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Application of thermal analysis in preservation and restoration of historic masonry materials: Part B. Degradation of materials (Conference Paper)

机译:热分析在历史性砖石材料的保存和恢复中的应用:B部分。材料的降解(会议论文)

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In part A, thermal analysis techniques were discussed to characterize masonry building materials from significant historic properties in the Charleston, South Carolina, area. In part B, thermal analysis confirms various modes of long-term degradation of the materials through environmental exposure. This research provides evidence of diagenesis within materials usually considered as chemically inert. Masonry mortars used in the nineteenth century include those composed of lime and sand in the early part of the period, with the use of natural (manufactured) cement in conjunction with the mid-century fortification of the harbor. Mortars with both types of binders have been found subject to chemical alteration by long-term reactions with intruding soluble salts to form phases rich in sulfur (primarily from ground salt intrusion) or rich in chloride (primarily from sea water intrusion). The general direction of reactions may be toward formation of smectite minerals found in salt water estuaries. Further, evidence of alkali-silica reaction was found in a mortar exposed to sea water. Differences were found in reactions between lime mortars and those containing natural cements in regard to reaction phenomena. Mineral phases as a result of chemical alteration were also found in "underfired" clay bricks. Thermal analysis techniques confirm the identities of new phases within the historic masonry materials. The results suggest new phases formed within the masonry elements have the potential to cause deterioration through salt crystallization phenomena.
机译:在A部分中,讨论了热分析技术,以从南卡罗来纳州查尔斯顿地区的重要历史属性来表征砌筑建筑材料。在B部分中,热分析证实了材料通过暴露于环境而长期降解的各种模式。这项研究提供了通常被认为是化学惰性的材料中成岩作用的证据。十九世纪使用的砌筑砂浆包括在该时期初期由石灰和沙子组成的砂浆,结合使用天然(人造)水泥和本世纪中叶的港口设防。已经发现具有两种粘合剂的砂浆会通过与侵入性可溶性盐长期反应而发生化学变化,形成富含硫的相(主要来自地盐的侵入)或富含氯化物(主要来自海水的侵入)的相。反应的总体方向可能是在盐水河口中发现的蒙脱石矿物的形成。此外,在暴露于海水的砂浆中发现了碱-二氧化硅反应的证据。在石灰砂浆和含有天然水泥的砂浆之间的反应现象方面发现差异。由于化学改变而导致的矿物相也出现在“未烧制”粘土砖中。热分析技术证实了历史性砖石材料中新相的身份。结果表明,在砌体元素中形成的新相有可能通过盐结晶现象而导致变质。

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