首页> 外文会议>International RILEM TC 186-ISA workshop on internal sulfate attack and delayed ettringite formation >ROLE OF MICROSTRUCTURAL CHARACTERISATION IN UNDERSTANDING THE MECHANISM OF EXPANSION DUE TO DELAYED ETTRINGITE FORMATION
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ROLE OF MICROSTRUCTURAL CHARACTERISATION IN UNDERSTANDING THE MECHANISM OF EXPANSION DUE TO DELAYED ETTRINGITE FORMATION

机译:微观结构特征在理解延迟Ettringite地层膨胀机制的作用

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摘要

Mortars or concretes that have been exposed to high temperatures, either through the application of external heat or through the endogenous heat of hydration may suffer from expansion during subsequent moist storage at room temperature. This phenomenon is usually referred to as Delayed Ettringite Formation (DEF), because ettringite deposits have been observed in damaged structures. However no direct correlation has been established between the amount of ettringite detected by XRD in expansive heat-cured mortars and the degree of expansion. In the present work, reported in detail elsewhere, various characterisation techniques were used to study the changes occurring heat cured mortars which were either dimensionally stable or which expanded on subsequent storage in water. X-ray microanalyses of the outer hydration products were found to be the key difference between the two cases. These findings are consistent with a mechanism of expansion in which the formation of ettringite from calcium alumino monosulfate in sub-microscopic pores (~50-100 nm) is the origin of expansion.
机译:通过施加外部热或通过内源性水化的砂浆或混凝土,通过应用外部热量或通过内源性热量可能在室温下湿储存期间膨胀。这种现象通常被称为延迟的Ettringite形成(Def),因为已经在受损的结构中观察到Ettringite沉积物。然而,在膨胀性热固化砂浆中XRD检测到的Ettringite的数量之间没有建立直接相关性和膨胀程度。在目前的工作中,在其他地方详细报道,使用各种表征技术来研究热固化砂浆的变化,其尺寸稳定或在随后的水中膨胀。发现外水合产物的X射线微囊性是两种情况之间的关键差异。这些发现与膨胀机制一致,其中从亚微观孔钙铝磺酸钙(〜50-100nm)中形成Ettringite是膨胀的起源。

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