3.8 Article

Effects of MgO and Fe2O3 Addition for Upgrading the Refractory Characteristics of Magnesite Ore Mining Waste/By-Products

期刊

CLEAN TECHNOLOGIES
卷 4, 期 4, 页码 1103-1126

出版社

MDPI
DOI: 10.3390/cleantechnol4040067

关键词

magnesite mining waste; MgO additive; Fe2O3 additive; forsterite (olivine); thermal treatment; refractory products

资金

  1. European Union
  2. Greek National Funds through the Operational Program Competitiveness, Entrepreneurship and Innovation
  3. [T1EDK-03543]

向作者/读者索取更多资源

In the context of a circular economy/zero-waste, the conversion of extractive wastes into new products is emphasized. The addition of caustic calcined magnesia (MgO) and iron oxide (Fe2O3) was found to enhance the refractoriness and mechanical strength of the waste, indicating their potential for waste upcycling.
In the context of a circular economy/zero-waste, the conversion of extractive wastes into new products is of particular importance. At the Grecian Magnesite SA mine (Chalkidiki, N. Greece), millions of tons of waste accumulate in the operation field. To achieve these goals, the effect of caustic calcined magnesia (MgO) at 10, 15, and 20 wt.% was investigated in combination with 0.5, 1, 2.5, and 5 wt.% Fe2O3 at 1300 degrees C and 1600 degrees C for 120 min. The main refractory properties were determined along with the mineralogical content. The morphological examination has been performed by SEM-EDS analysis. The addition of MgO increases the desired olivine and eliminates the unwanted pyroxenes, causing the formation of magnesium-ferrite and periclase. MgO wt.% addition resulted in the decrease of firing shrinkage at 1300 degrees C but increased with Fe2O3. At 1600 degrees C, firing shrinkage had a minimum value at the optimum MgO dose. Mechanical strength at 1600 degrees C achieved a maximum value at the optimum MgO dose plus 5 wt.% MgO and 2.5 wt.% Fe2O3 due to sintering process/magnesioferrite formation. These results indicate that MgO and Fe2O3 upgrade the refractoriness of magnesite mining wastes due to the diffusion of Fe2O3 in MgO excess.

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