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Hyperspectral imagery for mineral exploration: comparison of data from two airborne sensors

机译:矿物勘探的高光谱图像:两个机载传感器的数据比较

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Abstract: Hyperspectral image data sets acquired near Cuprite, Nevada in 1995 with the SWIR full spectrum imager (SFSI) and in 1996 with the Airborne Visible/IR Imaging Spectrometer (AVIRIS) are analyzed with a spectral unmixing procedure and the result compared. The SFSI image has pixels on 1 m by 1.5 m centers, the AVIRIS on 17 m centers; the region imaged by SFSI is a small portion of the full AVIRIS scene. Both have nominal spectral band center spacings of about 10 nm. The image data, converted to radiance units, are atmospherically corrected and converted to surface reflectance. Spectral end members are extracted automatically from the two data sets; those representing mineral species common to both are compared to each other and to reference spectra obtained with a portable IR mineral analyzer. The full sets of end members are used in a constrained linear unmixing of the respective hyperspectral image cubes. The resulting unmixing fraction images derived from the AVIRIS and the SFSI data sets for the minerals alunite, buddingtonite, and kaolinite exhibit strong similarities. !12
机译:摘要:1995年使用SWIR全光谱成像仪(SFSI)在内华达州Cuprite附近和1996年使用机载可见/红外成像光谱仪(AVIRIS)采集了高光谱图像数据集,并进行了光谱混合处理,并对结果进行了比较。 SFSI图像的像素位于1 m x 1.5 m的中心,AVIRIS的像素位于17 m的中心; SFSI成像的区域只是整个AVIRIS场景的一小部分。两者都具有大约10 nm的标称光谱带中心间距。转换为辐射单位的图像数据在大气中进行校正并转换为表面反射率。光谱末端成员是自动从两个数据集中提取的;将代表两者共同的矿物种类的那些相互比较,并与使用便携式红外矿物分析仪获得的参考光谱进行比较。全套末端构件用于各个高光谱图像立方体的约束线性解混合中。从AVIRIS和SFSI数据集得出的矿质亚矾石,芽孢石和高岭石的解混分数图像显示出很强的相似性。 !12

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