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Modeling the hyperspectral reflectance signal of moist sandy soils

机译:模拟潮湿沙质土壤的高光谱反射信号

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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:消除光谱图像中的土壤水分影响对于农业遥感至关重要。然而,当前可用的土壤水分反射率模型未能正确地解决相同质地类别的土壤中细微但显着的水分诱导反射率变化。因此,这些模型的操作实施受到限制,特别是在农田中有机质和黏土含量等土壤特征在田间变化普遍的农田中。在这项研究中,研究了位于南非西开普省柑桔园的六种沙质土壤在400至2500 nm光谱域中土壤水分含量(SMC,按重量计的水分含量)对反射率的影响。在沙质耕作土壤的土壤水分反射率模型中提供了新颖的见解。对模型参数中的波长和土壤特定变化进行了机械建模,并提出并成功地测试了人工沙土湿反射率的通用模型。

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