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首页> 外文期刊>Journal of spectroscopy >Characterization and Identification of Coal and Carbonaceous Shale Using Visible and Near-Infrared Reflectance Spectroscopy
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Characterization and Identification of Coal and Carbonaceous Shale Using Visible and Near-Infrared Reflectance Spectroscopy

机译:可见和近红外反射光谱法表征和鉴定煤和碳质页岩

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Because of the high organic carbon concentration in carbonaceous shale, a large proportion of carbonaceous shales are often misclassified into coals using visible and near-infrared (VIS-NIR) reflectance spectroscopy in the field of coal-gangue identification of hyperspectral remote sensing of coal mine. In order to study spectral characterization of coal and carbonaceous shale, three bituminite samples and three carbonaceous shales were collected from a coal mine of China, and their spectral reflectance curves were obtained by a field spectrometer in the wavelength range of 350–2500 nm. Only one carbonaceous shale could be easily identified from the three bituminite samples according to obvious absorption valleys near 1400 nm, 1900 nm, and 2200 nm of its reflectance curve while the other two carbonaceous shales have similar reflectance curves to the three bituminite samples. The effect of carbon concentration on reflectance curve was simulated by the mixed powder of ultralow ash bituminite and clay in 0.5 mm grain size under various mixing ratios. It was found that absorption valleys near 1400 nm, 1900 nm, and 2200 nm of the mixed powder become not obvious when the bituminite content is more than 30%. In order to establish an effective identification method of coal and carbonaceous shale, 250 other samples collected from the same coal mine were divided into 150 training samples and 100 prediction samples. Principal component analysis (PCA) and Gauss radial basis kernel principal component analysis (GRB-KPCA) were employed to extract principal components (PCs) of continuum removed (CR) spectra of the training samples in eight selected wavelength regions which are related to the main mineral and organic compositions. Two support vector machine- (SVM-) based models PCA-SVM and GRB-KPCA-SVM were established. The results showed that the GRB-KPCA-SVM model had better identification accuracies of 94% and 92% for powder and nature block prediction samples, respectively.
机译:由于碳质页岩中有机碳含量高,在煤-石识别高光谱遥感领域中,可见碳和近红外(VIS-NIR)反射光谱法经常将大量碳质页岩误分类为煤。 。为了研究煤和碳质页岩的光谱特征,从中国一个煤矿采集了三个沥青样品和三个碳质页岩,并通过现场光谱仪在350-2500 nm的波长范围内获得了光谱反射率曲线。根据其反射率曲线在1400 nm,1900 nm和2200 nm附近的明显吸收谷,可以从三个沥青样品中轻松识别出一个碳质页岩,而其他两个碳质页岩的反射率曲线与这三个沥青样品相似。在不同混合比下,以0.5 mm的超低灰烟灰石和粘土混合粉模拟了碳浓度对反射率曲线的影响。结果表明,当沥青含量超过30%时,混合粉体在1400 nm,1900 nm和2200 nm附近的吸收谷不明显。为了建立一种有效的煤和碳质页岩识别方法,将同一煤矿采集的其他250个样本分为150个训练样本和100个预测样本。采用主成分分析(PCA)和高斯径向基核主成分分析(GRB-KPCA)提取与八个样本相关的八个选定波长区域中训练样本的连续去除(CR)光谱的主成分(PC)。矿物和有机成分。建立了两个基于支持向量机(SVM)的模型PCA-SVM和GRB-KPCA-SVM。结果表明,对于粉末和自然块预测样品,GRB-KPCA-SVM模型具有更好的识别准确率,分别为94%和92%。

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