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Strength development in soft marine clay stabilized by fly ash and calcium carbide residue based geopolymer

机译:粉煤灰和电石渣渣基地质聚合物稳定的海洋软粘土的强度发展

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摘要

This research investigates strength development and the carbon footprint of Calcium Carbide Residue (CCR) and Fly Ash (FA) based geopolymer stabilized marine clay. Coode Island Silt (CIS), a soft and highly compressible marine clay present in Melbourne, Australia was investigated for stabilization with the CCR and FA geopolymers. CCR is an industrial by-product obtained from acetylene gas production, high in Ca(OH)(2) and was used as a green additive to improve strength of the FA based geopolymer binder. The liquid alkaline activator used was a mixture of sodium silicate solution (Na2SiO3) and sodium hydroxide (NaOH). The influential factors studied for the geopolymerization process were Na2SiO3/NaOH ratio, NaOH concentration, L/FA ratio, initial water content, FA content, CCR content, curing temperature and curing time. The strength of stabilized CIS was found to be strongly dependent upon FA content and NaOH concentration. The optimal ingredient providing the highest strength was found to be dependent on water content. Higher water contents were found to dilute the NaOH concentration, hence the optimal L/FA increases and the optimal Na2SiO3/NaOH decreases as the water content present in the clay increases. The maximum strength of the FA geopolymer (without CCR) stabilized CIS was found at Na2SiO3/NaOH = 70:30 ratio and L/FA = 1.0 for clay water content at liquid limit (LL). The role of CCR on the strength of FA geopolymer stabilized CIS can be classified into three zones: inactive, active and quasi-inert. The active zone where CCR content is between 7% and 12% is recommended in practice. The 12% CCR addition can improve up to 1.5 times the strength of the FA geopolymer. The carbon footprints of the geopolymer stabilized soils were approximately 22%, 23% and 43% lower than those of cement stabilized soil at the same strengths of 400 kPa, 600 kPa and 800 kPa. The reduction in carbon footprints at high strength indicates the effectiveness of FA geopolymer as an alternative and effective green soil stabilizer to traditional Portland cement. (C) 2016 Elsevier B.V. All rights reserved.
机译:这项研究调查了碳化钙残留物(CCR)和粉煤灰(FA)基地质聚合物稳定的海洋粘土的强度发展和碳足迹。研究了存在于澳大利亚墨尔本的Coode Island Silt(CIS)(一种柔软且高度可压缩的海洋粘土)与CCR和FA地质聚合物的稳定性。 CCR是从乙炔气生产中获得的工业副产品,Ca(OH)(2)含量高,并用作绿色添加剂以改善FA基地质聚合物粘合剂的强度。使用的液体碱性活化剂是硅酸钠溶液(Na 2 SiO 3)和氢氧化钠(NaOH)的混合物。影响地聚反应过程的因素是Na2SiO3 / NaOH比,NaOH浓度,L / FA比,初始水含量,FA含量,CCR含量,固化温度和固化时间。发现稳定的CIS的强度强烈依赖于FA含量和NaOH浓度。发现提供最高强度的最佳成分取决于水含量。发现较高的水含量可以稀释NaOH的浓度,因此,随着粘土中水含量的增加,最佳的L / FA会增加,而最佳的Na2SiO3 / NaOH会减少。在液体极限(LL)下,粘土水含量为Na2SiO3 / NaOH = 70:30,L / FA = 1.0时,发现了FA地聚合物(无CCR)稳定的CIS的最大强度。 CCR对FA地聚合物稳定的CIS强度的作用可分为三个区域:非活性区,活性区和准惰性区。在实践中建议CCR含量在7%和12%之间的有效区域。添加12%的CCR可以提高FA地质聚合物强度的1.5倍。在相同的400 kPa,600 kPa和800 kPa强度下,地聚合物稳定土的碳足迹比水泥稳定土的碳足迹分别低22%,23%和43%。高强度碳足迹的减少表明,FA地质聚合物可作为传统波特兰水泥的替代且有效的绿土稳定剂。 (C)2016 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《Applied clay science》 |2016年第7期|134-142|共9页
  • 作者单位

    Suranaree Univ Technol, Sch Civil Engn, 111 Univ Ave, Muang Dist 30000, Nakhon Ratchasi, Thailand;

    Suranaree Univ Technol, Sch Civil Engn, 111 Univ Ave, Muang Dist 30000, Nakhon Ratchasi, Thailand|Suranaree Univ Technol, Ctr Excellence Innovat Sustainable Infrastruct De, Muang Dist, Nakhon Ratchasi, Thailand;

    Swinburne Univ Technol, Dept Civil & Construct Engn, Hawthorn, Vic 3122, Australia;

    Rajamangala Univ Technol Isan, Program Civil Engn, Fac Engn & Architecture, Muang Dist 30000, Nakhon Ratchasi, Thailand;

    Suranaree Univ Technol, Sch Civil Engn, 111 Univ Ave, Muang Dist 30000, Nakhon Ratchasi, Thailand|Suranaree Univ Technol, Ctr Excellence Innovat Sustainable Infrastruct De, Muang Dist, Nakhon Ratchasi, Thailand;

  • 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

    Geopolymer; Strength; Coode Island Silt; Fly Ash; Calcium Carbide Residue; Marine clay; Carbon footprint;

    机译:地质聚合物;强度;库德岛粉砂;粉煤灰;碳化钙渣;海洋粘土;碳足迹;
  • 入库时间 2022-08-17 13:54:03

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