Creep and shrinkage of concrete are two physical properties of concrete. The creep of concrete, which originates from the calcium silicate hydrates (C-S-H) in the hardened Portland cement paste (which is the binder of mineral aggregates), is fundamentally different from the creep of metals and polymers. Unlike the creep of metals, it occurs at all stress levels and, within the service stress range, is linearly dependent on the stress if the pore water content is constant. Unlike the creep of polymers and metals, it exhibits multi-months aging, caused by chemical hardening due to hydration which stiffens the microstructure, and multi-year aging, caused by long-term relaxation of self-equilibrated micro-stresses in the nano-porous microstructure of the C-S-H. If concrete is fully dried, it does not creep, but it is next to impossible to dry concrete fully without severe cracking.
Changes of pore water content due to drying or wetting processes cause significant volume changes of concrete in load-free specimens. They are called the shrinkage (typically causing strains between 0.0002 and 0.0005, and in low strength concretes even 0.0012) or swelling (< 0.00005 in normal concretes, < 0.00020 in high strength concretes). To separate shrinkage from creep, the compliance function
J(t,t')
\epsilon
\sigma=1
t'
The multi-year creep evolves logarithmically in time (with no final asymptotic value), and over the typical structural lifetimes it may attain values 3 to 6 times larger than the initial elastic strain. When a deformation is suddenly imposed and held constant, creep causes relaxation of critically produced elastic stress. After unloading, creep recovery takes place, but it is partial, because of aging.
In practice, creep during drying is inseparable from shrinkage. The rate of creep increases with the rate of change of pore humidity (i.e., relative vapor pressure in the pores). For small specimen thickness, the creep during drying greatly exceeds the sum of the drying shrinkage at no load and the creep of a loaded sealed specimen (Fig. 1 bottom). The difference, called the drying creep or Pickett effect (or stress-induced shrinkage), represents a hygro-mechanical coupling between strain and pore humidity changes.
Drying shrinkage at high humidities (Fig. 1 top and middle) is caused mainly by compressive stresses in the solid microstructure which balance the increase in capillary tension and surface tension on the pore walls. At low pore humidities (<75%), shrinkage is caused by a decrease of the disjoining pressure across nano-pores less than about 3 nm thick, filled by adsorbed water.
The chemical processes of Portland cement hydration lead to another type of shrinkage, called the autogeneous shrinkage, which is observed in sealed specimens, i.e., at no moisture loss. It is caused partly by chemical volume changes, but mainly by self-desiccation due to loss of water consumed by the hydration reaction. It amounts to only about 5% of the drying shrinkage in normal concretes, which self-desiccate to about 97% pore humidity. But it can equal the drying shrinkage in modern high-strength concretes with very low water-cement ratios, which may self-desiccate to as low as 75% humidity.
The creep originates in the calcium silicate hydrates (C-S-H) of hardened Portland cement paste. It is caused by slips due to bond ruptures, with bond restorations at adjacent sites. The C-S-H is strongly hydrophilic, and has a colloidal microstructure disordered from a few nanometers up. The paste has a porosity of about 0.4 to 0.55 and an enormous specific surface area, roughly 500 m2/cm3. Its main component is the tri-calcium silicate hydrate gel (3 CaO · 2 SiO3 · 3 H2O, in short C3S2H3). The gel forms particles of colloidal dimensions, weakly bound by van der Waals forces.
The physical mechanism and modeling are still being debated. The constitutive material model in the equations that follow is not the only one available but has at present the strongest theoretical foundation and fits best the full range of available test data.
In service, the stresses in structures are < 50% of concrete strength, in which case the stress–strain relation is linear, except for corrections due to microcracking when the pore humidity changes. The creep may thus be characterized by the compliance function
J(t,t')
t'
t-t'
J
t-t'
t
t'
\sigma(t)
d\sigma(t')
t'
d\epsilon(t)=J(t,t')d\sigma(t')
Here
\epsilon0
\epsilonsh
\sigma(t)
d\sigma(t')= [d\sigma(t')/dt']dt'
\epsilon(t)
\sigma(t)
J(t,t')
\sigma(t)
\epsilon=1
\hat{t}
\epsilon0=0
R(t,\hat{t})
To generalize Eq. (1) to a triaxial stress–strain relation, one may assume the material to be isotropic, with an approximately constant creep Poisson ratio,
\nu ≈ 0.18
J(t,t')
At high stress, the creep law appears to be nonlinear (Fig. 2) but Eq. (1) remains applicable if the inelastic strain due to cracking with its time-dependent growth is included in
\epsilon0(t)
\epsilon0(t)
fc'
E
t'
J(t,t')
t-t'
E(t')=1/J(t'+\delta,t')
\delta
\delta ≈ 0.01
t'=28
E
E
t'
E=57,000psi
\sqrt{f'c/psi
(1psi=6895Pa,fc'=uniaxialcompressivestrengthofconcrete)
q1=J(t',t')=\lim\deltaJ(t'+\delta,t')
q1
J(t,t')
For creep at constant total water content, called the basic creep, a realistic rate form of the uniaxial compliance function (the thick curves in Fig. 1 bottom) was derived from the solidification theory:
