Effect of Ferrous Additives on Magnesia Stone Hydration

International Conference on Construction, Architecture and Technosphere Safety 2017

土木建筑工程

Zimich, V.^1

Architecture and Construction Institute, South Ural State University, Lenin Avenue, 76, Chelyabinsk

454080, Russia^1

关键词: Analysis method;    Iron hydroxides;    Magnesium hydroxide;    Stone structures;    Variable factors;    Water-resistances;    X-ray microanalyzer;    X-ray phase analysis;   

Others  :  https://iopscience.iop.org/article/10.1088/1757-899X/262/1/012001/pdf
DOI  :  10.1088/1757-899X/262/1/012001

学科分类：土木及结构工程学

来源: IOP

【 摘 要 】

The article deals with the modification of the magnesia binder with additives containing two- and three-valent iron cations which could be embedded in the chloromagnesium stone structure and also increase the strength from 60 MPa in a non-additive stone to 80MPa, water resistance from 0.58 for clear stone to 0.8 and reduce the hygroscopicity from 8% in the non-additive stone to 2% in the modified chloromagnesium stone. It is proposed to use the iron hydroxide sol as an additive in the quantities of up to 1% of the weight of the binder. The studies were carried out using the modern analysis methods: the differentialthermal and X-ray phase analysis. The structure was studied with an electron microscope with an X-ray microanalyzer. A two-factor plan-experiment was designed which allowed constructing mathematical models characterizing the influence of variable factors, such as the density of the zatcher and the amount of sol in the binder, on the basic properties of the magnesian stone. The result of the research was the magnesia stone with the claimed properties and formed from minerals characteristic for magnesian materials as well as additionally formed from amachenite and goethite. It has been established that a highly active iron hydroxide sol the ion sizes of which are commensurate with magnesium ions is actively incorporated into the structure of pentahydroxychloride and magnesium hydroxide changing the habit of crystals compacting the structure of the stone and changing its hygroscopicity.