波特兰岩
钙矾石
硅酸盐水泥
材料科学
相(物质)
氢氧化物
溶解度
水泥
氢氧化钙
矿物学
硫酸盐
原子力显微镜
碳酸盐
复合材料
化学工程
无机化学
化学
物理化学
冶金
纳米技术
有机化学
工程类
作者
Thomas Matschei,Barbara Lothenbach,F. P. Glasser
标识
DOI:10.1016/j.cemconres.2006.10.010
摘要
The AFm phase of Portland cements refers to a family of hydrated calcium aluminates based on the hydrocalumite-like structure of 4CaO·Al2O3·13–19 H2O. However OH− may be replaced by SO42− and CO32−. Except for limited replacement (50 mol%, maximum) of sulfate by hydroxide, these compositions do not form solid solutions and, from the mineralogical standpoint, behave as separate phases. Therefore many hydrated cements will contain mixtures of AFm phases. AFm phases have been made from precursors and experimentally-determined phase relationships are depicted at 25 °C. Solubility data are reported and thermodynamic data are derived. The 25 °C stability of AFm phases is much affected by the nature of the anion: carbonate stabilises AFm and displaces OH and SO4 at species activities commonly encountered in cement systems. However in the presence of portlandite, and as carbonate displaces sulfate in AFm, the reaction results in changes in the amount of both portlandite and ettringite: specimen calculations are presented to quantify these changes. The scheme of phase balances enables calculation of the mineralogical balances of a hydrated cement paste with greater accuracy than hitherto practicable.
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