Clay-Based Materials in Geopolymer Technology

M. Abdullah, L. Ming, Heah Cheng-Yong, M. F. Tahir
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引用次数: 49

Abstract

The term “geopolymer” was introduced by Davidovits in the 1970s. The prefix “geo” was selected to symbolize the constitutive relationship of the binders to geological materials, natural stone and/or minerals. Geopolymer is mineral polymers of inorganic polymer glasses with structure resembling natural zeolitic materials. Previously, geopolymer formation used source materials such as clay (e.g. kaolin and calcined kaolin) or industrial by-product (e.g. slag and fly ash). The precursor material plays an important role in the formation of geopolymer. The source material provides silicon (Si) and aluminum (Al) for reaction by an alkali activator solution. The Si and Al contents in the source materials dissolve in the alkaline activator solution and then polymerize to form a polymeric Si-O-Al-O framework which becomes the binder. Geopolymeric materials are attractive because of their excellent mechanical properties; durability and thermal stability can also be achieved. Owing to their low calcium content, they are more resistant to acid attack than materials based on Portland cement. In addition, they are of great interest because of the reduced energy requirement for their manufacture and the higher sustainability. Recently the search for alternative low cost and easily available materials led among oth- ers to Clay. Clay generally consists of a mixture of different clay minerals and associated minerals, which are strongly affected by the nature of the parent rocks. These materials are extensively distributed over the surface of the world and may show certain reac tivity after a thermal activation process shows a great potential to be utilized in geo- polymer technology. This article presents the potential of different types of clay as the source materials for geopolymerization reaction in terms of morphological properties. Moreover, the mechanical and microstructural properties of geopolymer made with various kinds of clay and its potential application are also presented.
土聚合物技术中的粘土基材料
“地聚合物”一词是由Davidovits在20世纪70年代提出的。选择前缀“geo”来象征粘合剂与地质材料、天然石材和/或矿物的本构关系。地聚合物是无机聚合物玻璃的矿物聚合物,其结构类似于天然沸石材料。以前,地聚合物的形成使用粘土(如高岭土和煅烧高岭土)或工业副产品(如矿渣和粉煤灰)等原料。前驱体材料在地聚合物的形成中起着重要的作用。源材料提供硅(Si)和铝(Al),用于碱激活剂溶液的反应。原料中的Si和Al含量溶解在碱性活化剂溶液中,然后聚合形成聚合物Si- o -Al- o骨架,成为粘合剂。地聚合物材料因其优异的力学性能而备受青睐;耐久性和热稳定性也可以实现。由于钙含量低,它们比波特兰水泥基材料更耐酸侵蚀。此外,由于其制造的能源需求减少和更高的可持续性,它们引起了极大的兴趣。最近,人们在寻找低成本和容易获得的替代材料时,把目光投向了粘土。粘土通常由不同粘土矿物和伴生矿物的混合物组成,这些矿物受母岩性质的强烈影响。这些材料广泛分布在地球表面,经热活化后可表现出一定的反应性,在地质聚合物技术中具有很大的应用潜力。本文从形态性质方面介绍了不同类型粘土作为地聚合反应源物质的潜力。此外,还介绍了各种粘土制成的地聚合物的力学和微观结构特性及其潜在的应用前景。
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