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Classification of hematite types in iron ores through circularly polarized light microscopy and image analysis

机译:通过圆偏振光显微镜和图像分析对铁矿石中的赤铁矿类型进行分类

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摘要

Brazilian iron ores are predominantly hematitic and may have different textures. In the mining industry, their microstructural characterization is manually performed, by analyzing samples under an optical microscope to identify the hematite textures and estimate'their fractions and crystal size. This procedure is subjective and consequently susceptible to random and systematic errors. The present paper proposes an automatic method for the identification, measurement and classification of hematite crystals in iron ore according to their textural types. The method exploits the use of circularly polarized light to amplify brightness and color differences among hematite crystals, allowing their individualization, and the subsequent morphological analysis and classification into granular, lamellar or lobular classes. The classifier was tested with more than 5400 crystals, reaching a global success rate close to 98%, and success rates per class above 96%.
机译:巴西铁矿石主要为杂矿物,质地可能不同。在采矿业中,通过在光学显微镜下分析样品以鉴定赤铁矿质地并估算其级分和晶体尺寸,可以手动进行其微结构表征。此过程是主观的,因此容易受到随机和系统错误的影响。本文提出了一种根据组织类型自动识别,测量和分类铁矿石中赤铁矿晶体的方法。该方法利用圆偏振光来放大赤铁矿晶体之间的亮度和色差,从而使它们个体化,并随后进行形态分析并将其分类为颗粒,层状或小叶类别。使用5400多个晶体对分类器进行了测试,全球成功率接近98%,每个类别的成功率都超过96%。

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