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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Lightning electromagnetic radiation over a stratified conducting ground:2. Validity of simplified approaches
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Lightning electromagnetic radiation over a stratified conducting ground:2. Validity of simplified approaches

机译:闪电电磁辐射了分层进行地面:2。简化的方法

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In the first part of this paper, the rigorous theory describing the electromagnetic field radiated by a lightning return stroke over a two-layered conducting ground was presented and the exact expressions for the lightning electromagnetic fields were developed and discussed. In this part of the paper, the theory along with its time domain numerical evaluation algorithm is used for the assessment of the validity of simplified approaches proposed in the literature for the vertical electric and horizontal magnetic field components. The simplified approaches are based on the concept of ground surface impedance and its corresponding attenuation function. It is shown that the results obtained using the simplified approaches are in excellent agreement with exact results in both near (50 m) and intermediate (1000 m) distance range. However, since the vertical electric and azimuthal magnetic field components are not appreciably affected by the ground finite conductivity, they can also be evaluated assuming the ground as a perfectly conducting ground. On the other hand, the horizontal electric field above a horizontally stratified ground is very much affected by the ground electrical parameters. Its waveform is characterized by an early negative excursion due to the currents flowing into the ground followed by a late time positive excursion which is due to the elevation of the observation point from the ground level. The magnitude of the negative peak is sharper for subsequent return strokes than first return strokes and is higher for lower conducting grounds. A new formula is proposed for the evaluation of the horizontal electric field at a given height above the air-ground interface. The formula can be viewed as the generalization of the Cooray-Rubinstein formula for the case of a two-layer ground. We show that the new formula is able to reproduce in a satisfactory manner the horizontal electric field above a two-layer ground. The proposed formulation is, however, less accurate at distances as close to 10 m from the channel base and for very poor ground conductivity (0.0001 S/m).
机译:在本文的第一部分,严格描述电磁场的理论辐射的闪电回击了两层导电地面了闪电的精确表达式发达国家和电磁场进行了讨论。连同其时域数值评估算法是用于评估的有效性提出的简化方法垂直电场和文学水平磁场分量。简化方法是基于的概念地面阻抗及其相应衰减函数。结果使用简化的方法是在良好的协议与准确的结果附近(50米)和中间(1000米)距离范围内。电场和磁场方位组件不明显影响地面有限电导率,他们也可以评估假设地上一个完美进行。另一方面,横向电场高于地面水平分层多地电的影响参数。早期的负偏移由于电流流入地面,后跟一个迟到的时间积极的偏移是由于海拔从地面观测点的水平。负峰的大小是尖锐的随后返回中风比第一次回来中风和降低导电高理由。评估水平电场的给予高度的空中接口。公式可以被视为的概括Cooray-Rubinstein公式的情况下两层。能够以令人满意的方式繁殖横向电场超过两层地面。不准确的距离接近10 m地面频道基础和非常贫穷电导率(0.0001 S / m)。

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