where
x |
=\partialx/\partialt
ηf
\theta
λ0
m=0.5
n=0.1
v(t)\rmMPa-1
q2,q3,q4
\rmMPa-1
Cg(\theta)
Cg(\theta)=
n] | |
ln[1+(\theta/λ | |
0) |
J(t, |
t')
J(t,t')
J(t,t')
J(t,t')
J(t, |
t')
Equations (3) and (4) are the simplest formulae satisfying three requirements: 1) Asymptotically for both short and long times
\theta
J(t, |
t')
{\rmdv-1(t)/dt}
\partial2J(t,t')/\partialt\partialt'>0
At variable mass
w
S
A crucial property is that the microprestress is not appreciably affected by the applied load (since pore water is much more compressible than the solid skeleton and behaves like a soft spring coupled in parallel with a stiff framework). The microprestress relaxes in time and its evolution at each point of a concrete structure may be solved from the differential equation
where
c0,c1
S
w
h
The concept of microprestress is also needed to explain the stiffening due to aging. One physical cause of aging is that the hydration products gradually fill the pores of hardened cement paste, as reflected in function
v(t)
t'
At variable environment, time
t
te=\int\betah\betaTdt
\betah
h
h<
\betah\propto
-QhT/R | |
e |
(Qh/R ≈ 2700K)
\theta =t-t'
tr-t'r
tr=\int\psih\psiTdt
h
T
\psih
h
h=1
h=0
\psiT\propto
-QvT/R | |
e |
Qv/R ≈
The evolution of humidity profiles
h(x,t)
x
\rm
h |
=
hs(te)
C(h)
h
where
ksh
\epsilon |
sh
For finite element structural analysis in time steps, it is advantageous to convert the constitutive law to a rate-type form. This may be achieved by approximating
Cg(\theta)
Conversion to a rate-type form is also necessary for introducing the effect of variable temperature, which affects (according to the Arrhenius law) both the Kelvin chain viscosities and the rate of hydration, as captured by
te
Although multidimensional finite element calculations of creep and moisturediffusion are nowadays feasible, simplified one-dimensional analysis of concrete beams or girders based on the assumption of planar cross sections remaining planar still reigns in practice. Although (in box girder bridges) it involves deflection errors of the order of 30%. In that approach, one needs as input the average cross-sectional compliance function
\barJ(t,t',t0)
\bar\epsilonsh(t,t0)
t0
he
where
D=2v/s
v/s
kt
ks
\epsilonshinfty ≈ \epsilonsinftyE(607)/(E(t0+\taush)
\epsilonsinfty
E(t) ≈ E(28)\sqrt{4+0.85t}
1/ηf
where
F(t)=\exp\{-8[1-(1-he)S(t)]\}
t'0=max(t',t0)
\taush
\bar\epsilonsh\propto\sqrt{t-t0}
Empirical formulae have been developed for predicting the parameter values in the foregoing equations on the basis of concrete strength and some parameters of the concrete mix. However, they are very crude, leading to prediction errors with the coefficients of variation of about 23% for creep and 34% for drying shrinkage. These high uncertainties can be drastically reduced by updating certain coefficients of the formulae according to short-time creep and shrinkage tests of the given concrete. For shrinkage, however, the weight loss of the drying test specimens must also be measured (or else the problem of updating
\epsilonshinfty
The foregoing form of functions
J(t,t')
\epsilonsh(t)
Creep and shrinkage can cause a major loss of prestress. Underestimation of multi-decade creep has caused excessive deflections, often with cracking, in many of large-span prestressed segmentally erected box girder bridges (over 60 cases documented). Creep may cause excessive stress and cracking in cable-stayed or arch bridges, and roof shells. Non-uniformity of creep and shrinkage, caused by differences in the histories of pore humidity and temperature, age and concrete type in various parts of a structures may lead to cracking. So may interactions with masonry or with steel parts, as in cable-stayed bridges and composite steel-concrete girders. Differences in column shortenings are of particular concern for very tall buildings. In slender structures, creep may cause collapse due to long-time instability.
The creep effects are particularly important for prestressed concrete structures (because of their slenderness and high flexibility), and are paramount in safety analysis of nuclear reactor containments and vessels. At high temperature exposure, as in fire or postulated nuclear reactor accidents, creep is very large and plays a major role.
In preliminary design of structures, simplified calculations may conveniently use the dimensionless creep coefficient
\varphi(t,t')=E(t')J(t,t')-1
\epsiloncreep/\epsiloninitial
t1
t
E
E''(t,t1)=[E(t1)-R(t,t1)]/\varphi(t,t1)
The best approach to computer creep analysis of sensitive structures is to convert the creep law to an incremental elastic stress–strain relation with an eigenstrain. Eq. (1) can be used but in that form the variations of humidity and temperature with time cannot be introduced and the need to store the entire stress history for each finite element is cumbersome. It is better to convert Eq. (1) to a set of differential equations based on the Kelvin chain rheologic model. To this end, the creep properties in each sufficiently small time step may be considered as non-aging, in which case a continuous spectrum of retardation moduli of Kelvin chain may be obtained from
J(t,t')
Ek(t)
k=1,2,...nE