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SECONDARY ETTRINGITE FORMATION AND DISTRESS IN A GROUT

机译:灌浆中的二次钙矾石的形成和应力

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Delayed ettringite formation (DEF) generally refers to an internal sulfate attack in portland cement concrete or similar materials in which the early normal formation of ettringite is postponed or interrupted, due to exposure to elevated temperature (greater than 70°C or 158℉) achieved either intentionally via heat-curing in precast products or inadvertently due to hydration, such as in mass concrete. If so affected, ettringite forms later after the concrete hardens and exposed to moisture. This delayed formation of ettringite generates substantial distress and results in expansion and subsequent cracking in concrete. Mitigation of DEF-related distress has to be considered in placing mass concrete and in production of precast concrete. Numerous publications are available on the topic. Two hypotheses have been proposed to explain the expansion caused by DEF: the uniform paste expansion theory and the crack expansion hypothesis. In the uniform paste expansion theory, the driving force is considered to be from the formation of submicroscopic ettringite within the bulk paste that causes expansion of the cement paste as a whole. The expansion creates peripheral gaps around aggregate particles, and the thickness of the gaps are proportional to the aggregate size. In the second hypothesis, the main driving force is considered to be local expansion resulted from the formation of ettringite in cracks in paste or rim cracks around aggregates where pressure comes either from an osmotic effect or from crystal growth. It is now generally believed that the paste expansion results from the growth of ettringite crystals in very small pores (~ 100 nm) of the cement paste (i.e. the uniform paste expansion theory) or both mechanisms may play a role (Taylor, 1997). Typical petrographic evidence of DEF includes: 1) frequent, partial or full peripheral gaps around aggregate lined with ettringite; 2) abundant cracks or microcracks within the paste that are lined with ettringite; 3) replacement of significant amounts of silicate paste by ettringite; and 4) presence of two-tone C-S-H inner products and variation in sulfate contents between the products. Some of these features, particularly the chemical composition, are not necessarily discernible using optical microscopy; thus, analysis using scanning electron microscopy equipped with energy dispersive X-ray spectrometry (SEM-EDS) is often needed. Exposure of concrete at the early age to elevated temperature has widely been accepted as the first prerequisite for DEF-related distress. Alleged DEF-related distress without heat exposure in some case studies had been reported, but was later found to be "unsubstantiated, inconclusive, or flawed" (Taylor, 1997). In our experience, the prerequisite of curing at elevated temperatures applies to concrete mixture with ordinary sulfate contents. For cementitious mixtures containing excessive sulfate, the heat curing for delayed formation of deleterious ettringite is not necessarily a required condition. This paper reports a case study that involves secondary ettringite-caused distress in an anchoring grout that was not subjected to elevated temperatures. A commercial, proprietary, pre-packaged