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Structure and development of fly ash and red mud-based geopolymers

机译:粉煤灰和赤泥基地质聚合物的结构与开发

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摘要

This research explores the role of water in fly ash-based geopolymers using the less conventional activators; Na2CO3 and Ca(OH)2. It included the determination of evaporable and combined water at ambient, 105°C and 1050 °C, and characterization of the micro-structure using SEM, XRD, IR, TGA and NMR. The results obtained suggested that the resulting geopolymer compounds contain a measurable amount of non-evaporable/combined water (which escapes at and above 105 °C) as distinguished from structural water which is rigidly bound, mainly by hydrogen bonding and constitutes an integral part of the geopolymer matrix in the form of molecular water. The backbone structure of Si-O-T (T=Si, Al) bonds was formed and developed as the reaction proceeds. The majority of the water escapes at below 200 °C, which enables the geopolymer to maintain its structural integrity at 1050 °C. The perception of whether Na-geopolymer is sodium aluminosilicate hydrate (N-A-S-H) was discussed, however, no sufficient evidence from IR, TGA and NMR was found in this research to prove that the geopolymer is a hydrate.The research also addresses the possibility of using red mud as an activator and a filler for fly ash-based geopolymers. The effect of activators such as Ca(OH)2, waterglass and NaOH on fly ash and red mud-based geopolymers were investigated. The micro-structure of such geopolymers was examined using techniques mentioned above. The results obtained suggested that red mud is not efficient as an activator for fly ash based-geopolymers; NaOH (above 4 M) causes the leaching of sodium resulting in formation of Na2CO3 in red mud-based geopolymers; water glass (mass ratio of SiO2 to Na2O is 2), which is effective for activating fly ash, led to unsatisfactory results with red mud based-geopolymers; 10% addition of Ca(OH)2 proved to be effective for red mud and fly ash based-geopolymers.This research provides an in-depth investigation on whether geopolymeric product is a hydrate. It also explores the possibility of non-traditional activators, such as red mud, from a novel angle. Further, it investigates the micro-structure of geopolymers using red mud which is a high Fe containing material, as a raw material.
机译:这项研究探索了水在使用较少常规活化剂的粉煤灰基地聚合物中的作用。 Na2CO3和Ca(OH)2。它包括在环境温度,105°C和1050°C下测定可蒸发和合并的水,并使用SEM,XRD,IR,TGA和NMR表征微观结构。所获得的结果表明,所得的地质聚合物化合物包含可测量量的不可蒸发/混合水(在105°C或以上逸出),与主要通过氢键牢固结合的结构水区别开来,构成了水的组成部分。分子水形式的地质聚合物基质。 Si-O-T(T = Si,Al)键的主链结构随着反应的进行而形成和发展。大部分水在低于200°C的温度下逸出,这使地质聚合物能够在1050°C下保持其结构完整性。讨论了关于Na-地聚合物是否为铝硅酸钠水合物(NASH)的看法,但是,本研究未从IR,TGA和NMR中获得足够的证据来证明该地聚合物是水合物。红泥作为粉煤灰基地质聚合物的活化剂和填料。研究了活化剂如Ca(OH)2,水玻璃和NaOH对粉煤灰和赤泥基地质聚合物的影响。使用上述技术检查了这种地质聚合物的微观结构。得到的结果表明赤泥不能有效地用作粉煤灰基地聚合物的活化剂。 NaOH(高于4 M)引起钠的浸出,导致在赤泥基地质聚合物中形成Na 2 CO 3。水玻璃(SiO2与Na2O的质量比为2)可有效活化粉煤灰,导致赤泥基地质聚合物的效果不理想;事实证明,添加10%的Ca(OH)2对于赤泥和粉煤灰基地质聚合物是有效的。本研究对地质聚合物产品是否为水合物进行了深入研究。它还从新颖的角度探讨了非传统活化剂(如赤泥)的可能性。此外,研究了使用高铁含量的赤泥作为原料的地聚合物的微观结构。

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