Growth of brucite (Mg(OH)2) on portlandite (Ca(OH)2)

被引:0
作者
Galan, I. [1 ,2 ]
Baumann, C. [1 ]
Sakoparnig, M. [2 ]
Grengg, C. [1 ]
Dietzel, M. [1 ]
机构
[1] Graz Univ Technol, Inst Appl Geosci, Rechbauerstr 12, A-8010 Graz, Austria
[2] Graz Univ Technol, Inst Technol & Testing Bldg Mat, Inffeldgasse 24, A-8010 Graz, Austria
关键词
A1; Characterization; A1. Crystal morphology; A2. Growth from solution; B1; Minerals; B1. Inorganic compounds; B1. Calcium compounds; MAGNESIUM-SULFATE ATTACK; CEMENT PASTE; CONCRETE; SEAWATER; THAUMASITE; STABILITY; CHLORIDES; CORROSION; MECHANISM; MODEL;
D O I
10.1016/j.jcrysgro.2025.128071
中图分类号
O7 [晶体学];
学科分类号
0702 ; 070205 ; 0703 ; 080501 ;
摘要
The potential protective effect of brucite (Mg(OH)2) grown on portlandite (Ca(OH)2) was analysed. Single crystals of portlandite were synthesized and exposed to Mg2+-containing solutions and the influence of the central parameters was analysed: (i) magnesium ion source (MgCl2 and MgSO4) (ii) initial Mg2+ concentration (0.01-1 mol/l), (iii) crystal surface to solution volume ratio, and (iv) duration of experiment. Solids and solutions were characterised by means of FTIR, ICP-OES, pH measurements, SEM and EPMA. Additionally, thermodynamic calculations were performed. The results showed that the morphology and thickness and thus the protective properties of the brucite layer were conditioned by the Mg2+ and Ca2+ concentration in the solution. Brucite layers grown during exposure to higher initial Mg2+ concentration were denser and thinner, offering better protection against further dissolution. In MgCl2 solutions, the precipitation of a compact brucite layer was accompanied by the formation of an empty cavity between brucite and portlandite. In MgSO4 solutions the space between brucite and portlandite was filled with gypsum as saturation conditions were reached providing extra protection but also leading to potential crack formation in the brucite layer.
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页数:8
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