We present a micro-Raman study on the hydration and carbonation of the main silicate phases of Portland cement, i.e. monoclinic dicalcium silicate (C2S) and monoclinic tricalcium silicate (C3S). We investigate the reaction products and the loss of crystallinity induced by hydration on these two compounds. In the CO2-contaminated pastes we find that calcite, aragonite, and vaterite are inhomogeneously formed. We study sample cross sections to evaluate the maximum depth at which CaCO3 is formed. We find that carbonation is limited to the first 500-1000 mu m from the surface in the C3S pastes, while in C2S pastes CaCO3 is formed well beyond this depth. Our results show the great potential of Raman spectroscopy in the study of the chemistry of cements. Copyright (c) 2006 John Wiley & Sons, Ltd.
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School of Materials Science and Engineering, Shenyang Jianzhu UniversitySchool of Materials Science and Engineering, Shenyang Jianzhu University
房延凤
LIU Zhichao
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School of Civil Engineering, Shenyang Jianzhu UniversitySchool of Materials Science and Engineering, Shenyang Jianzhu University
LIU Zhichao
WANG Qinghe
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School of Materials Science and Engineering, Wuhan University of TechnologySchool of Materials Science and Engineering, Shenyang Jianzhu University
WANG Qinghe
ZHANG Yuzhuo
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School of Materials Science and Engineering, Wuhan University of TechnologySchool of Materials Science and Engineering, Shenyang Jianzhu University
ZHANG Yuzhuo
ZHANG Miao
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School of Materials Science and Engineering, Shenyang Jianzhu UniversitySchool of Materials Science and Engineering, Shenyang Jianzhu University
ZHANG Miao
王晴
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School of Materials Science and Engineering, Shenyang Jianzhu UniversitySchool of Materials Science and Engineering, Shenyang Jianzhu University