cementitious product was used to anchor hundreds of aluminum handrails and posts at a Midwest train station. The grout is mainly composed of portland cement, calcium sulfoaluminate cement, and siliceous sand. The grout and the anchoring system exhibited apparent distress that caused displacement of the posts and cracking of surrounding concrete within five years from original installation. The product is intended for both exterior and interior use, and is expected to expand during setting rather than after setting, as the manufacturer claims. Our investigation, including field inspection, petrographic studies, X-ray diffraction analysis, and chemical composition analysis revealed that significant amounts of ettringite formed after the grout had set. Affected grout has altered substantially in physical, chemical and mechanical properties and eventually lost serviceability. Characteristics of the distress are similar to the heat-induced DEF, although the mechanism of ettringite formation is most likely very different. High mix water content in the grout, higher than manufacturer's recommendations, was suspected to have compromised the durability of the grout and contributed to the formation of excessive ettringite. Additional petrographic studies and mortar bar expansion tests were conducted on laboratory samples prepared using the commercial product to examine the hypothesis. The grout cylinders prepared with high water content (1.2 times of manufacturer's recommended) cracked in less than 40 days when saturated and exposed to the Chicago winter weather whereas the cylinders with the manufacturer's recommended water content and lower (0.8 time of recommended) stayed intact. Mortar bars did not expand but shrank up to 0.03 percent within the 3 months monitored when stored at an environment controlled room at 75℉ temperature and 75% relative humidity.
机译:延迟钙矾石形成(DEF)通常是指在硅酸盐水泥混凝土或类似材料中发生的内部硫酸盐侵蚀,其中由于达到较高的温度(高于70°C或158℉)而使钙矾石的早期正常形成被延迟或中断。要么有意通过预制产品中的热固化,要么由于水合而无意中(例如在大体积混凝土中)通过热固化。如果受到这种影响,则在混凝土硬化并暴露于湿气之后会形成钙矾石。钙矾石的这种延迟形成产生很大的困扰,并导致混凝土膨胀和随后的开裂。在放置大体积混凝土和生产预制混凝土时,必须考虑减轻与DEF有关的困扰。关于该主题的出版物很多。提出了两个假设来解释由DEF引起的膨胀:均匀膏体膨胀理论和裂纹膨胀假设。在均匀浆体膨胀理论中,驱动力被认为是由于块状浆体中亚微米级钙矾石的形成,从而导致水泥浆体整体膨胀。膨胀在聚集体颗粒周围产生周边间隙,并且间隙的厚度与聚集体尺寸成比例。在第二个假设中,主要驱动力被认为是局部膨胀,是由于钙钛矿在膏体裂纹或骨料周围的边缘裂纹中形成钙矾石而形成的,其中骨料的压力来自渗透作用或晶体生长。现在一般认为,糊料的膨胀是由钙矾石晶体在水泥浆的很小的孔(〜100nm)中的生长引起的(即均匀的糊料膨胀理论),或者这两种机理都可能起作用(Taylor,1997)。 DEF的典型岩相学证据包括:1)衬有钙矾石的骨料周围经常,部分或全部出现周边缝隙; 2)衬有钙矾石的浆料中有大量裂纹或微裂纹; 3)用钙矾石代替大量硅酸盐浆; 4)存在两个色调的C-S-H内在产物并且产物之间的硫酸盐含量变化。这些特征中的某些特征,特别是化学组成,不一定可以通过光学显微镜来辨别。因此,经常需要使用配备有能量色散X射线光谱仪(SEM-EDS)的扫描电子显微镜进行分析。在早期,将混凝土暴露于高温已被广泛接受为与DEF相关的困扰的首要前提。据报道,在某些案例研究中,没有热暴露的与DEF有关的困扰,但后来发现是“未经证实的,不确定的或有缺陷的”(Taylor,1997)。根据我们的经验,在高温下固化的前提条件适用于具有普通硫酸盐含量的混凝土混合物。对于含有过量硫酸盐的水泥混合物,不一定要进行热固化以延迟形成有害的钙矾石。本文报道了一个案例研究,该案例涉及在不经受高温的锚固灌浆中二次钙矾石引起的困扰。一种商业的,专有的,预包装的水泥产品被用来在中西部火车站固定数百根铝制扶手和立柱。水泥浆主要由硅酸盐水泥,硫铝酸钙水泥和硅质砂组成。水泥浆和锚固系统表现出明显的困扰,在最初安装后的五年内,导致了桩的位移和周围混凝土的开裂。该产品既可用于室内也可用于室内,并且预期会在凝固过程中膨胀,而不是在凝固之后膨胀,正如制造商所声称的那样。我们的调查,包括现场检查,岩石学研究,X射线衍射分析和化学成分分析,发现在灌浆后形成了大量的钙矾石。受影响的水泥浆的物理,化学和机械性能发生了很大变化,最终丧失了使用性。尽管钙矾石形成的机理很可能非常不同,但遇险的特征与热诱导的DEF相似。灌浆中的混合水含量高,高于制造商的建议被怀疑损害了水泥浆的耐久性,并导致了过多的钙矾石的形成。对使用商业产品制备的实验室样品进行了其他岩相学研究和砂浆棒膨胀试验,以检验该假设。含水量高(制造商推荐值的1.2倍)的灌浆气瓶在饱和并暴露于芝加哥冬季天气后不到40天会破裂,而制造商建议水含量低(推荐值0.8倍)的气瓶则完好无损。当存放在75℉温度和75%相对湿度的环境控制室中时,砂浆条没有膨胀,但在监测的3个月内收缩了0.03%。

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