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Alkali-Silica Reaction in concrete numerical modelling: an engineering approach *Andrzej Winnicki 1) and Szymon Seręga 2) 1), 2) Faculty of Civil Engineering, Cracow University of Technology, ul. Warszawska 24, 31-155 Kraków, Poland 1) [email protected] 2) [email protected] ABSTRACT Paper presents chemomechanical model of alkali-silica reaction (ASR) for concrete. Two models of first order kinetics are presented in depth and authors’ own modifications of them pertinent to dependence on variable temperature and humidity are discussed. Then, for the known reaction extent (scalar variable) a numerical algorithm developed by authors in order to solve chemomechanical problems is presented. The main advantage of the proposed algorithm lies in that there is no need to build special FEM code in order to solve the problem instead commercially available codes can be used. Performed exemplary numerical computations for a gravity dam show that the proposed approach renders quite well actual behaviour of an ASR affected structure. 1. INTRODUCTION Alkali-silica reaction (ASR) in concrete is nowadays a recognized cause of the progressive deterioration and damage in many plain and reinforced concrete structures (Hobbs 1988). The examples of damage caused by ASR are presented in Fig.1 and Fig.2. The reaction was for the first time noted in 1940 by Stanton who studied causes of cracking of RC structures in California (Hobbs 1988). He suggested chemical reaction taking place between alkalis in cement Na 2 O, K 2 O and silica SiO 2 in aggregate in presence of water as a cause of concrete deterioration. From that time chemistry of ASR has been studied by numerous researchers, e.g. Dent Glaser (1981), Garcia-Diaz (2006), Wang (1991). The classical explanation of the reaction is given by Wang (1991). Usually, it is assumed that ASR is at least two-stage process: - Hydroxyl ions OH in pore solution attack siloxane groups Si-O in aggregate (as in ordered lattice each atom of silicon is linked by four siloxane bridges this stage of reaction is slow and takes place only on the surface of aggregate grains being of 1) Professor 2) PhD Keynote Paper

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Page 1: Alkali-Silica Reaction in concrete numerical modelling: an … › publication_conf › asem17 › 0.Keynote › XH1B.k030… · Keynote Paper . topochemical nature) creating silanol

Alkali-Silica Reaction in concrete – numerical modelling:

an engineering approach

*Andrzej Winnicki1) and Szymon Seręga2)

1), 2) Faculty of Civil Engineering, Cracow University of Technology, ul. Warszawska 24,

31-155 Kraków, Poland 1)

[email protected] 2)

[email protected]

ABSTRACT

Paper presents chemomechanical model of alkali-silica reaction (ASR) for concrete. Two models of first order kinetics are presented in depth and authors’ own modifications of them pertinent to dependence on variable temperature and humidity are discussed. Then, for the known reaction extent (scalar variable) a numerical algorithm developed by authors in order to solve chemomechanical problems is presented. The main advantage of the proposed algorithm lies in that there is no need to build special FEM code in order to solve the problem – instead commercially available codes can be used. Performed exemplary numerical computations for a gravity dam show that the proposed approach renders quite well actual behaviour of an ASR affected structure. 1. INTRODUCTION Alkali-silica reaction (ASR) in concrete is nowadays a recognized cause of the progressive deterioration and damage in many plain and reinforced concrete structures (Hobbs 1988). The examples of damage caused by ASR are presented in Fig.1 and Fig.2. The reaction was for the first time noted in 1940 by Stanton who studied causes of cracking of RC structures in California (Hobbs 1988). He suggested chemical reaction taking place between alkalis in cement Na2O, K2O and silica SiO2 in aggregate in presence of water as a cause of concrete deterioration. From that time chemistry of ASR has been studied by numerous researchers, e.g. Dent Glaser (1981), Garcia-Diaz (2006), Wang (1991). The classical explanation of the reaction is given by Wang (1991). Usually, it is assumed that ASR is at least two-stage process: - Hydroxyl ions OH– in pore solution attack siloxane groups Si-O in aggregate (as in

ordered lattice each atom of silicon is linked by four siloxane bridges this stage of reaction is slow and takes place only on the surface of aggregate grains being of

1)

Professor 2)

PhD

Keynote Paper

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topochemical nature) creating silanol bridges instead of siloxane ones. - Dissolution of silica (as a result of continuous attack of hydroxyl ions) leads to

formation of silica ions; sodium and potassium cations also penetrates in pore solution. As a result a polyelectrolite is created which, in contact with water, sets up imbibition pressure and produces ASR gel.

