Chen Xiaoxiao, Yang Bin, Mao Zhongyang, Deng Min
College of Materials Science and Engineering, Nanjing Tech University, Nanjing 210009, China.
Materials (Basel). 2019 Apr 15;12(8):1228. doi: 10.3390/ma12081228.
In this study, concrete microbars and rock prisms made of dolomitic aggregates were cured in a 1-mol/L tetramethylammonium hydroxide (TMAH) solution at 80 °C to avoid the effect of alkali-silica reaction (ASR) on expansion. The expansion of specimens was only caused by the alkali-carbonate reaction (ACR). The reason that self-made cement was used in this work was to ensure that the Mg contained in the brucite originated only from dolomite. Expansion of concrete microbars and rock prisms was measured, the expansion cracks were systematically observed by orthogonal polarizing microscopy, and the products of ACR were analyzed by scanning electron microscopy (SEM) and energy dispersive spectrometry (EDS). The results showed that the dolomite crystals in the dolomitic aggregates reacted with the TMAH solution and resulted in ACR, which formed calcite and brucite and led to cracking of the specimens. The source of the expansion was the dolomite crystals of the dolomite enrichment area. Expansion cracks either extended inside the rock or into the cement phase and eventually disappeared. The alkali-carbonate reaction significantly contributed to the expansion of dolomitic aggregates cured in TMAH solution at a later curing age.
在本研究中,由白云质集料制成的混凝土微棒和岩石棱柱体在80℃的1mol/L氢氧化四甲铵(TMAH)溶液中养护,以避免碱-硅反应(ASR)对膨胀的影响。试件的膨胀仅由碱-碳酸盐反应(ACR)引起。本研究采用自制水泥的原因是确保水镁石中所含的镁仅来源于白云石。测量了混凝土微棒和岩石棱柱体的膨胀,通过正交偏光显微镜系统观察了膨胀裂缝,并通过扫描电子显微镜(SEM)和能谱仪(EDS)分析了ACR产物。结果表明,白云质集料中的白云石晶体与TMAH溶液发生反应,导致ACR,生成方解石和水镁石,从而导致试件开裂。膨胀的来源是白云石富集区的白云石晶体。膨胀裂缝要么在岩石内部延伸,要么延伸到水泥相中,最终消失。在后期养护龄期,碱-碳酸盐反应对在TMAH溶液中养护的白云质集料的膨胀有显著贡献。