波特兰岩
硅粉
粉煤灰
水泥
材料科学
硅酸盐水泥
穆斯堡尔谱学
八面体
钙矾石
冶金
矿物学
化学工程
复合材料
化学
结晶学
晶体结构
工程类
作者
Vili Lilkov,O. Petrov,Yana Tzvetanova,Plamen Savov
标识
DOI:10.1016/j.conbuildmat.2011.10.030
摘要
Two octahedral Fe3+ positions with close isomeric displacements and quadrupole splittings were proved for plain cement using Mössbauer spectroscopy. In cements with silica fume iron is registered as two Fe3+ and one Fe2+ doublets. Hydrating cement pastes display a third doublet of tetrahedral iron indicating ettringite–monosulfate transformation. With silica fume and fly ashes addition the tetrahedral iron doublet forms earlier. With hydration the tetrahedral iron increases at the expense of octahedral iron. During hydration of plain cement portlandite and hydration products form below 450 °С. Silica fume and fly ashes react with portlandite and form products decomposing above 620–640 °С.
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