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Extracting lithologic information from ASTER multispectral thermal infrared data in the eastern Kunlun

机译:从昆仑东部的ASTER多光谱热红外数据中提取岩性信息

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In this paper, mechanisms of mineral radiation transfer, atmospheric correction and surface temperature retrieve, method of minerals identification based on emissivity spectral features are studied. Mineral radiation transfer can model the mechanisms of spectral formation and variation, and is one of study methods of spectral mechanism. Along with the variation of mineral granularity, the shape and absorption depth of mineral emissivity spectral will all variate. However, the law of emissivity variation with emission angle of different minerals is identical. Along with the increasement of emission angle, emissivity decrease. The more emissivity is small, the more variation range and speed are large. The reflectance mixture of mineral is non-linear, and can be lineated using mineral radiative transfer model. After the mixture spectral is lineated, the precision of linear unmixing of spectral and mineral content extraction will be improved greatly. The atmospheric correction and surface temperature retrieve of thermal remote sensing data will affect extraction lithologic information greatly. In this paper, using the MODTRAN model to atmospheric correction, and using split-window algorithm for retrieving surface temperature from ASTER thermal infrared data. With the minerals emissivity spectral features and the index (QI, CI and SI), retrieving Si0_2 content of rock quantitatively using ASTER thermal infrared data. The method can be used to extract lithologic information.
机译:本文研究了矿物辐射的传输机理,大气校正和地表温度反演,基于发射率光谱特征的矿物识别方法。矿物辐射传递可以模拟光谱形成和变化的机制,是光谱机制的研究方法之一。随着矿物粒度的变化,矿物发射光谱的形状和吸收深度都会发生变化。但是,不同矿物的发射率随发射角的变化规律是相同的。随着发射角的增加,发射率降低。发射率越小,变化范围和速度越大。矿物的反射率混合物是非线性的,可以使用矿物辐射传递模型进行拟合。对混合光谱进行划线后,光谱和矿物含量提取物的线性解混精度将大大提高。热遥感数据的大气校正和地表温度反演将极大地影响提取岩性信息。本文使用MODTRAN模型进行大气校正,并使用分割窗口算法从ASTER热红外数据中检索表面温度。利用矿物的发射率光谱特征和指数(QI,CI和SI),使用ASTER热红外数据定量检索岩石中的Si0_2含量。该方法可用于提取岩性信息。

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