The modern, modified model of ASR reaction proposed by Ichikawa (2007) is shown in Fig. 3.

Fig.1 Chambon Dam (France) built in 1934 (https://structurae.net/structures/chambon-dam)

Fig.2 Concrete pavement (AASHTO)

Fig.3 Modified model of ASR by Ichikawa (2007)

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The commonly accepted fact is that the amorphous gel located either in material pores or on the surface of aggregate grains is the final product of ASR. The gel is highly hydrophilic, imbibes large amounts of water and swells considerably leading to local internal cracking and volumetric expansion of concrete. In general gel is composed of alkali-silica hydrate N(K)-S-H (Na2(K2)O-SiO2-H2O) and/or calcium alkali-silica hydrate C-N(K)-S-H (CaO-Na2(K2)O-SiO2-H2O). The detailed composition of these end-member phases is an object of still ongoing debate. For example the exemplary stoichiometric ratios as reported by Dent Glaser (1981) are:

2 2 2 21.47Ca O? a O? .40SiO ? 2.57H O . Other possible stoichiometric ratios (without imbibed water) are presented in Fig. 4.

Fig.4 Exemplary stoichiometric ratios: 1) Dent Glaser (1981), 2) Moon (2013), 3) Kawamura (2004)

Many experimental and some theoretical works (based among others on molecular dynamics) are devoted to composition, water imbibition and swelling properties of the gel, e.g. Kirkpatrick (2005), Struble (1981). In the last two decades much effort was put into chemomechanical aspects of ASR and their influence on the behaviour of existing structures. This effort resulted in development of many phenomenological chemomechanical models describing the behaviour of concrete subjected to action of ASR dependent on both temperature and humidity – see for example Pietruszczak (1996), Poyet (2003), Ulm (2000), Winnicki (2008). It is generally accepted that key factors influencing the reaction development are: temperature, relative humidity, compressive stress level and concentration of reactive aggregate (pessimum effect) – Larive (1998), Poyet (2003), Hobbs (1988). Those factors are shown schematically in Fig. 5.

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Fig. 5 Key factors governing ASR development (Léger 1996) A well-known feature of ASR is a prolonged time of its development lasting even twenty to thirty years. Usually there is a latency period (up to three - four years) directly after construction in which there is no signs of ongoing ASR. The commonly observed results of ASR are swelling and local cracking of mass concrete leading to deterioration of strength and elastic properties. The quantitative assessment of strength and elastic properties deterioration is still a subject of controversy (Larive 1998, Hobbs 1988, Giaccio 2008, Ben Haha 2006). 2. ASR KINETICS 2.1 Existing models

The standard way of describing kinetics of ASR used in chemomechanics is to introduce nondimensional variable called reaction extent which describes progress of the reaction and changes in its course from zero to one (Pietruszczak 1996, Ulm 2000). In the case of the ASR which is characterized by the increase of the volume of the material (swelling) reaction extent can be linked to chemical strain caused by ASR using the equation:

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( )

, , 0 1ASR

ASR

tt t t

(1)

where ( )t - concrete expansion at time t,

ASR - maximal linear concrete expansion.

