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首页> 外文期刊>Magazine of Concrete Research >Investigation of pore structure and ITZ of concrete blended with mineral admixtures in a seawater environment
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Investigation of pore structure and ITZ of concrete blended with mineral admixtures in a seawater environment

机译:海水环境下掺矿物掺合料混凝土的孔结构和ITZ研究。

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摘要

The pore structure and interfacial transition zone (ITZ) in seawater concrete as indicators of marine concrete durability are explored and analysed. Mercury intrusion porosimetry, microhardness tester and scanning electron microscopy are employed to characterise the evolution of the pore structure and ITZ with curing time. Effects of mineral admixtures including slag, silica fume and metakaolin on pore structure and ITZ are also investigated. In addition, the influence of slag, silica fume and metakaolin on the thermodynamic stability of hydrate phases is investigated. The experimental results show that, compared to normal concrete, concrete subjected to simulated seawater conditions at early ages has a higher ratio of fine porosity as well as higher ITZ microhardness, and the ITZ is narrower. However, the microstructure of concrete in the seawater environment degrades up to longer ages. With the addition of mineral admixtures, the pore characteristics of marine concrete are greatly improved. The effect of the mineral admixtures on microstructure is in the sequence: metakaolin > silica fume > slag. Thermodynamic analysis indicates that stable hydration products ettringite (C6AsH32:6CaO center dot Al2O3.3CaSO(4).32H(2)O) and siliceous hydrogarnet (C3As0.8H4.4:3CaO center dot Al2O3 center dot 0.8SiO(2)center dot 4.4H(2)O) form due to pozzolanic reactions to optimise the microstructure and enhance the compressive strength of concrete.
机译:探索和分析了海水混凝土中的孔结构和界面过渡区(ITZ),作为海洋混凝土耐久性的指标。采用水银压入孔隙率法,显微硬度测试仪和扫描电子显微镜来表征孔结构和ITZ随固化时间的演变。还研究了矿渣,矿渣,硅粉和偏高岭土等矿物混合物对孔结构和ITZ的影响。另外,研究了炉渣,硅粉和偏高岭土对水合物相热力学稳定性的影响。实验结果表明,与普通混凝土相比,早期模拟海水条件下的混凝土具有较高的细孔比和较高的ITZ显微硬度,并且ITZ较窄。但是,海水环境中混凝土的微观结构会退化到更长的寿命。通过添加矿物掺合料,大大改善了船用混凝土的孔隙特性。矿物掺合料对微观结构的影响顺序为:偏高岭土>硅粉>矿渣。热力学分析表明稳定的水合产物钙矾石(C6AsH32:6CaO中心点Al2O3.3CaSO(4).32H(2)O)和硅质水石榴石(C3As0.8H4.4:3CaO中心点Al2O3中心点0.8SiO(2)中心点4.4H(2)O)由于火山灰反应而形成,可优化微观结构并增强混凝土的抗压强度。

著录项

  • 来源
    《Magazine of Concrete Research》 |2015年第16期|812-820|共9页
  • 作者

    Duan Ping; Zhou Wei; Yan Chunjie;

  • 作者单位

    China Univ Geosci, Fac Mat Sci, Wuhan 430074, Peoples R China|China Univ Geosci, Chem & Engn Res Ctr Nanogeomat, Minist Educ, Wuhan 430074, Peoples R China|China Univ Geosci, Zhejiang Res Inst, Hangzhou, Zhejiang, Peoples R China;

    China Univ Geosci, Fac Mat Sci, Wuhan 430074, Peoples R China|China Univ Geosci, Chem & Engn Res Ctr Nanogeomat, Minist Educ, Wuhan 430074, Peoples R China;

    China Univ Geosci, Zhejiang Res Inst, Hangzhou, Zhejiang, Peoples R China|China Univ Geosci, Chem & Engn Res Ctr Nanogeomat, Minist Educ, Wuhan 430074, Peoples R China|China Univ Geosci, Fac Mat Sci, Wuhan 430074, Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
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