模拟了不同几何形状传感器的大气电场和电流结构与外电路中测量电流的关系

K. Sobolewski, M. Kubicki
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引用次数: 0

摘要

电场测量有许多科学应用。他们的研究结果可用于大气电力、优化电力安全,例如防雷和气象学。然而,测量应该同样可靠地进行,以得出可靠的结论。在理论和实践中,你可以找到各种各样的测量方法,有些已经使用了很多年,并且可以使用计算机模拟的可能性来验证它们的准确性。这项工作包括电场传感器实例的场分析,在此基础上进行了讨论并得出了实用的结论。描述式测量方法常用于雷电电场分布的测量。本文在数值模拟的基础上,研究了电场和电流传感器的原理。它既可用于大气闪电放电的物理问题,也可用于晴天电的物理问题。电场E和$\mathbf{\Delta} \mathbf{E}$测量在文献中得到了广泛的描述,并具有大量的技术应用。雷暴电和晴朗天气条件下麦克斯韦电流密度及其分量的测量与许多解释和技术困难有关。它可能会接触到雷云下的电流或来自远处放电的电流。例如,Krider和Musser[1]确定了$\mathbf{Ez}(\mathbf{t}) =\mathbf{0}$情况下的麦克斯韦电流(导通电流是当E为零时它总是消失)。目前的测量方法直接基于高斯或安培-麦克斯韦方程,并选择适当的传感器表面在这些表面或边界表面的路径上进行积分操作,可能证明是困难的或不可能的。它需要选择一个唯一的高斯曲面来计算电场,需要选择一个特定的安培回线来确定磁场和电流密度。
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Simulation of the atmospheric electric field and current structure for sensors with different geometry in relation to the electric current measured in the external circuit
Electric field measurements have many scientific applications. Their results can be used in atmospheric electricity, optimisation of electric safety, e.g. lightning protection and meteorology. However, a measurement should be performed equally reliably to draw reliable conclusions. In theory and practice, you can find various measurement methods, some used for many years and which can be verified in terms of their accuracy using the possibility of computer simulations. This work contains a field analysis of examples of electric field sensors, based on which a discussion was held and practical conclusions were drawn. Described measurement methodology is often used for measurements of lightning electric field distribution. The article concerns the theory of sensors for measuring electric field and current based on numerical simulations. It can be used both in the problems of the physics of atmospheric lightning discharges and fair-weather electricity. Electric field E and $\mathbf{\Delta} \mathbf{E}$ measurements are widely described in the literature and have large technical applications. Measurements of the Maxwell current density and its components for thunderstorm electricity and fair weather conditions are associated with many interpretations and technical difficulties. It may touch cases like currents under a thundercloud approaching or currents from distant discharges. For example, Krider and Musser [1] determined the Maxwell current in a situation where $\mathbf{Ez}(\mathbf{t}) =\mathbf{0}$ (conduction current is that it always vanishes when E is zero). Current measurement methods based directly on Gauss or Ampere-Maxwell equations and selecting appropriate sensor surfaces to carry out the integration operation on these surfaces or the path that bounds that surface may prove difficult or impossible. It needs to choose a unique Gaussian surface to calculate the electric field and a particular Amperian loop to determine the magnetic field and current density.
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