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Changes in constituent equilibrium leaching and pore water characteristics of a Portland cement mortar as a result of carbonation

机译:碳化导致波特兰水泥砂浆的组成平衡浸出和孔隙水特征的变化

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摘要

Two equilibrium-based characterization protocols were applied to ground samples of a cement-based material containing metal oxide powders in both noncarbonated and carbonated states. The effects of carbonation were shown through comparison of (ⅰ) material buffering capacity, (ⅱ) constituent equilibrium as a function of leachate pH, and (ⅲ) constituent solubility and release as a function of liquid-to-solid (LS) ratio. As expected, the material alkalinity was significantly neutralized during carbonation. In addition, carbonation of the cement material led to the formation of calcium carbonate and a corresponding increase in arsenic release across the entire pH range. The solubility as a function of pH for lead and copper was lower in the alkaline pH range (pH > 9) for carbonated samples compared with the parent material. When solubility and release as a function of LS ratio was compared, carbonation was observed to decrease calcium solubility, sodium and potassium release, and ionic strength. In response to carbonate solid formation, chloride and sulfate release as a function of LS ratio was observed to increase. Trends in constituent concentration as a function of LS ratio were extrapolated to estimate pore water composition at a 0.06 mL/g LS ratio. Significant differences were observed upon comparison of estimated pore water composition to leachate concentrations extracted at LS ratio of 5 mL/g. These differences show that practical laboratory extractions cannot be assumed directly representative of pore water concentrations.
机译:将两种基于平衡的表征方案应用于包含非碳化和碳酸态的金属氧化物粉末的水泥基材料的地面样品。通过比较(○)材料的缓冲能力,(○)组成平衡与渗滤液pH的函数以及(○)组成的溶解度和释放与液/固(LS)比的函数,可以看出碳酸化的影响。不出所料,碳化过程中材料的碱度被中和。另外,水泥材料的碳酸化导致碳酸钙的形成,并且在整个pH范围内砷释放量相应增加。与母体材料相比,在碳酸化样品的碱性pH范围内(pH> 9),铅和铜的溶解度随pH的变化而降低。当比较溶解度和释放量作为LS比的函数时,观察到碳酸化会降低钙的溶解度,钠和钾的释放量以及离子强度。响应于碳酸盐固体的形成,观察到作为LS比率的函数的氯化物和硫酸盐释放增加。推断出作为LS比率的函数的成分浓度趋势,以估计0.06mL / g LS比率的孔隙水组成。通过比较估计的孔隙水成分与以5 mL / g的LS比提取的渗滤液浓度,可以观察到显着差异。这些差异表明,不能假定实际的实验室提取物可以直接代表孔隙水的浓度。

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