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Advances in Understanding Damage by Salt Crystallization

机译:理解盐结晶损害的进展

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Tnhe single most important cause of the deterioration of mon-numents in the Mediterranean basin, and elsewhere around thenworld, is the crystallization of salt within the pores of the stone.nConsiderable advances have been made in recent years in eluci-ndating the fundamental mechanisms responsible for salt dam-nage. As a result, new methods of treatment are being proposednthat offer the possibility of attacking the cause of the problem,nrather than simply treating the symptoms. In this Account, wenreview the thermodynamics and kinetics of crystallization, thennexamine how a range of technological innovations have beennapplied experimentally to further the current understanding of in-npore crystallization. We close with a discussion of how computernmodeling now provides particularly valuable insight, includingnquantitative estimates of both the interaction forces between thenmineral and the crystal and the stresses induced in the material.nAnalyzing the kinetics and thermodynamics of crystal growthnwithin the pores of a stone requires sensitive tools used in com-nbination. For example, calorimetry quantifies the amount of saltnthat precipitates in the pores of a stone during cooling, andndilatometric measurements on a companion sample reveal thenstress exerted by the salt. Synchrotron X-rays can penetratenthe stone and identify the metastable phases that often appearnin the first stages of crystallization. Atomic force microscopy andnenvironmental scanning electron microscopy permit study of the nanometric liquid film that typically lies between salt andnstone; this film controls the magnitude of the pressure exerted and the kinetics of relaxation of the stress. These experi-nmental advances provide validation for increasingly advanced simulations, using continuum models of reactive transport onna macroscopic scale and molecular dynamics on the atomic scale.
机译:在地中海盆地以及整个世界其他地方,单石退化的最重要原因是盐在石头孔隙中的结晶。近年来,在阐明造成这种现象的基本机理方面取得了相当大的进展。盐损坏。结果,提出了新的治疗方法,其提供了解决问题原因的可能性,而不是简单地治疗症状。在此报告中,温雷回顾了结晶的热力学和动力学,然后研究了如何通过实验应用一系列技术创新以进一步了解当前的纳米孔结晶。我们以计算机建模现在如何提供特别有价值的见解作为结尾,其中包括对矿物和晶体之间相互作用力以及材料中产生的应力的定量估计.n分析石头孔隙中晶体生长的动力学和热力学需要灵敏的工具结合使用。例如,量热法可量化冷却过程中沉淀在石头孔隙中的盐分的数量,而对比例样品的二次热膨胀测量则表明盐分所施加的应力。同步加速器X射线可以穿透石头并识别出在结晶的第一阶段中经常出现的亚稳相。原子力显微镜和环境扫描电子显微镜可以研究通常位于盐和nstone之间的纳米级液膜。该膜控制施加压力的大小和应力松弛的动力学。这些实验性进展使用宏观尺度上的反应性传输和原子尺度上的分子动力学的连续模型,为日益高级的仿真提供了验证。

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  • 来源
    《Accounts of Chemical Research》 |2010年第6期|p.897-905|共9页
  • 作者单位

    †Department of Civil and Environmental Engineering, Princeton University,Princeton, New Jersey, and ‡Empa, Swiss Federal Laboratories of MaterialsScience and Technology, Duebendorf 8600, Switzerland;

  • 收录信息 美国《科学引文索引》(SCI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
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  • 正文语种 eng
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  • 入库时间 2022-08-17 13:24:21

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