Journal
MATERIALS AND STRUCTURES
Volume 52, Issue 1, Pages -Publisher
SPRINGER
DOI: 10.1617/s11527-018-1307-8
Keywords
Autogenous shrinkage; Swelling; Hydration; Swelling; Drying; Biot coefficient; Pore water; Thermodynamics; Unsaturated poromechanics; Capillarity and adsorption
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Funding
- DoE through Los Alamos National Labgrant
- U.S. Department of Transportation through the Infrastructure Technology Institute of Northwestern University [20778]
- U.S. Department of Transportation through NSF [CMMI-1129449]
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A physically based model for auotgenous shrinkage and swelling of portland cement paste is necessary for computation of long-time hydgrothermal effects in concrete structures. The goal is to propose such a model. As known since 1887, the volume of cement hydration products is slightly smaller than the original volume of cement and water (chemical shrinkage). Nevertheless, this does not implythat the hydration reaction results in contraction of the concrete and cement paste. According to the authors' recently proposed paradigm, the opposite is true for the entire lifetime of porous cement paste as a whole. The hydration process causes permanent volume expansion of the porous cement paste as a whole, due to the growth of C-S-H shells around anhydrous cement grains which pushesthe neighbors apart, while the volume reduction of hydration products contributes to porosity. Additional expansion can happen due to the growth of ettringite and portlandite crystals. On the material scale, the expansion always dominates over the contraction, i.e., the hydration per se is, in the bulk, always and permanently expansive, while the source of all of the observed shrinkage, both autogenous and drying, is the compressive elastic or viscoelastic strain in the solid skeleton caused by a decrease of chemical potential of pore water, along with the associated decrease in pore relative humidity. As a result, the selfdesiccation, shrinkage and swelling can all be predicted from one and the same unified model, in which, furthermore, the low-density and high-density C-S-H are distinguished. A new thermodynamic formulation of unsaturated poromechanics with capillarity and adsorption is presented. The recently formulated local continuum model for calculating the evolution of hydration degree and a new formulation of nonlinear desorption isotherm are important for realistic and efficient finite element analysis of shrinkage and swelling. Comparisons with the existing relevant experimental evidence validate the proposed model.
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