Abstract
The carbonation is a fundamental durability process for concrete structures exposed to nearly all environments. In air-borne chloride environments, the chloride ingress occurs simultaneously with the carbonation, constituting a multi-phase and multi-species transport-reaction problem. This paper regards concrete as a reactive porous medium partially saturated by pore solution and addresses this problem through a comprehensive transport-reaction model taking into account the dissociation and dissolution–precipitation equilibria in pore solution, transport of gas and aqueous phases and local electrical field. Especially the incongruent dissolution of C–S–H is addressed, a coating-reaction kinetics is assumed for the CH carbonation and new chloride adsorption laws are used upon carbonation of C–S–H. The established model is solved through finite volume method and validated by laboratory experiments of chloride ingress in carbonated OPC concretes. The parametric analysis for concurrent carbonation and chloride ingress under constant relative humidity shows that: (1) the concurrent carbonation will globally promote the chloride ingress and the involved corrosion risk for embedded steel; (2) the significant RH range for this carbonation impact will be on medium levels around 75%; (3) the concretes incorporating SCMs, especially in large quantities, will behave differently to the influence of carbonation. Accordingly, the concurrent carbonation should be considered in appropriate way in durability design against chloride ingress.
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This study was funded by NSFC Grant No. 51778332 and CSC scholarship (201706210326). This work is also a part of Innovandi partner project 31.1.
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Appendices
Appendix A: CH carbonation kinetics
Based on the mechanism described in Fig. 11, the dissolution kinetics of portlandite was derived in [43] as,
where the characteristic time \(\tau_{{{\text{CH}}}}\) is approximated to 720 s for spherical crystals of portlandite with radius of R0 = 40 μm. The geometry factors, rp and rc, are the relative radii of internal and external spheres, i.e. Rp/R0 and Rc/R0, and can be related to the molar quantities as,
The parameter \(c\) was calibrated, as 0.32 × 106, by accelerated carbonation experiment (50% CO2) on hardened cement pastes (HCP) with OPC CEM I as binder and w/c ratio of 0.45. The CH content at the surface of HCP specimens (cylindrical specimens with 4 cm in length and 3.2 cm in diameter) was measured by TGA after 14d of accelerated carbonation.
Appendix B: Supplementary relations for transport properties
2.1 Diffusion coefficients for CO2 and water vapour
The diffusion coefficients \(D_{{{\text{CO}}_{{2}} (G)}}^{e}\) and \(D_{{{\text{va}}(G)}}^{e}\) in (18) and (19) take into account the porosity and tortuosity of pore structure [69],
The term D0CO2,va refer to the specific diffusion coefficients of CO2 and water vapour in air, taking 1.6 × 10−5 m2/s for CO2 and 2.82 × 10−5 m2/s for water vapour under T = 293 K and patm = 101.325 kPa.
For cement-based materials with higher w/c ratios, between 0.5 and 0.8, Papadakis et al. [70] proposed an empirical relation for the effective diffusivity of CO2,
with ϕp standing for the porosity of cement paste in concretes. Both models in (25) and (26) are used in the simulations for CO2 diffusivity respectively for w/c lower and higher than 0.5.
2.2 Permeability
Carbonation will also decrease the intrinsic permeability in (20) by pore precipitation. The intrinsic permeability considers the porosity change through the following relation [71],
with k0int and ϕ0 referring to the initial values for intrinsic permeability and porosity. The relative permeability coefficient of liquid \(k_{rl}\) is also derived from van Genuchten’s model [54], taking the following form,
with the parameter b taking the same value as in (6). The dynamic viscosity of liquid water is retained for the pore solution, taking ηl = 0.1 Pas for T = 293 K.
2.3 Ionic diffusion coefficient
The ionic diffusivity model from Yokozeki et al. [72] is retained in the simulations, taking the following form,
From the right side to left side, D0i represents the diffusivity of ion i in pure water (dilute solution), e.g. 2.032 × 10–9 m2/s for Cl− in water under 25 °C. The function sLλ scales the pore saturation effect on the diffusivity, and the exponent λ takes 6.0 following Nguyen [45] for cement-based materials. The function f(ϕp) represents the effect of pore structure on the diffusivity, taking the following expression based on percolation theory [73],
with ϕp for capillary porosity of cement paste in concrete. So far, the diffusivity is scaled from pore solution to cement pastes. Then, the term vp refers to the volumetric fraction of cement paste in concrete, and the last term describes the tortuosity effect provided by the fine and coarse aggregates: vfa and vca refer to the volumetric fractions of fine and coarse aggregates, and c = 2.1, d = 0.65 for two tortuosity parameters.
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Xie, M., Dangla, P. & Li, K. Reactive transport modelling of concurrent chloride ingress and carbonation in concrete. Mater Struct 54, 177 (2021). https://doi.org/10.1617/s11527-021-01769-9
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DOI: https://doi.org/10.1617/s11527-021-01769-9