous phases within the ghiara aggregate, which were identified by means of SEM morphological observations. These phases, formed during the “firing” process of palaeo-soils, react with lime producing hydraulic compounds (C–S–H and C–A–H), which are responsible for the mortars durability.
机译:本文介绍了在历史悠久的卡塔尼亚(西西里岛东部)市中心许多建筑物中发现的一些典型灰浆的新石化数据。从19世纪下半叶到20世纪中期,这些砂浆被广泛地用于城市建筑中,这些砂浆的特点是当地称为“ agghiara”或“ ghiara”的特殊骨料。这是原始土壤富含有机质的古土壤受热引起的热转化产物,这些古土壤被熔岩流覆盖,这些熔岩的颜色变为细微的细微差别。吉亚拉火山的起源是埃特纳地区的独特特征。与石灰混合后,灰浆具有强烈的红色和水硬性,可与历史上使用的火山灰相媲美。这项工作旨在完全表征这些ghiara砂浆,以提供有关几个重要技术方面的信息。为了获得有关使用过的原材料的信息,还对历史悠久的市中心和外围的一些古代地下采石场进行了采样。结果导致对选定的ghiara砂浆的完整表征,并获得了有关某些技术特征以及新形成相和次要相的组成的信息,而后者是由于变更工艺而产生的。砂浆的水硬性与ghiara骨料中非晶相的出现有关,这是通过SEM形态学观察确定的。这些阶段是在古土壤“烧成”过程中形成的,与产生石灰的水硬性化合物(C–S–H和C–A–H)发生反应,这决定了砂浆的耐久性。

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