电气化铁路接地电位问题分析

Chen Jiancheng
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引用次数: 2

摘要

电气化铁路的牵引回回路通常是由架空接触线系统将电流传输到电力机车,再通过轨道和接地返回到牵引变电所。也就是说,它属于以轨道和接地为回线的不平衡供电系统。在电流进入轨道的接地点附近,引起接地电位上升,通过地电阻耦合的方式对接地的电信设备和线路产生危险的冲击或干扰冲击。在现有的地球势理论计算中,假定地球是具有无限平面的均匀介质。然而,铁路所经过的自然地质大多属于不规则非均质介质。这给理论上计算地电位提出了一个问题。此外,在过去电气化铁路的勘测设计过程中,许多技术人员将可用于计算互感系数的地电阻率引用到地电位公式中。这种方法在计算非均匀介质中的地电位时是错误的。对地电位的计算会产生多重误差,对地电位采取保护措施时也会出现失误。针对上述情况,本文分析了干扰源和影响方式的特点,提出了一种解决非均匀介质中大地电位计算问题的新方法。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Analysis of the earth potential problems of the electrified railway
The traction return circuit of the electrified railway is usually that the overhead contact line system (OHL) transmits current to the electric locomotives, then the current returns to the traction substations by the rails and earth. That is, it belongs to the unbalanced power-supply system that uses the rails and earth as return conductor. Near the point of earth that current enters into the rails, it causes the earth potential to rise, and it cause dangerous impact or interference impact on the earthed telecommunication equipment and lines by the way of earth resistance coupling. Earth is assumed to be a homogeneous medium with an infinite plane in the existing theoretical calculation of earth potential. However, most of geology in nature where railway passes belongs to irregular nonhomogeneous medium. It raises a problem for theoretically calculating the earth potential. Furthermore, during the processes of survey and design of the electrified railway in the past, many technicians cited the earth resistivity that can be used for calculating mutual inductance coefficient to the formulas of earth potential. This method is wrong for calculating the earth potential in the nonhomogeneous medium. It may cause multiple error for calculating the earth potential and slip in adopting the protective measures for the earth potential. In view of the above-mentioned circumstances, this paper analyzes the characteristics of the interference sources and impact ways, and presents a new method for solving the problem of calculating the earth potential in the nonhomogeneous medium.
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