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Influencing Factors of the Mineral Carbonation Process of Iron Ore Mining Waste in Sequestering Atmospheric Carbon Dioxide

机译:在螯合大气二氧化碳中铁矿石采矿废弃物矿物碳化过程的影响因素

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摘要

Mining waste may contain potential minerals that can act as essential feedstock for long-term carbon sequestration through a mineral carbonation process. This study attempts to identify the mineralogical and chemical composition of iron ore mining waste alongside the effects of particle size, temperature, and pH on carbonation efficiency. The samples were found to be alkaline in nature (pH of 6.9–7.5) and contained small-sized particles of clay and silt, thus indicating their suitability for mineral carbonation reactions. Samples were composed of important silicate minerals needed for the formation of carbonates such as wollastonite, anorthite, diopside, perovskite, johannsenite, and magnesium aluminum silicate, and the Fe-bearing mineral magnetite. The presence of Fe2O3 (39.6–62.9%) and CaO (7.2–15.2%) indicated the potential of the waste to sequester carbon dioxide because these oxides are important divalent cations for mineral carbonation. The use of small-sized mine-waste particles enables the enhancement of carbonation efficiency, i.e., particles of <38 µm showed a greater extent of Fe and Ca carbonation efficiency (between 1.6–6.7%) compared to particles of <63 µm (0.9–5.7%) and 75 µm (0.7–6.0%). Increasing the reaction temperature from 80 °C to 150–200 °C resulted in a higher Fe and Ca carbonation efficiency of some samples between 0.9–5.8% and 0.8–4.0%, respectively. The effect of increasing the pH from 8–12 was notably observed in Fe carbonation efficiency of between 0.7–5.9% (pH 12) compared to 0.6–3.3% (pH 8). Ca carbonation efficiency was moderately observed (0.7–5.5%) as with the increasing pH between 8–10. Therefore, it has been evidenced that mineralogical and chemical composition were of great importance for the mineral carbonation process, and that the effects of particle size, pH, and temperature of iron mining waste were influential in determining carbonation efficiency. Findings would be beneficial for sustaining the mining industry while taking into account the issue of waste production in tackling the global carbon emission concerns.
机译:采矿废物可能含有潜在的矿物,可以通过矿物碳化过程作为长期碳封存的基本原料。该研究试图鉴定铁矿石采矿废物的矿物学和化学成分以及粒度,温度和pH对碳化效率的影响。发现样品在性质上是碱性的(pH为6.9-7.5),并包含粘土和淤泥的小尺寸颗粒,从而表明它们适合于矿物碳化反应。样品由重要的硅酸盐矿物组成,所述硅酸盐如硅酸岩,钙钛矿,偶孔,钙钛矿,约翰烯及铝硅酸镁,以及Fe轴承的矿物质。 Fe2O3(39.6-62.9%)和CaO(7.2-15.2%)的存在表明废物沉浸二氧化碳的潜力,因为这些氧化物是矿物质碳化的重要二价阳离子。使用小尺寸的矿井废物颗粒能够提高碳化效率,即,与<63μm的颗粒相比,<38μm的颗粒显示出更大程度的Fe和Ca碳化效率(1.6-6.7%)(0.9 -5.7%)和75μm(0.7-6.0%)。将反应温度从80℃升高至150-200℃,导致一些样品的Fe和Ca碳化效率分别为0.9-5.8%和0.8-4.0%。增加了8-12的pH从8-12的效果在0.7-5.9%(pH12)之间,而0.6-3.3%(pH 8)。随着pH值的增加,适度地观察到Ca碳化效率(0.7-5.5%)。因此,已经证明了矿物学和化学组成对于矿物质碳化过程具有重要意义,并且粒度,pH值和铁矿垃圾的效果在确定碳化效率时受到影响。在考虑到解决全球碳排放问题时,在考虑到废物生产问题时,调查结果将有利于维持矿业。

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