Mechanisms of cement hydration

被引:1393
作者
Bullard, Jeffrey W. [1 ]
Jennings, Hamlin M. [2 ]
Livingston, Richard A. [3 ]
Nonat, Andre [4 ]
Scherer, George W. [6 ]
Schweitzer, Jeffrey S. [5 ]
Scrivener, Karen L. [7 ]
Thomas, Jeffrey J. [8 ]
机构
[1] Natl Inst Stand & Technol, Mat & Construct Res Div, Gaithersburg, MD 20899 USA
[2] MIT, Dept Civil & Environm Engn, Cambridge, MA 02139 USA
[3] Univ Maryland, Dept Mat Sci & Engn, College Pk, MD 20742 USA
[4] Univ Bourgogne, CNRS, UMR 5209, Lab Interdisciplinaire Carnot de Bourgogne ICB, Dijon, France
[5] Univ Connecticut, Dept Phys, Storrs, CT USA
[6] Princeton Univ, Dept Civil & Environm Engn, PRISM, Princeton, NJ 08544 USA
[7] Ecole Polytech Fed Lausanne, Inst Mat, Construct Mat Lab, Lausanne, Switzerland
[8] Schlumberger Doll Res Ctr, Cambridge, MA USA
基金
美国国家科学基金会;
关键词
Hydration; Kinetics; Microstructure; C-S-H; CALCIUM-SILICATE-HYDRATE; TRICALCIUM SILICATE; PORTLAND-CEMENT; INDUCTION PERIOD; INDIVIDUAL PARTICLES; MOLECULAR-DYNAMICS; NEUTRON-SCATTERING; DISSOLUTION; GROWTH;
D O I
10.1016/j.cemconres.2010.09.011
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The current state of knowledge of cement hydration mechanisms is reviewed, including the origin of the period of slow reaction in alite and cement, the nature of the acceleration period, the role of calcium sulfate in modifying the reaction rate of tricalcium aluminate, the interactions of silicates and aluminates, and the kinetics of the deceleration period. In addition, several remaining controversies or gaps in understanding are identified, such as the nature and influence on kinetics of an early surface hydrate, the mechanistic origin of the beginning of the acceleration period, the manner in which microscopic growth processes lead to the characteristic morphologies of hydration products at larger length scales, and the role played by diffusion in the deceleration period. The review concludes with some perspectives on research needs for the future. Published by Elsevier Ltd.
引用
收藏
页码:1208 / 1223
页数:16
相关论文
共 125 条
[1]  
Adamson A.W., 1967, Physical Chemistry of Surfaces
[2]   In situ quasi-elastic scattering characterization of particle size effects on the hydration of tricalcium silicate [J].
Allen, AJ ;
McLaughlin, JC ;
Neumann, DA ;
Livingston, RA .
JOURNAL OF MATERIALS RESEARCH, 2004, 19 (11) :3242-3254
[3]   TIME-RESOLVED PHENOMENA IN CEMENTS, CLAYS AND POROUS ROCKS [J].
ALLEN, AJ .
JOURNAL OF APPLIED CRYSTALLOGRAPHY, 1991, 24 :624-634
[4]   DEVELOPMENT OF THE FINE POROSITY AND GEL STRUCTURE OF HYDRATING CEMENT SYSTEMS [J].
ALLEN, AJ ;
OBERTHUR, RC ;
PEARSON, D ;
SCHOFIELD, P ;
WILDING, CR .
PHILOSOPHICAL MAGAZINE B-PHYSICS OF CONDENSED MATTER STATISTICAL MECHANICS ELECTRONIC OPTICAL AND MAGNETIC PROPERTIES, 1987, 56 (03) :263-288
[5]   Composition and density of nanoscale calcium-silicate-hydrate in cement [J].
Allen, Andrew J. ;
Thomas, Jeffrey J. ;
Jennings, Hamlin M. .
NATURE MATERIALS, 2007, 6 (04) :311-316
[6]  
[Anonymous], 2008, THESIS ECOLE POLYTEC
[7]  
Arvidson RS, 2008, GEOCHIM COSMOCHIM AC, V72, pA34
[8]   Variation in calcite dissolution rates: A fundamental problem? [J].
Arvidson, RS ;
Ertan, IE ;
Amonette, JE ;
Luttge, A .
GEOCHIMICA ET COSMOCHIMICA ACTA, 2003, 67 (09) :1623-1634
[9]   MECHANISM OF C3S DISSOLUTION AND PROBLEM OF THE CONGRUENCY IN THE VERY INITIAL PERIOD AND LATER ON [J].
BARRET, P ;
MENETRIER, D ;
BERTRANDIE, D .
CEMENT AND CONCRETE RESEARCH, 1983, 13 (05) :728-738
[10]   FILTER DISSOLUTION OF C3S AS A FUNCTION OF THE LIME CONCENTRATION IN A LIMITED AMOUNT OF LIME WATER [J].
BARRET, P ;
MENETRIER, D .
CEMENT AND CONCRETE RESEARCH, 1980, 10 (04) :521-534