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Monitoring of Soil Degradation Potential in Semi Arid Soils Using Hyper spectroscopy Technology

机译:利用高光谱技术监测半干旱土壤退化潜力

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摘要

Based on previous studies that showed significant correlation between crusted soil and their reflectance properties, we applied a systematic study over Loess soil from Israel using Hyperspectral (or Imaging Spectroscopy) technology. A simulation for rain events under laboratory conditions, using the selected soil and varying ram energy treatments was conducted and reflectance properties of the crusted soils were measured. A spectral parameter defined as a Normalized Spectral Area (NSA) was used to assess for the crust status (based on the area under a ratio spectrum relative to a known non-crusted soils' plot). The NSA laboratory parameter was applied to the AISA data using ground controlled soil plots (crusted and non crusted). A reasonable agreement was obtained between the two data sets (laboratory and air) suggesting that infiltration rates values can be estimated remotely. It is strongly suggested that future study, will use the full optical range (VIS-NER-SWIR-TIR) in the IS technology to map the crust status in a better precise way.
机译:基于先前的研究表明,结皮土壤与其反射特性之间存在显着相关性,我们使用高光谱(或成像光谱)技术对以色列的黄土进行了系统的研究。使用选定的土壤和不同的夯锤能量处理对实验室条件下的降雨事件进行了模拟,并测量了结皮土壤的反射特性。定义为归一化光谱区域(NSA)的光谱参数用于评估结皮状态(基于相对于已知非结皮土壤图的比率谱下的面积)。使用地面控制的土壤图(硬皮和非硬皮)将NSA实验室参数应用于AISA数据。在两个数据集(实验室数据和空气数据)之间获得了合理的共识,这表明可以远程估计渗透率值。强烈建议将来的研究将使用IS技术中的整个光学范围(VIS-NER-SWIR-TIR),以更好的精确方式绘制地壳状态图。

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