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Alkali activation behaviour of un-calcined montmorillonite and illite clay minerals

机译:未煅烧蒙脱石和伊利石黏土矿物的碱活化行为

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摘要

Using alkali activation, un-calcined soils have potential as precursors for low carbon, low cost, geopolymer-stabilised construction materials. This technology has been recently promoted as a lower impact alternative to cement stabilisation for walling materials in construction around the world. There is a lack of fundamental understanding around the alkali activation of un-calcined montmorillonite and illite, which, along with kaolinite, are clay minerals commonly found in soils. Kaolinite, as a 1:1 clay mineral, has been shown to form crystalline hydrosodalite when alkali-activated, but 2:1 montmorillonite and illite could form stronger geopolymer structures due to the higher Si:Al ratio in the precursor mineral. The lack of understanding of the underlying mechanisms at work with 2:1 clay minerals is a barrier to knowing how viable un-calcined geopolymer stabilised soil materials are for the range of soil types found in nature. In this study, montmorillonite and illite precursors were activated with a range of sodium hydroxide concentrations, compacted, and then cured at 80 degrees C for 24 h. The cured samples were characterised using a variety of advanced analytical techniques, including powder XRD, SEM, TGA, Al-27 and Si-29-MAS-NMR, and FTIR. For the first time it was confirmed that alkali activation of uncalcined montmorillonite forms a NASH or (N,C)ASH geopolymer as the major product phase, which increases in quantity with increasing Na:Al molar ratio of the system. Although it has a similar Si:Al ratio, alkali activation of illite seems to result in structural alteration and increased porosity for Na:Al = 0.5. The behaviour of these individual clay minerals suggests that the alkali activation of un-calcined 2:1 clay minerals is complex. Although alkali activation of montmorillonite can form a geopolymer, alkali activation of soils containing illite may lead to poor quality materials. This research has shown that the focus of future development work should be around montmorillonite-based clays.
机译:使用碱活化,未煅烧的土壤有可能成为低碳,低成本,经地质聚合物稳定的建筑材料的前体。最近,该技术已被推广为对世界各地建筑墙体材料使用的水泥稳定剂的影响较小的替代品。对于未煅烧的蒙脱石和伊利石(它们与高岭石一起是土壤中常见的粘土矿物)的碱活化缺乏基本的了解。高岭石作为一种1:1的粘土矿物,经碱活化后已显示出形成结晶的水钠钙石,但2:1的蒙脱石和伊利石由于前体矿物中较高的Si:Al比而可形成更强的地质聚合物结构。缺乏对使用2:1粘土矿物的潜在机理的了解,阻碍了人们了解未煅烧的地聚合物稳定的土壤材料对于自然界中各种土壤类型的可行性。在这项研究中,将蒙脱石和伊利石前体用一定浓度的氢氧化钠活化,压实,然后在80摄氏度下固化24小时。使用各种先进的分析技术(包括粉末XRD,SEM,TGA,Al-27和Si-29-MAS-NMR和FTIR)对固化的样品进行表征。首次证实未煅烧的蒙脱石的碱活化形成NASH或(N,C)ASH地质聚合物作为主要产物相,其数量随体系中Na:Al摩尔比的增加而增加。尽管它具有相似的Si:Al比,但伊利石的碱活化似乎会导致Na:Al> = 0.5的结构改变和增加的孔隙率。这些单独的粘土矿物的行为表明未煅烧的2:1粘土矿物的碱活化是复杂的。尽管蒙脱石的碱活化可形成地聚合物,但对含伊利石的土壤进行碱活化可能会导致劣质材料。这项研究表明,未来开发工作的重点应该放在蒙脱石基粘土周围。

著录项

  • 来源
    《Applied clay science 》 |2018年第12期| 250-261| 共12页
  • 作者单位

    Univ Bath, Dept Architecture & Civil Engn, Bath BA2 7AY, Avon, England;

    Univ Bath, Dept Architecture & Civil Engn, Bath BA2 7AY, Avon, England;

    Univ Bath, Dept Chem, Bath BA2 7AY, Avon, England;

    Univ Bath, Dept Architecture & Civil Engn, Bath BA2 7AY, Avon, England;

    Univ Bath, Dept Architecture & Civil Engn, Bath BA2 7AY, Avon, England;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Alkali activation; Geopolymer; Montmorillonite; Illite; Clay;

    机译:碱活化;地聚合物;蒙脱土;伊利石;粘土;

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