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首页> 外文期刊>Journal of Electromagnetic Waves and Applications >Analytic modeling of oblique penetration of early-time high altitude electromagnetic pulse into dispersive underground multilayer structures
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Analytic modeling of oblique penetration of early-time high altitude electromagnetic pulse into dispersive underground multilayer structures

机译:早期高空电磁脉冲斜渗透到分散地下多层结构中的解析模型

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摘要

In this paper, a formulation for obliquely incident electromagnetic wave has been presented for an analysis of high-power electromagnetic pulse penetration into multilayer dispersive media. Based on generalized models of measured dielectric constants and propagation channels reflecting the Earths general features, the propagation phenomenon of the obliquely incident early-time (E1) high-altitude electromagnetic pulse (HEMP) is analyzed in frequency as well as in time domains. In addition, the polarization and critical angle are also considered. It is found that the total reflection occurs at an incident angle of about 38 at the soil-rock interface, and that the parallel-polarized E1 HEMP penetrates better than the perpendicular-polarized one. The peak level of the penetrating electric field is found to be 5.6 kV/m at normal incidence, regardless of the type of polarization, and 1.1 kV/m for incidence at 30 in perpendicular case.
机译:本文提出了一种倾斜入射电磁波的配方,用于分析高功率电磁脉冲穿透到多层分散介质中的情况。基于测得的介电常数和反映地球一般特征的传播通道的通用模型,对斜入射的早期(E1)高空电磁脉冲(HEMP)的传播现象进行了频率和时域分析。另外,还考虑了极化和临界角。发现在土壤-岩石界面处的全反射以约38的入射角发生,并且平行偏振的E1 HEMP的穿透性比垂直偏振的更好。不论极化类型如何,在垂直入射情况下,穿透电场的峰值水平均为5.6 kV / m,在垂直入射情况下,在30°C时入射电场的峰值水平为1.1 kV / m。

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