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IR Spectral Similarity Studies of Geothermal Silica-Bentonite Based Geopolymer

机译:地质二氧化硅 - 膨润土基地质聚合物的IR光谱相似性研究

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The geopolymer structures are formed through polymerization of silicate and aluminate species. The resulted structure is predicted to be similar with zeolite. In this study, geopolymer samples were made from mix powder of geothermal silica and bentonite, then activated with sodium hydroxide and sodium silicate. The effect of silica content, NaOH molarity and curing temperature effect were investigated on geopolymer IR spectra and compared with 3A zeolite IR spectra. Pearson correlation value (r) and spectral similarity correlation (Corr) were used to assess spectra similarity between geopolymer samples and zeolite. The development of geopolymer bond and microstructure of samples were then investigated by FTIR technique. IR spectra of geopolymer samples show that Si-O-Al absorption bands are formed around 900-1300 cm~(-1) and 400-800 cm~(-1). The optimum of silica contents, NaOH molarity and curing temperature obtained from the experiment were 140 grams, 10 M and 80°C with Corr value of 922 and compressive strength of 7,59 MPa. Corr value is proven to have relation with material strength. Higher Corr value is identified to have higher aluminosilicate species which contributes to higher compressive strength.
机译:通过硅酸盐和铝酸盐物质的聚合形成地质聚合物结构。预测所得结构与沸石相似。在该研究中,地质聚合物样品由地热二氧化硅和膨润土的混合粉末制成,然后用氢氧化钠和硅酸钠活化。研究了二氧化硅含量,NaOH摩尔性和固化温度效应的影响,并与3A沸石IR光谱进行比较。 Pearson相关值(R)和光谱相似性相关性(COR)用于评估地质组聚合物样品和沸石之间的光谱相似性。然后通过FTIR技术研究了地质聚合物键和样品的微观结构。地质物样品的IR光谱表明,Si-O-Al吸收带形成约900-1300cm〜(-1)和400-800cm〜(-1)。从实验中获得的二氧化硅含量,NaOH摩尔性和固化温度的最佳值为140克,10μm和80℃,腐蚀值为922,抗压强度为7,59MPa。经证据腐败价值与材料强度有关。鉴定出更高的腐蚀值以具有更高的硅铝酸盐物质,这有助于更高的抗压强度。

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