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Effect of Antireflective Surface at the Radiobrightness Observations for the Topsoil Covered with Coniferous Litter

机译:覆盖有针叶凋落物的表层土壤的抗光性观察对减反射表面的影响

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In radio thermal remote sensing of the land, a spot on the earth surface emitting the signal received by the microwave radiometer antenna may be partially or completely covered by forest. We developed a theoretical model to calculate radiobrightness of the layered topsoil. Using this model we derived the dielectric constants pertaining to the separate layers of topsoil. For this purpose, we applied the least squares method for fitting the calculated diurnal radiobrightness dependences to those measured. The forest soil covered with coniferous litter was modeled by a three steps dielectric profile, the interfaces between the separate layers being smooth. The theoretical modeling conducted confirmed that, at the moments of maximal radiobrightness, an antireflective layer was formed on the topsoil surface, most probably due to nonisothermal upward moving of soil moisture. At that, the theoretically calculated dielectric constant of the litter antirefiecting layer was found to be on the same order as the value measured in laboratory conditions.
机译:在陆地的无线电热遥感中,地球表面上发出微波辐射计天线接收到的信号的点可能会被森林部分或完全覆盖。我们开发了一个理论模型来计算层状表层土壤的放射亮度。使用该模型,我们得出了与表土各层有关的介电常数。为此,我们应用了最小二乘法,将计算出的昼间放射线亮度依赖性与所测得的值进行拟合。针叶树覆盖的森林土壤通过三步介电剖面进行建模,各层之间的界面光滑。进行的理论建模证实,在最大的辐射亮度时刻,在表土表面上形成了抗反射层,这很可能是由于土壤水分的非等温向上运动所致。那时,发现理论上计算出的垫料防反射层的介电常数与在实验室条件下测得的值处于同一数量级。

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