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Geological Zoning of Tideland Sediments by a Combination of Sample Reflectance and Satellite Remote Sensing

机译:样本反射率与卫星遥感相结合的滩涂沉积物地质分区

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For detecting spatio-temporal changes of tideland environments in a closed sea by remote sensing technique, geological zoning is proposed based on the surface reflectance spectra from visible to short wave infrared wavelength. The spectra are characterized by sample measurements and satellite image data analyses. The measurements clarify that the spectra patterns, which are the increase degree of reflectance with wavelength and the existence of reflectance absorption, are attributable to die mineral composition and that the magnitudes of reflectance are determined by particle size of the sediments. In general, the spectra are classified into two types which are mainly located around two river mouths. We present effectiveness of two-band ratio processing and color composite using ASTER image data for the geological zoning. The zoning is also investigated by a kriging method using the semivariogram of the average reflectance of image data and the category data depending on the spectral pattern at the sample locations. The kriging map can contribute to interpret the extent of sediments bearing similar particle size and main constituent minerals.
机译:为了利用遥感技术检测封闭海域潮间带环境的时空变化,提出了基于从可见光到短波红外波长的表面反射光谱的地质分区方法。通过样品测量和卫星图像数据分析来表征光谱。测量结果表明,光谱模式,即反射率随波长的增加程度和反射率吸收的存在,可归因于矿物成分,并且反射率的大小由沉积物的粒径决定。通常,光谱分为两种类型,主要位于两个河口附近。我们介绍了使用ASTER图像数据进行地质分区的两频带比率处理和颜色合成的有效性。分区也通过克立格方法使用图像数据和类别数据的平均反射率的半变异函数根据样本位置处的光谱模式进行研究。克里金图可以帮助解释具有相似粒径和主要组成矿物的沉积物的范围。

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