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Modelling the backscattering coefficient of salt-affected soils using AIEM model

机译:利用AIEM模型建模盐影响土壤的后散射系数

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Soil salinity principally affects soil properties, environment and productivity of agricultural areas for developing countries. Currently, no inversion algorithms exist for directly determining soil salinity from microwave remote sensing data, but we hope to draw on the soil moisture retrieval algorithms to obtain soil salinity amount. So the effect of moisture and salinity on dielectric constant and the backscattering coefficient (VV and HH polarization mode) are simulated using the advanced integral equation model (AIEM) combined with the modified Dobson dielectric mixing model. The results indicate that real part of dielectric constant decreases with soil salinity content, however, the imaginary part increases with it especially for the high moisture regions. Both soil moisture and salinity affect the VV and HH polarization backscattering coefficient, with moisture the backscattering coefficient increases evidently, but with soil salinity backscattering coefficient increase at the small moisture region and it remains unchanged for the HH polarization or expresses the weakly downward tendency for VV polarization respectively at the high moisture region. Moreover, the simulation results also suggest that VV or HH polarization can be used to retrieve soil salinity for the soil with low moisture (<0.3 cm~(3) (centre dot) cm~(-3)).
机译:土壤盐度主要影响发展中国家农业区域的土壤性质,环境和生产力。目前,不存在从微波遥感数据中确定土壤盐度的反演算法,但我们希望利用土壤水分检索算法来获得土壤盐度。因此,使用先进的整体方程模型(AIEM)与改进的多板电介质混合模型相结合模拟了水分和盐度对介电常数和后散射系数(VV和HH偏振模式)的影响。结果表明,介电常数的实际部分随着土壤盐度含量降低,然而,假想部分随着高湿度区域而增加。土壤湿度和盐度都会影响VV和HH偏振反向散射系数,水分随着后散射系数显然增加,但是在小水分区域的土壤盐度反向散射系数增加,并且对于HH偏振,它们保持不变或表达VV的弱向下趋势分别在高水分区域处的偏振。此外,仿真结果还表明VV或HH偏振可用于检索具有低水分的土壤的土壤盐度(<0.3cm〜(3)(中心点)cm〜(-3))。

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