This paper studied in situ, by Micro-Raman spectroscopy, the very early hydration of C(3)A in the presence and absence of sulphates and with sucrose as an additive. For C(3)A hydration in the absence of gypsum, when carbonation is not avoided, carbonate-AFm phases are formed, but in the presence of gypsum, hydroxi-AFm are the main phases. Ettringite is the AFm stable phase developed initially at 70 min of hydration with gypsum and no monosulphate is formed. In the presence of sucrose, this salt, instead of sulphate, is adsorbed over the surface of the C(3)A, avoiding its reaction with sulphates until sucrose desorption. Three hours are necessary to lead to ettringite formation. A nucleation poisoning/adsorption surface mechanism is proposed for added sucrose systems. (C) 2016 Elsevier Ltd. All rights reserved.
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Chinese Acad Sci, Lab High Temp & High Pressure Study Earths Interi, Inst Geochem, 99 Lincheng West Rd, Guiyang 550081, Guizhou, Peoples R China
Univ Chinese Acad Sci, Beijing 100049, Peoples R ChinaChinese Acad Sci, Lab High Temp & High Pressure Study Earths Interi, Inst Geochem, 99 Lincheng West Rd, Guiyang 550081, Guizhou, Peoples R China
Chen Lin
Li Heping
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Chinese Acad Sci, Lab High Temp & High Pressure Study Earths Interi, Inst Geochem, 99 Lincheng West Rd, Guiyang 550081, Guizhou, Peoples R ChinaChinese Acad Sci, Lab High Temp & High Pressure Study Earths Interi, Inst Geochem, 99 Lincheng West Rd, Guiyang 550081, Guizhou, Peoples R China
Li Heping
Li Shengbin
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Chinese Acad Sci, Lab High Temp & High Pressure Study Earths Interi, Inst Geochem, 99 Lincheng West Rd, Guiyang 550081, Guizhou, Peoples R China
Univ Chinese Acad Sci, Beijing 100049, Peoples R ChinaChinese Acad Sci, Lab High Temp & High Pressure Study Earths Interi, Inst Geochem, 99 Lincheng West Rd, Guiyang 550081, Guizhou, Peoples R China
Li Shengbin
Xu Liping
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Zhejiang Pharmaceut Coll, Ningbo 315100, Peoples R ChinaChinese Acad Sci, Lab High Temp & High Pressure Study Earths Interi, Inst Geochem, 99 Lincheng West Rd, Guiyang 550081, Guizhou, Peoples R China
Xu Liping
Lin Sen
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Chinese Acad Sci, Lab High Temp & High Pressure Study Earths Interi, Inst Geochem, 99 Lincheng West Rd, Guiyang 550081, Guizhou, Peoples R ChinaChinese Acad Sci, Lab High Temp & High Pressure Study Earths Interi, Inst Geochem, 99 Lincheng West Rd, Guiyang 550081, Guizhou, Peoples R China
Lin Sen
Zhou Hongbin
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Chinese Acad Sci, Lab High Temp & High Pressure Study Earths Interi, Inst Geochem, 99 Lincheng West Rd, Guiyang 550081, Guizhou, Peoples R ChinaChinese Acad Sci, Lab High Temp & High Pressure Study Earths Interi, Inst Geochem, 99 Lincheng West Rd, Guiyang 550081, Guizhou, Peoples R China
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Laboratory of High Temperature and High Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences
University of Chinese Academy of Sciences,Beijing 100049,ChinaLaboratory of High Temperature and High Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences
Lin Chen
Heping Li
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Laboratory of High Temperature and High Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of SciencesLaboratory of High Temperature and High Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences
Heping Li
Shengbin Li
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Laboratory of High Temperature and High Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences
University of Chinese Academy of SciencesLaboratory of High Temperature and High Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences
Shengbin Li
Liping Xu
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Zhejiang Pharmaceutical CollegeLaboratory of High Temperature and High Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences
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Sen Lin
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Laboratory of High Temperature and High Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of SciencesLaboratory of High Temperature and High Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences
Sen Lin
Hongbin Zhou
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Laboratory of High Temperature and High Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of SciencesLaboratory of High Temperature and High Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences
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Laboratory of High Temperature and High Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences
University of Chinese Academy of Sciences,Beijing ,ChinaLaboratory of High Temperature and High Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences
Lin Chen
Heping Li
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Laboratory of High Temperature and High Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of SciencesLaboratory of High Temperature and High Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences
Heping Li
Shengbin Li
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Laboratory of High Temperature and High Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences
University of Chinese Academy of SciencesLaboratory of High Temperature and High Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences
Shengbin Li
Liping Xu
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Laboratory of High Temperature and High Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of SciencesLaboratory of High Temperature and High Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences
Sen Lin
Hongbin Zhou
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Laboratory of High Temperature and High Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of SciencesLaboratory of High Temperature and High Pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences