延迟蚀变体形成的砂浆的长期特性

Benjamin J. Mohr , M. Shariful Islam , L. Bryant
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引用次数: 0

摘要

乙丁睛石的形成是一种膨胀反应,会导致水化胶凝材料开裂。这项研究通过考察晚龄期(15 年以上)乙丁二酸盐形成过程中反应物和生成物的化学和物理结构,以及随后的膨胀和开裂过程,研究了乙丁二酸盐形成的机理。为此,采用了七种不同类型的市售水泥及其独特成分,并将热固化温度提高到 100 ℃。通过长度变化比较仪监测了砂浆棒因延迟形成乙丁质岩而产生的物理膨胀。环境扫描电子显微镜(ESEM)用于鉴定和量化水泥基质微观结构和化学成分的变化。结果表明,高温热固化加速了膨胀的开始,但限制了膨胀的过度幅度。结果还显示,膨胀可能需要数年才能开始,这可能是由于诱发应力所需的临界孔径阈值。如果延迟膨胀,膨胀幅度会大于立即膨胀的情况。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Long-term behavior of mortars experiencing delayed ettringite formation

Ettringite formation is an expansive reaction that causes cracking in the hydrated cementitious materials. This research has investigated the mechanisms of ettringite formation by examining the chemical and physical structure of the reactants and products involved in the process of late age (over 15 years) ettringite formation, and subsequent expansion and cracking. For this, seven different types of commercially available cement with their unique composition, and an elevated heat curing temperature of up to 100 °C were applied. The physical expansion of mortar bars due to delayed ettringite formation was monitored by the length change comparator. Environmental scanning electron microscopy (ESEM) was used to qualify and quantify changes in the microstructure and chemical composition of the cementitious matrix. Results revealed that the high-temperature heat curing accelerated the onset of expansion but limited the over-magnitude of the expansion. Results also revealed that the expansion may take years to initiate, likely due to a critical pore size threshold necessary to induce stresses. If expansion is delayed, the expansion magnitude is greater than those that expanded immediately.

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