Dissolution kinetics of C-S-H gel: Flow-through experiments

被引:53
作者
Trapote-Barreira, Ana [1 ]
Cama, Jordi [1 ]
Soler, Josep M. [1 ]
机构
[1] CSIC, Inst Environm Assessment & Water Res IDAEA, Dept Geosci, ES-08034 Barcelona, Spain
关键词
Cement; Concrete; C-S-H; Kinetics; Dissolution; CALCIUM-SILICATE-HYDRATE; WASTE STABILIZATION SYSTEMS; AQUEOUS SOLUBILITY DIAGRAMS; BETA-DICALCIUM SILICATE; TRICALCIUM SILICATE; PORTLAND-CEMENT; THERMODYNAMIC MODEL; PASTE; SLAG;
D O I
10.1016/j.pce.2013.11.003
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
C-S-H gel dissolution kinetics was studied by means of flow-through experiments under CO2-free atmosphere at room temperature (23 +/- 2 degrees C). The starting C-S-H gel was obtained by hydration of commercial C3S (3CaO center dot SiO2) and consisted of 67 wt% C-S-H with a Ca/Si ratio of 1.7 +/- 0.1 and 33 wt% portlandite. Based on the changes in aqueous chemistry and in the C-S-H solid, it was observed that the C-S-H gel dissolves incongruently when the Ca/Si ratio is high and congruently as the Ca/Si ratio decreases to the tobermorite stoichiometric Ca/Si ratio of 0.83. First, a dissolution rate law for C-S-H gel with Ca/Si ratio equal to 0.83 is proposed based on the dissolution rates normalized to the final BET surface area. Additionally, reactive transport modeling of the changes in aqueous chemistry allowed the fitting of the rate constants for C-S-H with Ca/Si ratio ranging from 1.7 to 0.83. Solid examination by SEM-EDX and EPMA before and after the experiments showed some variability of the Ca/Si ratios of the analyzed particles, suggesting the existence of compositional domains with variable Ca/Si ratios. Si-29 MAS NMR spectra showed an increase in polymerization of the reacted C-S-H, and also the formation of Si-rich domains in some cases, mainly under slow flow conditions. Inhibition of the rates in these cases will have to be further investigated. (C) 2013 Elsevier Ltd. All rights reserved.
引用
收藏
页码:17 / 31
页数:15
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