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CE-1干涉成像光谱仪数据信息提取技术研究
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摘要
针对西安光机所研制的嫦娥一号(CE-1)干涉成像光谱仪(IIM)数据信息提取技术展开研究。IIM数据对于完成分析月球表面矿物类型含量与分布,绘制月球表面岩石分布图等科学任务具有重要意义。首先讨论了数据优化技术,其次研究了针对IIM数据的光度校正和反射率反演技术,最后分析月表高光谱图像的矿物质信息提取技术。
     首先讨论了数据优化技术。针对IIM数据中的条带噪声,在传统线性插值法基础上,提出结合了三阶插值的改进线性插值方法,该方法对噪声点定位后,根据图像中噪声点上下行相应点的数值差别是否超过预设阈值,确定是采用线性插值还是三阶插值算法,修正噪声点像素值。对比试验采用均值和标准偏差以及图像质量因子(IQ因子)作为评价标准。结果表明:改进的线性插值方法在去除IIM影像条带噪声方面明显优于传统线性插值法和频域滤波法。
     CE-1干涉成像光谱仪获取的干涉图数据通过光谱复原后得到的是目标的光谱辐亮度,其包含了目标反照率、光照条件、地形等因素的信息,而光谱反射率是分析月表物质类型的主要因素,故必须去除地形、光照等干扰。文中通过比较各种光度校正及反射率反演算法的优劣,采用布朗大学的经验公式对其进行光度校正,取得了良好的效果。并采用了平场域法、利用太阳辐射光谱两种方法对图像进行反射率反演,将辐亮度值反演为绝对反射率值。结果表明:两种方法反演后的绝对反射率曲线是基本一致的。
     由于仪器分辨率、月壤混和特性等原因,IIM获得的光谱数据实际是多种物质类型的混合光谱。要提取物质类型的含量信息,必须进行混合像元分解。文中讨论了各种混合像元分解算法,选择最小距离分类法、光谱角分类法作为IIM的影像分析模型,将该方法用于CE-1的光谱反射率数据,得到的结果现有的理论是基本一致的。
Research on CE-1 Imaging Interferometer (IIM) spectral information extraction technology is implemented. The instrument is developed by Xi'an Institute of Optics and Precision Mechanics to analyze mineral contents and distribution of different types and draw rock distribution map on lunar surface. Data optimization technology is discussed firstly and the Photometric correction and reflection inversion is researched then. At last, the mineral information distraction technology on lunar surface is analyzed.
     Data optimization technology is discussed. Aiming at the striping noise existing in IIM data, the Fourier transform algorithm and the linear interpolation algorithm are experimentally utilized for strip noise removal in IIM images. A modified linear interpolation algorithm is proposed, which combines low rank algorithm with high rank algorithm. After noise location, high rank interpolation or linear interpolation is used by judging whether the pixel difference between the upper and lower lines goes up to the threshold. Comparison of mean values and standard deviations as well as the IQ (Image Quality) factor shows that this modified method is evidently superior to the linear algorithm.
     Hyperspectral images transformed from Interferogram obtained by IIM contain information on reflectance, light condition, terrain and so on. Reflectance is the main factor to analyze mineral type on lunar surface. Therefore, interference caused by terrain and light condition should be removed. By summarize the advantages and disadvantages of several kinds of method of Photometric correction and reflection inversion, empirical formula of Brown University is used on photometric correction. Both the Flat-Field method and the method which utilize the solar radiation spectrum are used on reflectance, inversion in order to transform radiant brightness image into reflectance, image. Results show that the absolute reflectance, curves obtained by both two methods are basically identical.
     The spectrum data obtained by IIM is actually mixed spectrum of various materials due to instrumental resolution, mixed lunar soil, and so on. Therefore, pixel unmixing is essential to distraction information on mineral type. Different kinds of algorithms of pixel unmixing are discussed and compared. The minimum distance and spectrum angle mapper method are chosen as analyzing model for IIM data. Results show that the mineral distribution in the image is basically identical to the theory known to people in nowadays.
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