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Mechanical activation of volcanic ash for geopolymer synthesis: effect on reaction kinetics, gel characteristics, physical and mechanical properties

机译:地缘合成火山灰机械活化:对反应动力学,凝胶特性,物理和机械性能的影响

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This paper looks at the possibility of using low reactive volcanic ash for making geopolymer cement. The research is directed towards (a) alteration of the reactivity of volcanic ash by mechanical activation, and (b) use of mechanically activated volcanic ash for the synthesis of a geopolymer. The effect of mechanical activation was quite visible on particle size distribution and the degree of crystallinity. The disappearance of some anorthite peaks and appearance of quartz peaks in volcanic ashes milled for 120 min demonstrate the change in mineralogy. The appearance of an intense carbonate band with milling time could be related to sorption of atmospheric CO2 on the grains surface during mechanical activation. The manifestation of mechanical activation of volcanic ash was prominent on (a) the reaction kinetics, (b) microstructural development, and (c) physico-mechanical properties of the geopolymer product. The rate constant and extent of geopolymerization increased with milling time but decreased with curing temperature. This decrease is in non-conformity with other alumina-silicate materials used for geopolymerization such as metakaolin and fly ash. FEG-SEM and EDAX results revealed that the geopolymer gel obtained is mixture of poly(ferro-sialate-siloxo) and poly(ferro-sialate-disiloxo) binder type with a formula close to [Ca,Na,K,Mg]-[-Fe-O-](x)-[Si-O-Al-O-](1-x)-[-Si-O-](y). The physico-mechanical properties changed significantly. Setting time reduced by >95% in samples milled for 60 min or more. The compressive strength which was negligible for 0-30 min milled volcanic ash reached 29-54 MPa after 60-120 min of milling time. Heat curing influenced the early age (7 and 28 days) compressive strength but the 90 day compressive strength of both ambient and heat cured samples were comparable.
机译:本文探讨了使用低活性火山灰来制造地缘聚合物水泥的可能性。该研究旨在(a)通过机械活化的火山灰反应性改变(b)使用机械活化的火山灰来合成地质聚合物。机械活化的效果在粒度分布和结晶度的程度上非常可见。在火山灰烬中的一些钙质峰值和石英峰的出现消失为120分钟,证明了矿物学的变化。在机械活化期间,具有铣削时间的强碳酸盐带的外观可能与晶粒表面上的大气二氧化碳的吸附有关。火山灰机械活化的表现突出(a)反应动力学,(b)微观结构发育和(c)地质聚合物产物的物理机械性能。通过研磨时间增加,地质聚合物的速率恒定和程度增加,但固化温度降低。这种减少与用于偶然聚合物化的其他氧化铝 - 硅酸盐材料如甲曲蛋白和粉煤灰的不合格。 Feg-SEM和edax结果显示,获得的地质聚合物凝胶是聚(铁唾液酸硅氧烷)和聚(铁唾液酸二硅氧烷)粘合剂型的混合物,其配方接近[Ca,Na,K,Mg] - [ -fe-o - ](x) - [si-o-al-o - ](1-x) - [ - si-o - ](y)。物理机械性能显着变化。在铣削60分钟或更大的样品中,设定时间减少> 95%。在研磨时间60-120分钟后,0-30 min磨损的火山灰可忽略不计的抗压强度达到29-54MPa。热固化影响了休眠(7和28天)的抗压强度,但环境和热固化样品的90天抗压强度是可比的。

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  • 来源
    《RSC Advances》 |2016年第45期|共12页
  • 作者单位

    Univ Yaounde I Fac Sci Dept Inorgan Chem Lab Appl Inorgan Chem POB 812 Yaounde Cameroon;

    Univ Yaounde I Fac Sci Dept Inorgan Chem Lab Appl Inorgan Chem POB 812 Yaounde Cameroon;

    Univ Yaounde I Fac Sci Dept Inorgan Chem Lab Appl Inorgan Chem POB 812 Yaounde Cameroon;

    CSIR Natl Met Lab Jamshedpur 831007 Bihar India;

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  • 正文语种 eng
  • 中图分类 化学;
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