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Modeling the hyperspectral reflectance signal of moist sandy soils

机译:潮湿含沙土的高光谱反射信号

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Removing soil moisture effects in spectral images is critical for agricultural remote sensing. Yet, current available soil moisture reflectance models fail to properly address subtly, yet significant, moisture induced reflectance changes within soils of the same texture class. The operational implementation of these models is as such limited, particularly in agricultural fields where within-field variations in soil characteristics such as organic matter and clay content prevail. In this study, the effect of soil moisture content (SMC, water content by weight) on the reflectance in the 400 to 2500 nm spectral domain is studied for six sandy soils located in Citrus orchards in the Western Cape Province, South Africa. Novel insights in soil moisture reflectance modeling of sandy cultivated soils are provided. The wavelength and soil specific variations in model parameters are mechanistically modeled and a general model for moist reflectance of cultivated sand soils is presented and successfully tested.
机译:去除光谱图像中的土壤湿度效应对于农业遥感至关重要。然而,目前可用的土壤水分反射模型不能正确地解决相同纹理阶级的土壤中的土壤中的含水量,但显着的水分诱导的反射率变化。这些模型的操作实施是如此有限,特别是在农业领域,其中土壤特征如有机物和粘土含量的现场变化。在这项研究中,对在400〜2500nm的频域反射土壤含水量(SMC,重量的水含量)的影响。研究了坐落在西开普省,南非柑橘园6个沙质土壤。提供了砂土栽培土壤土壤水分反射率建模的新型见解。模型参数的波长和土壤特定变化是机械模型的,并呈现并成功地测试了培养砂土的湿润反射率的一般模型。

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