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Thermomechanical modelling of maturing concrete mixture<br />

Stanislav Šťastník, Jiří Vala, Jaroslav Nováček<br />

Faculty of Civil Engineering, Brno University of Technology,<br />

Veveří 95, CZ ‐ 602 00 Brno, Czech Republic,<br />

email: stastnik.s@fce.vutbr.cz, vala.j@fce.vutbr.cz, novacek.j@fce.vutbr.cz<br />

Abstract: Concrete is a natural composite whose properties are determined by hygro‐thermo‐chemo‐<br />

mechanical processes at early age of its existence. Namely in the case of massive structures such processes<br />

should be controlled carefully to guarantee the optimal behaviour of a structure according to its proposed<br />

use. The complete mathematical model of heated concrete, treated as a multi‐phase porous material,<br />

consists i) of 20 balance equations, coming from the mass, momentum and energy balance laws for<br />

continua with microstructure, corresponding to solid concrete, liquid mixture, water vapour and dry air,<br />

coming from the mass, momentum and energy balance laws for continua with microstructure and ii) of a<br />

set of constitutive relationships, identified by laboratory experiments. Some preliminary simulation<br />

results are available.<br />

Keywords: Material properties of early‐age concrete, thermodynamic principles, hygro‐thermo‐chemo‐<br />

mechanical modelling, partial differential equations of evolution.<br />

Introduction<br />

Quantitative analysis of early‐age behaviour of concrete is a rather complicated multi‐physical<br />

problem. Every reliable thermomechanical model of maturing concrete mixture should include<br />

at least a) reversible elastic deformation, b) viscous creep of material and c) volume changes,<br />

unlike a) and b) independent of external loads, namely c1) autogenous volume changes, driven<br />

by chemical shrinkage of cement particles, c2) subsequent thermal expansion, c3) drying caused<br />

by water loss into environment and c4) later carbonation. Three principal internal and external<br />

influences are 1) internal hydration heat, generated by the hydration hydraulic processes, 2)<br />

ambient temperature variation, connected with ambient humidity variation (natural or artificial<br />

ones), 3) external mechanical loads; thus evidently hygro‐thermo‐chemo‐mechanical modelling<br />

and simulation is needed.<br />

Moreover, the proper quantitative study such physical and chemical processes should be<br />

supported by the multi‐scale analysis: especially [4] for samples prepared as mixtures of<br />

cement, water and air distinguishes anhydrous‐cement scale (from 10 ‐8 to 10 ‐6 m), cement‐paste<br />

scale (from 10 ‐6 to 10 ‐4 m) with growing crystals and capillary phenomena, mortar scale (about<br />

10 ‐2 m) with particles included in a seemingly homogenous matrix and macroscale (about 10 ‐1 m)<br />

for a natural composite. The physical formulations come i) in [1] from common<br />

phenomenological relations with a large number of model parameters, ii) in [7] from<br />

phenomenological coefficients in Onsager reciprocity relations and Gibbs‐Duhem conditions,<br />

iii) in [2] and [4] from mechanistic calculations at representative volume elements for<br />

multiple scales and, alternatively, iv) in [3] and [5] from thermodynamic conservation<br />

principles applied to hybrid mixture theory.<br />

The mathematical and computational homogenization techniques cannot be assigned to i), ii),<br />

iii), iv) exactly; their applicability is also limited by reasonable quantitative data from laboratory<br />

measurements (at all considered scales) and corresponding observations in situ. In the rough<br />

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