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Measurement and modeling of the millimeter-wave backscatter response of soil surfaces

机译:土壤表面毫米波反向散射响应的测量和建模

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The millimeter-wave (MMW) backscatter response of bare-soil was examined by conducting experimental measurements at 35 and 94 GHz using a truck-mounted polarimetric scatterometer and by developing appropriate models to relate the backscattering coefficient to the soil's surface and volume properties. The experimental measurements were conducted for three soil surfaces with different roughnesses under both dry and wet conditions. The experimental measurements indicate that in general the backscattering coefficient is comprised of a surface scattering component /spl sigma//sup s/ and a volume scattering component /spl sigma//sup v/. For wet soil conditions, the backscatter is dominated by surface scattering, while for dry conditions both surface and volume scattering are significant, particularly at 94 GHz. Because theoretical surface scattering models were found incapable of predicting the measured backscatter, a semiempirical surface scattering model was developed that relates the surface scattering component of the total backscatter to the roughness parameter ks, where k=2/spl pi///spl lambda/ and s is the rms height, and the dielectric constant of the soil surface. Volume scattering was modeled using radiative transfer theory with the packed soil particles acting as the host material and the air voids as the scattering particles. The combined contribution of surface and volume scattering was found to provide good agreement between the model calculations and the experimental observations.
机译:裸土的毫米波(MMW)反向散射响应是通过使用车载式偏振散射仪在35 GHz和94 GHz上进行实验测量并开发适当的模型以将反向散射系数与土壤的表面和体积特性相关联来检查的。在干燥和潮湿条件下,对三个具有不同粗糙度的土壤表面进行了实验测量。实验测量表明,总体上后向散射系数由表面散射分量/ spl sigma // sup s /和体积散射分量/ spl sigma // sup s /组成。对于潮湿的土壤条件,后向散射主要由表面散射引起,而对于干燥的条件,表面散射和体积散射均很明显,尤其是在94 GHz时。由于发现理论表面散射模型无法预测测得的反向散射,因此开发了半经验表面散射模型,该模型将总反向散射的表面散射分量与粗糙度参数ks相关,其中k = 2 / spl pi /// spl lambda / s是均方根值,是土壤表面的介电常数。使用辐射传递理论对体积散射进行建模,其中填充的土壤颗粒充当主体材料,空气空隙作为散射颗粒。发现表面和体积散射的组合贡献在模型计算和实验观察之间提供了良好的一致性。

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