Abstract
The equations governing drying and wetting of concrete are formulated, assuming the diffusivity and other material parameters to be dependent on pore humidity, temperature and degree of hydration. By fitting of computer solutions for slabs, cylinders and spheres against numerous test data available in the literature it is found that the diffusion coefficient decreases about 10 to 20 times when passing from 0.9 to 0.6 pore humidity. The problem is thus strongly nonlinear. Dependence on temperature is found to agree satisfactorily with the rate process theory. Effect of temperature on equilibrium pore humidity is also studied. The aging effect is defined by means of an equivalent hydration period. To enable easy prediction of drying of simple bodies, charts for the solution in terms of nondimensional variables are presented. Finally, correlation to the diffusion in a saturated concrete is discussed.
Résumé
On présente les équations du séchage et de l'humidification du béton, étant supposé que le coefficient de diffusion et les autres paramètres du matériau sont déterminés par l'humidité interstitielle, la température et le degré d'hydratation. On examine le traitement numérique de l'équation de diffusion, et par comparaison des solutions calculées pour le séchage de dalles, cylindres et sphères, avec les nombreux résultats d'essais fournis par la littérature on démontre que le coefficient de diffusion diminue d'environ 20 fois lorsque l'humidité interstitielle passe de 0,9 à 0,6. On voit donc que le problème de la diffusion est nettement non linéaire. Ce résultat confirme aussi que la migration superficielle le long des couches constitue le mécanisme dominant de la diffusion. L'influence de la température se révèle en accord satisfaisant avec le concept d'énergie d'activation. L'effet de la température sur l'équilibre de l'humidité interstitielle est traduit par un coefficient hygrothermique dont on donne les valeurs approximatives. On tient compte des variations des paramètres des matériaux avec l'âge du béton par l'intermédiaire d'une période équivalente d'hydratation dont l'accroissement dépend de la température et de l'humidité interstitielle. On montre que l'influence de l'humidité interstitielle sur la perméabilité peut être très simplement déterminée en mesurant le transfert permanent de l'eau à travers des parois minces dont l'une des faces est exposée à différentes conditions d'humidité ambiante. Afin de faciliter la prédiction du séchage de corps simples, on présente des diagrammes pour la résolution du problème du séchage non linéaire en fonction de variables non dimensionnelles. Enfin on examine la diffusion de l'eau dans des éléments présentant des régions de béton saturé sous une surpression hydraulique, à côté de régions de béton non saturé. On montre que de part et d'autre de la limite entre ces deux régions, le coefficient de diffusion varie d'environ / 000 fois.
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Abbreviations
- c, ĉ:
-
permeability given by Eqs. (1) and (3)
- C, C1 :
-
diffusivity (Eqs. 8–11) and its value at H→1
- H, H en , H s , H eq :
-
pore humidity (or relative vapor pressure), environmental humidity (Eq. 12), self-dessiccation (Eq. 4), and equivalent humidity (Eq. 22)
- H c :
-
parameter in Eq. (20)
- J:
-
mass flux of water (Eq. 1)
- k:
-
inverse slope of desorption isotherm (Eq. 4)
- L:
-
half thickness of a slab
- n:
-
exponent in Eq. (20)
- p1, p v :
-
pressure in pore water or pore vapor
- Q, Q h :
-
activation energy for diffusion (Eq. 21) and for hydration (Eq. 7a)
- r:
-
radius coordinate
- R:
-
radius of a cylinder or a sphere
- t, t e , t0 :
-
time, equivalent hydration period (Eq. 7) and instant of drying exposure
- T:
-
absolute temperature
- W, W e , W n :
-
mass of water contained in a unit volume of material, and its evaporable and non-evaporable parts (Eqs. 4, 9–11)
- x:
-
coordinate across the thickness of slab
- α0, α1 :
-
parameters in Eqs. (20) and (20a)
- β = β T β H :
-
relative hydration rate (Eq. 7)
- K:
-
hygrothermic coefficient (Eq. 4)
- ϱ, ϱ g :
-
specific mass and specific weight of water
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Subscript sat … for saturation, H=1; Primes in r′, t′, H′ refer to non-dimensional variables Eq. (18).
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Bažant, Z.P., Najjar, L.J. Nonlinear water diffusion in nonsaturated concrete. Mat. Constr. 5, 3–20 (1972). https://doi.org/10.1007/BF02479073
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DOI: https://doi.org/10.1007/BF02479073