In such a way internal variable is associated with concrete expansion which is an observable and measurable quantity. Kinetics of the reaction is governed by the equation:

m d

dA k

dt

(2)

where mA is a change in the molar concentration of reactants or chemical affinity,

dk is a reaction parameter. In the course of the reaction variable mA decreases from the initial value

00m mA A at which reaction starts to end value 1 0mA when reaction stops. Order of the reaction kinetics is determined by relation of the function mA to variable . For the kinetics of the first order the linear relation is assumed which leads to the relationship which was introduced for ASR firstly by Hobbs (1988) and subsequently used by Pietruszczak (1996):

01 c

dt for

d

(3)

where tc = kd/Am0 is an internal time parameter responsible for reaction rate and 0 is delay time (time needed to start forming the gel pressure). For 0 gel is produced and fills pores of the material but does not exert pressure therefore is assumed that remains equal to zero for that time period (latency period). Kinetics of the reaction depends strongly on both relative humidity and temperature (Hobbs 1998, Larive 1998, Poyet 2003). This phenomenon is taken into account by the rate relation linking real physical time with time parameter of reaction (as used in Eq. (3)):

1 2d f T f RH dt (4)

Exemplary forms of functions 1( )f T , 2( )f RH are given as:

1

0

1 1expf T U

T T

(5)

2100

mRH

f RH

(6)

where U is thermal activation constant and T0 means the reference temperature. The first function is Arrhenius law, the latter one is taken according to Capra (1998).

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For the constant temperature and relative humidity values Eq. (3) can be integrated and presented in the closed form:

0

0 0

1 exp

0

c

for

t for

(7)

It can be seen that the assumption that the kinetics is of the first order leads to the exponential development of the reaction in time domain – see Fig. 6a. Such a description does not match the experimental results closely enough, therefore the modified form of the first order kinetics equation has been introduced by Larive (1998), then subsequently used by Ulm (2000):

1 c

dt

dt

(8)

In this approach, contrary to Eq. (3), the latency period does not appear in the explicit form. ASR takes place starting from the very beginning for time 0 . In Eq. (8) tc is not any longer reaction parameter but additional variable changing in ASR course according to relation:

1 exp( / )

exp( / )lat ch

c ch

lat ch

t

(9)

where lat - latency time (equivalent of delay time 0 in Eq. (3)), ch - characteristic time which governs the reaction rate. Again it is possible to get closed form solution of Eq. (8):

1 exp ( )

,1 exp ( ) ( )

ch

lat ch

t Tt T

t T T

(10)

for the case of constant temperature and humidity (when lat and ch remain constant) – see Fig. 6b. In the original work by Larive (1998) only dependence of lat and ch on temperature was taken into account in the form:

0

0

1 1exp lat lat latT T U

T T

(11)

0

0

1 1expch ch chT T U

T T

(12)

where Ulat and Uch are the thermal activation constants for lat and ch , respectively.

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2.2. Parametrical modifications The experimental data (Larive 1998, Poyet 2003) point out clearly that not only rate of ASR but also latency period depends strongly on both the temperature and relative humidity. Therefore authors proposed the modified description of the model parameters. For Hobbs (1988) and Pietruszczak (1996) model (Eq. (3)) the following functions were introduced for latency time:

30 40 , ( ) ( )T RH f T f RH (13)

where

3 0

0

1 1( ) exp f T U

T T

(14)

4 ( )

100

nRH

f RH

(15)

and 0U is thermal activation constant. For Larive (1998) approach (Eq. (8)) the formulae for latency and characteristic times take forms:

0 5

0

1 1, exp ( )lat lat latT RH T U f RH

T T

(16)

0 6

0

1 1, exp ( )ch ch chT RH T U f RH

T T

(17)

where

,

5,6( )100

k lRH

f RH

(18)

As can be seen in the above equations additional new parameters n, k, l, U0 are introduced. Authors developed procedure for calibrating values of all (original and newly introduced) parameters for given experimental data using the least square method. 2.3. Comparison with experiments The above presented theoretical formulation is compared with experimental data provided in Larive (1998) and Poyet (2003). In the comparison it is assumed that for experimental data the reaction extent can be computed directly from actual concrete expansion according to Eq. (1).

