首页> 外文会议>Developments in strategic ceramic materials >METAKAOLIN-BASED GEOPOLYMER CEMENTS FROM COMMERCIAL SODIUM WATERGLASS AND SODIUM WATERGLASS FROM RICE HUSK ASH: A COMPARATIVE STUDY
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METAKAOLIN-BASED GEOPOLYMER CEMENTS FROM COMMERCIAL SODIUM WATERGLASS AND SODIUM WATERGLASS FROM RICE HUSK ASH: A COMPARATIVE STUDY

机译:来自商品钠水玻璃和稻壳灰的钠水玻璃的基于METAKAOLIN的地聚合物:对比研究

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摘要

Sodium waterglass (NWG) such as commercial NWG (SI), NWG from pure rice husk ash (S2) and NWG from raw rice husk ash (S3) were used for producing geopolymer cements from metakaolin (MK) as aluminosilicate source. Geopolymers (Geol, Geo2, Geo3) were prepared using each NWG with the molar ratios SiO_2/Na_2O and H_2O/Na_2O kept constant at 1.5 and 12 respectively. It could be observed that the water absorption of Geol, Geo2 and Geo3 are 7%, 9% and 13.2% and the mass loss are 15.8%, 14.7% and 12.4% respectively. The compressive strengths (43.3/40.3/33.2 MPa) decrease in the course Geol/Geo2/Geo3. It is discussed that the presence of phosphate known as corrosion inhibitors in raw rice husk ash hinders the dissolution of SiO_2. It entails the formation of NaH_2PO_4 in S3 which reduces the soluble Si atoms suggesting thus sodium waterglass from raw rice husk ash is a less depolymerized solution. Therefore, less amount of metakaolin could be dissolved leaving thus a higher amount of unreacted metakaolin particles in Geo3. The reacted volumes and compositions of the geopolymers are different in the three cases, too. A content of approximately 20%, 25% and 35% of unreacted metakaolin was proven for Geol, Geo2 and Geo3 respectively.
机译:水玻璃(NWG)(例如商业NWG(SI),纯米糠灰(S2)的NWG和原米糠灰(S3)的NWG)用于由偏高岭土(MK)作为铝硅酸盐源生产地聚合物水泥。使用每种NWG制备的地聚合物(Geol,Geo2,Geo3),其摩尔比SiO_2 / Na_2O和H_2O / Na_2O分别保持恒定在1.5和12。可以看出,Geol,Geo2和Geo3的吸水率分别为7%,9%和13.2%,质量损失分别为15.8%,14.7%和12.4%。在Geol / Geo2 / Geo3过程中,抗压强度(43.3 / 40.3 / 33.2 MPa)降低。据讨论,生稻壳灰中作为腐蚀抑制剂的磷酸盐的存在会阻止SiO_2的溶解。这需要在S3中形成NaH_2PO_4,这会减少可溶性Si原子,这表明来自稻壳灰的水玻璃酸钠是一种解聚程度较低的溶液。因此,较少量的偏高岭土可以溶解,因此在Geo3中留下了较高数量的未反应的偏高岭土颗粒。在三种情况下,地质聚合物的反应体积和组成也不同。已证明Geol,Geo2和Geo3分别含有约20%,25%和35%的未反应偏高岭土。

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  • 会议地点 Daytona Beach FL(US)
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    Laboratory of Applied Inorganic Chemistry, University of Yaounde I, Faculty of Science, Department of InorganicChemistry, PO. Box 812, Yaounde, Cameroon,Institut fuer Mineralogie, Leibniz Universitaet Hannover, Callinstrasse 3, D-30167 Hannover, Germany;

    Institut fuer Mineralogie, Leibniz Universitaet Hannover, Callinstrasse 3, D-30167 Hannover, Germany;

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