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Experimental research on hygroscopic behaviour of porous specimens contaminated with salts

机译:盐污染的多孔样品的吸湿性能的实验研究

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Salt crystallisation is one of the main causes of masonry decay in monuments. The salt content in a wall is a very important parameter that should be known in order to give a reliable diagnosis on the causes of damage; if a restoration work and a surface treatment are necessary, the salt content has to be known. In fact the presence of salts in the wall can not only reduce the efficiency of a treatment but also form a potential risk for the occurrence of a damaging salt crystallisation process. Different methods and instruments are available to detect salt content and type of salt present, but most of them are quite expensive and time consuming. For this reason, other methods, cheaper and quicker, are preferably adopted. In building practice often the hygroscopic moisture content of powder samples is measured in order to have an indication of the salt content. This method is cheap and simple and, in case of material contaminated with a single salt, gives reliable results on the quantity of salts present because of the linear relation between HMC and salt content. However, in case a mix of salts is involved, as usual in reality, the relation between the HMC and the salt content is not clear yet and the HMC measurement can give only an indication and not a quantitative value of the salt content. This paper presents the experimental results of a research carried out on the hygroscopic behaviour of sodium salts introduced in a typical clay-brick either as single salts or as a mix. The obtained results point out a clear linear relation between salt content and hygroscopic moisture content. This proportionality is verified for (brick) specimens contaminated with pure salts as well as with salt mixtures. Salt mixtures appeared to correspond with hygroscopic moisture contents that are higher than the one calculated according to the amount of single salts present in the mixture. As expected beforehand no difference was found between the hygroscopic behaviour of solid brick specimen and brick powder, only a longer time to reach equilibrium in case of brick powder. This paper suggests in the case of the presence of single salts to use the HMC measurement instead of more complicate and expensive analyses (as for example in laboratory experiments). In building practice, the measurement of the HMC can help in selecting the most interesting spots on which to focus the research avoiding extensive campaigns of sampling and analyses. Besides, HMC measurements performed at different RH, can give suggestions about the type of salt present.
机译:盐的结晶是古迹中砖石腐烂的主要原因之一。墙壁中的盐含量是一个非常重要的参数,应该对其进行诊断,以便对损坏的原因进行可靠的诊断。如果需要进行修复工作和表面处理,则必须知道盐含量。实际上,壁中盐的存在不仅会降低处理效率,而且还可能导致发生破坏性的盐结晶过程。可以使用不同的方法和仪器来检测盐含量和存在的盐的类型,但是大多数方法都非常昂贵且耗时。因此,优选采用更便宜,更快的其他方法。在建筑实践中,通常要测量粉末样品的吸湿性水分含量,以表明盐含量。该方法便宜且简单,并且在材料被单一盐污染的情况下,由于HMC和盐含量之间存在线性关系,因此可以对存在的盐量给出可靠的结果。然而,如果涉及到盐的混合物,则实际上仍然像往常一样,HMC与盐含量之间的关系尚不清楚,并且HMC测量值只能给出指示,而不能给出盐含量的定量值。本文介绍了一项研究的实验结果,该研究是对作为典型盐砖或单盐或混合形式引入的典型粘土砖中钠盐的吸湿性进行的。所得结果指出了盐含量和吸湿性水分之间的明确线性关系。对于被纯盐和盐混合物污染的(砖)样品,已验证了此比例。盐混合物似乎与吸湿性水分含量相对应,该含量高于根据混合物中单一盐的含量计算得出的含量。如预料的那样,在实心砖样品和砖粉的吸湿性能之间没有发现差异,对于砖粉,只有更长的时间才能达到平衡。本文建议在存在单一盐的情况下,使用HMC测量代替更复杂和昂贵的分析(例如在实验室实验中)。在建筑实践中,HMC的测量可以帮助选择最有趣的点,以便将重点放在研究上,而无需进行大量的采样和分析活动。此外,在不同的相对湿度下进行的HMC测量可以提供有关盐类型的建议。

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