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Fig. 6a presents the development of the reaction for different temperatures using Hobbs (1988) and Pietruszczak (1996) model in comparison with experimental data of Larive (1998). The same set of experimental data is presented in Fig. 6b, this time, compared to numerical prediction according to Larive (1998) model. a) b)

Fig. 6 ASR development for different temperatures according to: a) Hobbs (1988) and Pietruszczak (1996) model, b) Larive (1998) model – all experimental data by Larive

(1998) a) b)

Fig. 7 ASR development for different RH levels according to: a) Hobbs (1988) and Pietruszczak (1996) model, b) Larive (1998) model – all experimental data by Poyet

(2003) Fig. 7a and Fig. 7b show numerical simulations of ASR development as predicted by Hobbs (1988) and Pietruszczak (1996) model and Larive (1998) model for different relative humidity levels (experimental data from Poyet (2003)). In the Fig. 6 and Fig. 7 the numerical predictions are shown for different but constant in time domain values of temperatures and relative humidity. Poyet (2003) performed also experiments for different relative humidity levels changing periodically in time domain. In those tests relative humidity was changed from value 59% to 96% and then back in two types of cycles: a short one equal to 14 days and a long one equal to 28 days. Fig. 8a presents numerical prediction for short cycles whereas Fig. 8b presents numerical prediction for long cycles (Larive (1998) model).

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It has to be noted that in experiments concrete expansion was partially reversible at the end of the given cycle. This phenomenon can be explained by partial drying of the specimen when relative humidity goes down. In order to account for this phenomenon in theoretical model additional instantaneous drying strains (which are linear function of RH level) were added by authors. a) b)

Fig. 8 ASR development for RH changing in: a) short cycles, b) long cycles according to Larive (1998) model (experimental data by Poyet (2003))

In the available literature there is lack of experimental data pertinent to temperature changing periodically in time domain. Authors made computations for five different temperature histories changing periodically in time domain (Fig. 9), namely for the sinusoidal change in one year period with average temperature 12ºC and amplitude 12ºC (case 1), stepwise approximation between 0ºC and 24ºC (case 2), constant temperature equal to 24ºC (case 3), real monthly temperatures as recorded in Toruń, Poland (case 4) and additionally constant temperature equal to 12ºC (case 5). a) b)

Fig. 9 Assumed temperature changes: a) cases 1 and 2, b) cases 3 and 4 For all cases numerical predictions were performed using Hobbs (1988) and Pietruszczak (1996) model and Larive (1998) model (Fig. 10). Taking as a reference development of the reaction for the real temperature change as recorded on the spot (case 4) it is seen that for both models these results are fairly well approximated by the

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numerical simulation for the constant temperature equal to 12ºC (case 5). This means that for the analysis of the ASR effects in long time scale it is not necessary to recreate in the exact way temperature change in year period – instead of that an average temperature can be used. a) b)

Fig. 10 Reaction development in time domain for temperature changes according to case 1 to 5 using: a) Hobbs (1988) and Pietruszczak (1996) model, b) Larive (1998)

model 3. CHEMOPLASTIC MODEL The above presented description of the reaction kinetics has to be included in the constitutive relationships for concrete. Two phenomena should be taken into account: at first free chemomechanical strain as described by Eq. (1) according to formula:

( ) ( )ASR ASR t ε I I (19)

where I is an identity tensor of the second rank, secondly deterioration of the strength and stiffness has to be described as an appropriate functions of reaction extent . Assuming small strains the total strains are the sum of the elastic, chemical, thermal and plastic terms in the form:

el ASR T pl ε ε (20)

Chemical strains are described by Eq. (19) which locates this model in the category of isotropic models. Yield function is given by the formula:

, , 0plF σ ε (21)

In this formulation mechanical hardening/softening is described as a function of the total plastic strains (based on their invariants) whereas the dependence of yield function on the reaction extent enable us to describe chemical softening. In such a way deterioration of both compressive and tensile strengths of concrete in the course of

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ASR development is taken into account. Consistency condition (Prager’s condition) in this case has a form:

: : 0,pl

pl

F F F

n nσ εε σ

(22)

