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Active Iron-Rich Belite Sulfoaluminate Cements: Clinkering and Hydration

机译:富铁活性贝利特硫铝酸盐水泥:熟料和水化

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摘要

Ordinary Portland cement (OPC) is an environmentally contentious material, as for every ton of OPC produced, on average, 0.97 tons of CO_2 are released. Conversely, belite sulfoaluminate (BSA) cements are promising eco-friendry building materials, as their production may deplete CO_2 emissions up to 35% (compared to OPC). However, the hydration rate of belite is slow. Here, we report the clinkering of iron-rich BSA materials, their activation with B_2O_3, and establishing a methodology to measure their improved reactivities. Nonactivated BSA clinker contained only β belite phase, 52 wt %. Meanwhile, BSA clinkers activated with 1 and 2 wt % of B_2O_3 contained 28 wt % of β and 25 wt % of α'_H; and 54 wt % of α'_H phase, respectively. Therefore, activation of BSA has been proved as α'_H belite is stabilized. The hydration of the cements has been studied by laboratory and synchrotron X-ray powder diffraction (using Rietveld method and chemical constraints), calorimetry, and environmental scanning electron microscopy. Cement pastes have different hydration rates. For nonactivated BSA cement 20 and 48% of the belite reacted after one and three months, respectively. Conversely, 37-49% after one month and 52-62% after three months of overall belite reactivities have been measured for BSA cements activated with B_2O_3.
机译:普通波特兰水泥(OPC)是一种对环境有害的材料,每生产一吨OPC,平均会释放0.97吨CO_2。相反,贝利特硫铝酸盐(BSA)水泥是有希望的生态友好型建筑材料,因为其生产可能消耗高达35%的CO_2排放量(与OPC相比)。但是,珍珠岩的水合速率很慢。在这里,我们报告了富铁BSA材料的熟料,B_2O_3对其的活化作用,并建立了测量其提高的反应活性的方法。未活化的BSA熟料仅包含52 wt%的β珍珠岩相。同时,被1和2重量%的B_2O_3活化的BSA熟料包含28重量%的β和25重量%的α'_H; α′_H相的含量分别为54wt%。因此,已经证明,由于稳定​​了α'_H珍珠岩,BSA的活化。水泥的水合作用已通过实验室和同步加速器X射线粉末衍射(使用Rietveld方法和化学约束),量热法和环境扫描电子显微镜进行了研究。水泥浆的水合速率不同。对于未活化的BSA水泥,一个月和三个月后分别有20%和48%的珍珠岩反应。相反地​​,对于用B_2O_3活化的BSA水泥,在一个月后的总珍珠岩反应性中测得37-49%,在三个月后的52-62%。

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  • 来源
    《Environmental Science & Technology》 |2010年第17期|p.6855-6862|共8页
  • 作者单位

    Departamento de Quimica Inorgdnica, Crystalografta y Mineralogia, Universidad de Malaga. 29071 MAlaga, Spain;

    rnDepartamento de Quimica Inorgdnica, Crystalografta y Mineralogia, Universidad de Malaga. 29071 MAlaga, Spain;

    rnDepartamento de Quimica Inorgdnica, Crystalografta y Mineralogia, Universidad de Malaga. 29071 MAlaga, Spain;

    rnDepartamento de Quimica Inorgdnica, Crystalografta y Mineralogia, Universidad de Malaga. 29071 MAlaga, Spain;

    rnMartin-Luther-Universitat Halle-Wittenberg, Institut fuer Geologische Wissenschaften und Geiseltalmuseum, Mineralogy/Geochemistry, 06120 Halle, Germany;

    rnMartin-Luther-Universitat Halle-Wittenberg, Institut fuer Geologische Wissenschaften und Geiseltalmuseum, Mineralogy/Geochemistry, 06120 Halle, Germany;

    rnDepartamento de Quimica Inorgdnica, Crystalografta y Mineralogia, Universidad de Malaga. 29071 MAlaga, Spain;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
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  • 正文语种 eng
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  • 入库时间 2022-08-17 14:04:00

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