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

机译:用AIEM模型模拟盐分土壤的反向散射系数

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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 W polarization respectively at the high moisture region. Moreover, the simulation results also suggest that VVor HH polarization can be used to retrieve soil salinity for the soil with low moisture (<0.3 cm~3·m~(-3)).
机译:土壤盐分主要影响发展中国家的农业地区的土壤特性,环境和生产力。目前,尚无反演算法可直接根据微波遥感数据确定土壤盐分,但我们希望利用土壤水分反演算法获得土壤盐分量。因此,结合改进的Dobson介电混合模型,使用高级积分方程模型(AIEM)模拟了水分和盐度对介电常数和反向散射系数(VV和HH极化模式)的影响。结果表明,介电常数的实部随土壤盐分含量的增加而降低,而虚部则随其增加而增加,特别是在高水分地区。土壤水分和盐分都影响VV和HH极化后向散射系数,随着水分的后向散射系数明显增加,但随着土壤盐分后向散射系数在较小的水分区域增加,HH极化保持不变或表现出W的弱向下趋势在高水分区域分别极化。此外,模拟结果还表明,VVor HH极化可用于恢复低水分(<0.3 cm〜3·m〜(-3))土壤的盐度。

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