The last term on the left hand side differs this approach from the classical rate independent plasticity introducing change of the yield function in time domain even for constant loading (similarly to the viscoplastic models). Additionally it is assumed that the elastic stiffness operator D is also the function of the reaction extent:

D D (23)

A direction of plastic strain rate is defined in the standard form as being normal to the plastic potential Q in the stress space:

,pl

Q

m mε

σ (24)

where is a plastic multiplier to be determined from the consistency conditions – Eq. (22). Using the standard procedure of the derivation of elastoplastic tangent continuum operator the final form of the chemoplastic rate relationship can be presented as:

: Tep ASR T

T

D

εσ ε Γ (25)

where Dep is the classical tangent continuum elastoplastic operator

1

: :: :

epH

D D D m n Dn D m

(26)

with the generalized plastic modulus given as:

:pl

FH

(27)

Operator ΓASR describes additional strains caused by chemical expansion of concrete (first term), change of the elastic stiffness operator due to the reaction extent (second term) and chemical softening of yield function (third term) in the form:

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1 1

:ASRASR

F

H

Dm

εΓ σ (28)

Details of this formulation can be found in Winnicki (2008). 4. CREEP INFLUENCE

ASR takes place over the long period of time, therefore the chemomechanical analysis of ASR should also take into account the creep effects. Among many creep models Model Code 2010 (MC2010) approach can be followed. In the creep model it is necessary to include ASR influence assuming that the concrete Young modulus is a

function of current value of reaction extent . In such a way coupling between ASR (causing deterioration of stiffness) and creep is introduced as:

0 0

1 ( , )( , , )

( ) ( 0.0)

tJ t

E E

(29)

where E0 is concrete elastic modulus, is a creep coefficient taken according to MC2010. In Fig. 11a the exemplary creep functions for different times of loading and reaction extent 0.0 are presented neglecting drying part of creep (it is reasonably to assume that for large structures undergoing ASR the relative humidity level is large enough in order not to produce drying creep strains). For numerical computations using FEM it is convenient to approximate the creep function J in the form of truncated Dirichlet series. This simplified form of creep function can be interpreted as Kelvin chain model:

10

1 1( , , ) 1

( ) ( )i

tn

i i

J t eE E

(30)

where Ei are the stiffness of the individual springs in Kelvin chain and i are retardation times. It appears that in order to approximate MC2010 analytical formulae reasonably well, it is enough to take only three terms of the series. The fitting procedure was performed for no ASR influence (i.e. 0.0 ). The values of the spring stiffness and retardation times adopted are shown in Fig. 11b. Numerical examples at the material point level were done using both the exact

analytical formulation of MC2010 (coded in Mathcad) and Kelvin chain model (available in DIANA code) with the extent parameter being defined in time domain as the input value. Fig. 12 shows two analyzed loading scenarios and the reaction course in time. The first loading scenario is periodically constant load in time whereas the second one is described by the sine function. In both cases the extent parameter increases continually in time domain from zero to one. The given examples show clearly that numerical approximation in the form of finite Kelvin chain renders MC2010 approach in a very good way – see Fig. 13.

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a) b)

Fig. 11 a) example of creep functions for concrete in analyzed dam, b) materials parameters for Kelvin chain model

a) b)

Fig. 12 Loading scenarios and reaction course in time a) b)

Fig. 13 Calculated strains for creep functions according to Eq. (29) and Eq. (30)

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5. NUMERICAL IMPLEMENTATION For the practical engineering computations of the large structures instead of the chemoplastic model presented in Section 3 much simpler chemomechanical model is used based on the smeared crack approach in the form of multidirectional fixed crack model as implemented in DIANA FEM code (Manie 2010, de Borst 1987). In this model the regularization of obtained numerical results after cracking is provided by keeping the constant fracture energy value for a given area of a cracked element (“fracture energy trick” - de Borst (1987)). In the performed computations chemical strains are taken into account using Eq. (19) and, in addition, tensile strength and fracture energy of concrete are functions of the reaction extent in the simplest linear form. In such a chemomechanical formulation both concrete extension and reaction

