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RICE HUSK ASH AS A SILICA SOURCE IN A GEOPOLYMER FORMULATION

机译:稻壳灰作为地聚合物配方中的二氧化硅来源

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Geopolymer is the refractory inorganic ps formed from both aluminum and silicon source. South Korean rice husk ash (RHA) has been investigated as an alternative silica source to replace fume silica currently used in geopolymer rdfdffdfdesearch. In order to acquire proper RHA from raw rice husk, the optimal calcination temperature, which produces the highest amount of amorphous silica, was studied. Scanning Electron Microscopy with Energy-Dispersive X-ray Spectroscopy (SEM-EDS) and X-ray diffraction (XRD) have been used to verify the contents of RHA. Previously many researchers have studied mixtures of RHA/fly ash (FA) or RHA/red mud (RM), resulting the ratio of SiO_2/Al_2O_3 varied by the each mixture. However, in this paper, RHA is only replaced to a certain portion of fumed silica. Thus, the fundamental ratio of each ingredient in the geopolymer (M: SiO_2: AlO_2: H_2O =1:1:4:11) where M is Na, K or Cs was strictly kept. Five variations of RHA/Fumed silica mixture (0/100, 25/75, 50/50, 75/25, 100/0) have been studied. Each mixture was dissolved with potassium hydroxide (KOH) and deionized water for 24 hours on the stirring plate and then became water glass. Metakaolin was added to water glass and mixed properly. The geopolymer slurry was poured into the mold and cured at 50℃ for 24 hours. After demolding, the RHA geopolymer samples were kept for a minimum of 3 days at the room temperature. The flexural stress of RHA geopolymer samples were investigated by 3-point bend tests at room temperature using the guidelines prescribed by ASTM C78/C78-M standard. The fracture surfaces from the bending tests were examined by using Scanning Electron Microscope (SEM). It was demonstrated that the RHA can clearly be the fumed-silica alternative.
机译:地质聚合物是由铝和硅来源形成的难熔无机ps。韩国稻壳灰(RHA)已作为替代二氧化硅的来源进行了研究,以取代目前在地质聚合物rdfdffdfdesearch中使用的烟气二氧化硅。为了从生稻壳中获得合适的RHA,研究了产生最大量无定形二氧化硅的最佳煅烧温度。带有能量色散X射线光谱仪(SEM-EDS)和X射线衍射仪(XRD)的扫描电子显微镜已用于验证RHA的含量。以前,许多研究人员研究了RHA /粉煤灰(FA)或RHA /红泥(RM)的混合物,导致SiO_2 / Al_2O_3的比例随每种混合物而变化。但是,在本文中,RHA仅被替换为气相二氧化硅的特定部分。因此,严格保持了其中M为Na,K或Cs的地聚合物中每种成分的基本比率(M:SiO_2:AlO_2:H_2O = 1:1:4:11)。研究了五种RHA /气相二氧化硅混合物(0 / 100、25 / 75、50 / 50、75 / 25、100 / 0)。将每种混合物在搅拌板上用氢氧化钾(KOH)和去离子水溶解24小时,然后变成水玻璃。将偏高岭土加入水玻璃中并适当混合。将地质聚合物浆液倒入模具中,并在50℃固化24小时。脱模后,将RHA地质聚合物样品在室温下至少保留3天。使用ASTM C78 / C78-M标准规定的准则,在室温下通过三点弯曲试验研究了RHA地聚合物样品的弯曲应力。通过使用扫描电子显微镜(SEM)检查来自弯曲测试的断裂表面。事实证明,RHA可以明显地替代气相二氧化硅。

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  • 会议地点 Daytona Beach FL(US)
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    Department of Material Science and Engineering, University of Illinois at Urbana-Champaign Urbana, IL, USA;

    Department of Material Science and Engineering, University of Illinois at Urbana-Champaign Urbana, IL, USA;

    Department of Material Science and Engineering, University of Illinois at Urbana-Champaign Urbana, IL, USA;

    Department of Material Science and Engineering, University of Illinois at Urbana-Champaign Urbana, IL, USA;

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