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Visualization and quantification of weathering effects on capillary water uptake of natural building stones by using neutron imaging

机译:使用中子成像可视化和量化风化对天然建筑石材毛细水吸收的影响

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摘要

Building stones are frequently subjected to very intense degradation due to salt crystallization, often responsible for strong modifications of their pore network. These effects have a great influence on the mechanical properties and durability of the materials, and on the penetration of water. Therefore, the quantification and visualization of water absorption into the pore network of degraded stones could provide useful information to better understand the weathering process. In this study, neutron radiography has been used (1) to monitor and visualize in two dimensions the capillary water uptake in a Sicilian calcarenite widely used as building and replace stone (namely Sabucina stone) and (2) to quantify the water content distribution, as a function of time and weathering degree. Additionally, traditional experiments based on gravimetric methods have been performed, following the standard recommendations. Results demonstrated a change in the physical properties of Sabucina stones with the intensification of the degradation process, with severe effects on the capillary imbibition dynamics. The water penetration depth at the end of the experiment was substantially higher in the fresh than in the weathered stones. The water absorption kinetics was faster in the weathered samples, and the amount of water absorbed increased with the number of weathering cycles. Good agreement between classical and neutron imaging data has also been evidenced. However, neutron radiography has allowed retrieving additional spatial information on the water absorption process, and to better understand how salt weathering affects the petrophysical properties of the studied stone and how it influences then the stone response against water.
机译:建筑石材经常会由于盐的结晶而发生非常强烈的降解,这通常会导致其孔隙网络的强烈改变。这些影响对材料的机械性能和耐用性以及对水的渗透有很大影响。因此,对降解石头孔隙网络中水吸收的量化和可视化可以提供有用的信息,以更好地了解风化过程。在这项研究中,中子射线照相技术已被用于(1)在两个维度上监测和可视化西西里钙钙石中广泛用作建筑和替代石材(即Sabucina石材)的毛细管吸水,以及(2)量化水含量分布,作为时间和风化程度的函数。此外,遵循标准建议,已经执行了基于重量分析法的传统实验。结果表明,随着降解过程的加剧,沙布奇纳结石的物理性质发生了变化,这对毛细管吸收动力学产生了严重影响。在试验结束时,新鲜水的透水深度比风化石头高。在风化的样品中,吸水动力学更快,并且吸水量随风化循环次数的增加而增加。还已经证明经典和中子成像数据之间的良好一致性。但是,中子射线照相术允许检索有关吸水过程的其他空间信息,并可以更好地了解盐的风化如何影响所研究石头的岩石物理特性以及它如何影响石头对水的响应。

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  • 来源
    《Applied Physics》 |2016年第11期|969.1-969.9|共9页
  • 作者单位

    Department of Biological, Geological and Environment Sciences, University of Catania, Corso Italia 57, 95129 Catania, Italy;

    Department of Biological, Geological and Environment Sciences, University of Catania, Corso Italia 57, 95129 Catania, Italy;

    Department of Biological, Geological and Environment Sciences, University of Catania, Corso Italia 57, 95129 Catania, Italy;

    Laboratoire Leon Brillouin (CNRS/CEA), CEA Saclay, 91191 Gif-Sur-Yvette, France;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
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