extent are treated as input variables. Therefore for a given boundary conditions problem in time domain the reaction extent has to be computed as a scalar variable over the given area for every time instant. In turn the reaction extent depends strongly on temperature and relative humidity fields. In the algorithm proposed by authors at first temperature and relative humidity fields for the whole structure are computed in time domain solving Fourier-Kirchhoff equation for temperature and moisture transport equation given by Xi (1994a). For the Fourier-Kirchhoff equation the constant thermal capacity and conductivity coefficients are assumed. For the moisture transport equation both moisture capacity and diffusion coefficient are taken as functions of relative humidity according to Xi (1994b). These computations are performed using standard transport models of DIANA code (Manie 2010). Having temperature and relative humidity values computed for the whole structure in time domain the reaction extent and concrete expansion are calculated according to the formulae presented in Section 2 and then used as an input values for mechanical analysis being performed again in DIANA code. The presented algorithm is summarised in Fig. 14a and Fig. 14b.

Fig. 14a Computational algorithm – temperature and relative humidity calculations

Thermal

analysis

Material prop.

p

c

c

c const

const

const

( , 0)initT T t x

( , )b b bT T t x

( , )T tx

( )

( )

( )

h h

w

D D RH

w w RH

dwc

d RH

Calculation of

reaction extent ξ

Initial condt.

Boundary condt.

RH

analysis

Material prop.

( , )RH tx

Initial condt.

Boundary condt.

1.0initRH

( , )b b bRH RH t x

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Fig. 14b Computational algorithm – computation of reaction extent and mechanical analysis

6. CASE STUDY – FONTANA DAM As a numerical example Fontana gravity dam was chosen following the numerical analysis made by Comi (2009). Fontana dam is located in Graham County, North Carolina USA and its construction was finished in 1946. Three years after the end of completing (1949) for first time a pattern of cracking was observed together with an upstream movement of the structure. Later inspections (1972) found large cracks inside the dam. According to the information provided by Comi (2009) petrographic examination made in 1999 revealed the presence of ASR. The analyzed cross-section of the dam together with the subsoil is presented in Fig. 15 also showing assumed FE mesh. The applied initial conditions together with the imposed changes of thermal, hygral and mechanical boundary conditions in a year period are presented in Fig. 15 to Fig. 17. Presented analysis of the Fontana dam comprises two parts. The first one is pertinent to the normal exploitation state of the dam within time period of 30 years, the second one concerns the catastrophic situation in which the overtopping load till the failure of the dam is analyzed. Following the numerical algorithm outlined above first the relative humidity and temperature fields were computed. Fig. 18a and Fig. 18b show the computed fields of relative humidity and temperature after 30 years in summer, respectively. On the basis of known humidity and temperature fields the reaction extent in time domain for the whole structure was computed. The kinetics of ASR was described by Larive (1998) model modified by authors (see Section 2). Assumed ASR parameters for concrete are given in Table 1. Fig. 19 shows development of the reaction extent in time domain for a few selected points in the body of the dam (the location of chosen points is given in Fig. 15). In turn Fig. 20 presents the reaction extent for different time instants,

,lat chU U

( , )RH tx

( , )t x

( , )lat T RH

,k l

( , )ch T RH

Calculation of

reaction extent ξ

Temperature field

RH field

( , )T tx

Material prop.

Mechanical

analysis( , )t x

Material properties

0( ) (1 (1 ) )EE E B

0( )

0( ) (1 (1 ) )t t ff f B

0( ) (1 (1 ) )F F GG G B

Isotropic field of

ASR strain

ASR ASR I

DIANA

Mechanical fields

( , )tu u x

( , )t x

( , )t x

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of which the last one corresponds to above presented relative humidity and temperature fields. As mentioned in Section 5 for the description of concrete behaviour in tension the multidirectional fixed crack model was chosen together with linear softening in the post-critical range. The creep of concrete was modelled following the approximation of MC2010 creep function as described in Section 4. ASR dependent mechanical properties of concrete are given in Table 2.

