Modeling the hyperspectral reflectance signal of moist sandy soils

B. Somers, W. Verstraeten, S. Delalieux, P. Coppin
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Abstract

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.
湿润沙质土壤高光谱反射信号的模拟
去除光谱图像中的土壤水分效应是农业遥感的关键。然而,目前可用的土壤水分反射率模型无法正确地处理相同质地类别土壤中微妙但重要的水分诱导反射率变化。这些模型的实际执行是有限的,特别是在农田里,农田内的土壤特征,如有机质和粘土含量的变化很普遍。在本研究中,研究了土壤含水量(SMC,重量含水量)对位于南非西开普省柑橘果园的6个沙质土壤400 ~ 2500nm光谱域反射率的影响。提供了沙质耕地土壤水分反射率模型的新见解。本文对模型参数的波长变化和土壤特性变化进行了力学模拟,提出了耕作沙土湿润反射率的一般模型,并成功地进行了测试。
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