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Coupled chemo-transport-mechanical modelling and numerical simulation of external sulfate attack in mortar

机译:砂浆中外部硫酸盐侵蚀的化学迁移-力学耦合模型与数值模拟

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摘要

We develop and apply in this study a chemo-transport-mechanical model for simulating the external sulfate attacks in Portland (CEM I) cement pastes and mortars. Basically, this degradation consists in the simultaneous decalcification of the hydrated phases resulting from leaching processes, and the migration of sulfate ions within the material and its subsequent interactions with these phases. The sulfate uptake leads generally to ettringite precipitation mainly from monosulfate, which in turn may produce intense macroscopic expansions and cracking. In our approach, crystallization pressures arising from the restrained growth of monosulfate crystals due to the confinement of the surrounding C-S-H matrix are assumed to initiate the observed macroscopic expansions. A macroscopic strain tensor evaluated from the volume fraction of supplementary precipitated ettringite is further introduced in the mechanical behavior law for explicitly reproducing the macroscopic expansions. Analytical homogenization schemes are applied to estimate both mechanical and diffusive properties from the local volume fraction of solid phases. The numerical platform Alliances is then used for solving both reactive transport and mechanical coupled problems, and is applied to the simulation of laboratory tests consisting in prismatic mortar specimens immersed in solutions containing sodium sulfate and subjected to free expansions. Comparison of the numerical results with experimental ones in terms of phase assemblage profiles, evolutions of mass changes and expansions shows a correct agreement. Finally, the extension of the model towards cases of restrained displacement conditions is discussed and some modifications regarding the kinetics of ettringite precipitation are proposed for such situations.
机译:我们开发并在这项研究中应用化学迁移力学模型来模拟波特兰(CEM I)水泥浆和砂浆中的外部硫酸盐侵蚀。基本上,这种降解包括浸出过程导致水合相同时脱钙,以及材料中硫酸根离子的迁移及其与这些相的后续相互作用。硫酸盐的吸收通常导致钙矾石主要由单硫酸盐沉淀,这反过来可能产生强烈的宏观膨胀和开裂。在我们的方法中,假定由于周围C-S-H基质的限制,由单硫酸盐晶体的生长受限而产生的结晶压力会引发观察到的宏观膨胀。根据补充的沉淀钙矾石的体积分数评估的宏观应变张量进一步引入机械行为定律中,以明确再现宏观膨胀。均质分析方案可用于根据固相的局部体积分数估算机械性能和扩散性能。数值平台Alliances然后用于解决反应性运输和机械耦合问题,并被用于模拟实验室测试,包括将棱柱形砂浆样本浸入含有硫酸钠的溶液中并进行自由膨胀。将数值结果与实验结果进行相组装图,质量变化和膨胀演化的比较显示出正确的一致性。最后,讨论了将模型扩展到约束位移条件下的情况,并针对这种情况提出了关于钙矾石沉淀动力学的一些修改。

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