Fig. 15 Cross section of Fontana dam together with foundation on subsoil Table 1 ASR parameters for concrete

Latency, characteristic times [day] τlat = 246 τch = 136 Thermal activation constants [K] Ulat = 9400 Uch = 5400 Reference temperature [K] T0 = 311.5 RH constants [-] k = -3.5 l = 1.0

Table 2 Mechanical properties of concrete

ξ = 0.0 ξ = 1.0

E [MPa] 22000 11000 ν 0.2 0.2 fct [MPa] 2.10 1.05 Gf [N/m] 135 67.5

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a) b)

Fig. 16 a) thermal boundary conditions (one year period), b) hygral boundary conditions (one year period)

Fig. 17 Mechanical boundary conditions (one year period)

a) b)

Fig. 18 a) relative humidity field in dam (30 years, summer), b) temperature field in dam (30 years, summer) [ºC]

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Fig. 19 Development of reaction extent in time domain

a) b) c)

Fig. 20 Reaction extent fields in dam: after 7, 14 and 30 years, respectively

In Fig. 21 the crack patterns after 30 years of ASR action are shown for the cases with and without creep effects, respectively. It can be concluded from this figure that creep effects result in reducing the cracked area mainly in the middle part of the dam. For a selected point at the crown of the dam the histories of the displacements are shown in Fig. 22. It follows from this figure that after 30 years of ASR influence displacements are eventually stabilized. It can be also observed that the influence of creep on displacements is negligibly small.

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a) b)

Fig. 21 Crack pattern after 30 years, 0.075%ASR : a) without creep, b) with creep (note that closed cracks are also shown)

a) b)

Fig. 22 Displacements of the crown of dam: a) horizontal, b) vertical As a next case the overtopping load till the failure of the dam applied to the structure after 30 years of ASR action together with creep is analyzed. Fig. 23 shows the overtopping ratio versus horizontal displacement of the crown (overtopping ratio is defined as Hwave/Hdam, where Hwave is the height of water level during flood, Hdam means the height of a dam). This overtopping ratio can be considered as the global safety factor for the dam structure. The ratio Hwave/Hdam calculated after 30 years of ASR action is approximately equal to 2.1. In Fig. 23 Hwave/Hdam values are also plotted for dam not affected by ASR. It turns out that in this case the overtopping ratio is less than for dam affected by ASR. This controversial observation can be explained by the fact

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that ASR strains introduce compressive stresses at the upstream side of the dam, at the critical section located above the inspection gallery. From Fig. 23 it follows that ASR affected dam behaves in the softer way (in the sense of the maximum load displacement curve) than ASR-free dam. This behavior is caused by the amount of accumulated cracks due to ASR.

Fig. 23 Overtopping ratio versus horizontal displacement

Comparing the above presented results with previously published results concerning a case without creep effects (Winnicki 2014, Winnicki 2015) it can be stated that influence of creep on the overtopping ratio is negligibly small. 7. CONCLUSIONS The presented paper is a summary of a continuous, long-run research project devoted to the numerical modelling of ASR mechanical effects in concrete. Parts of the presented materials were previously published by Winnicki (2014), Winnicki (2015), Seręga (2015). In the paper the most commonly used models of ASR kinetics are presented. The dependence of ASR kinetics on humidity and temperature is discussed in depth and authors’ own improvements are presented. The proposed improved model of ASR kinetics matches well the experimental results for wide range of temperature and humidity including also temperature and humidity histories which change in time domain. In the paper the chemoplastic mechanical model is presented, however for the practical engineering computations the simpler approach is devised based on available commercial software (DIANA) using the smeared crack approach existing in the code. A creep phenomenon is additionally taken into account using approach based on truncated Kelvin chain rendering very well the MC2010 creep function. The proposed approach is fully decoupled – at first temperature and relative humidity fields are computed independently, on their basis reaction extent is calculated for whole structure in time domain. Using those results in final stage mechanical problem is solved.

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