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Voltages induced on a test power line from artificially initiated lightning: Theory and experiment.

机译:由人工引发的雷电在测试电源线上感应的电压:理论和实验。

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Measurements are presented and characterized of vertical electric fields 500 m from artificially initiated lightning return strokes and of voltages induced at both ends of a 448 m distribution power line by the same discharges, which are about 20 m from one end of the line. The experiment, which took place during the Summer of 1986 at the NASA Kennedy Space Center, is described. The measured line voltages could be grouped into two categories, those in which multiple, similarly shaped, evenly spaced pulses were observed, which we call oscillatory, and those dominated by a principal pulse with subsidiary oscillations of much smaller amplitude, which we call impulsive. Voltage amplitudes range from tens of kilovolts for oscillatory voltages to hundreds of kilovolts for impulsive voltages. Contrary to what was expected, the voltage at the transmission line end farther from the lightning was found to be considerably larger than the voltage at the end nearer to the lightning.;A new technique is derived for the calculation of the electromagnetic fields from nearby lightning over an imperfectly conducting ground. This technique is used in conjunction with a time domain coupling theory to calculate voltages at either end of the line. The results show fair agreement with the measured oscillatory voltage waveforms if corona is ignored and improved results when corona effects are modelled. Reasonable wave shape agreement is obtained for voltages of the impulsive type when these are modelled by the introduction of non-linear flashover effects, although unrealistically high return stroke currents are required to obtain good amplitude agreement. Suggestions for future experiments are given in the light of the present experience in measuring electric fields and their associated voltages from very close lightning.
机译:给出并表征了测量结果,这些测量结果来自人工引发的雷电回击500 m的垂直电场,以及在448 m配电电源线两端通过相同的放电感应的电压,这些放电距离该线的一端约20 m。描述了该实验,该实验于1986年夏季在NASA肯尼迪航天中心进行。测得的线电压可分为两类,其中观察到多个形状相似,间隔均匀的脉冲,我们称其为振荡脉冲,而以主脉冲为主,其副振荡幅度较小,我们称其为脉冲。电压幅度范围从振荡电压的几十千伏到脉冲电压的数百千伏不等。与预期相反的是,发现传输线远离雷电的一端的电压比靠近雷电的一端的电压大得多。;推导了一种新技术来计算附近闪电的电磁场在不完全导电的地面上。该技术与时域耦合理论结合使用,可以计算线路两端的电压。结果表明,如果忽略电晕,则与测得的振荡电压波形相当吻合;对电晕效应进行建模后,结果会得到改善。当通过引入非线性闪络效应来对脉冲类型的电压进行建模时,可以获得合理的波形一致性,尽管需要不切实际的高返回冲程电流才能获得良好的振幅一致性。根据目前在非常近的闪电中测量电场及其相关电压的经验,提出了对未来实验的建议。

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