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Comparison Between 1-D and 3-D Geoelectric Field Methods to Calculate Geomagnetically Induced Currents: A Case Study

机译:1-D和3-D地质电场方法计算地磁诱导电流的比较 - 以案例研究

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摘要

Severe Geomagnetic Disturbances (GMD) pose a threat to the reliability of the United States bulk electrical power system. The NERC reliability standard TPL-007 requires transmission planners to assess potential problems in their service territories due to Geomagnetically Induced Currents (GIC) including transformer thermal assessment. If the assessment indicates a vulnerability, the standard requires the development of a corrective action plan to resolve potential issues. GIC calculation accuracy is critical to the assessment. In this paper, the impact of various geoelectric field calculation methods on the accuracy of calculated GIC is evaluated by comparing with observations for a geomagnetic storm that occurred on 07–08 September, 2017. The GIC calculation is carried out for a fairly large-scale power system model and the comparison with observation indicates that better results are achieved using magnetotelluric transfer functions that incorporate the effects of 3-D earth conductivity. The results also indicate an improvement in the comparisons when the transfer-function derived E-fields are interpolated between the original survey site locations.
机译:严重的地磁干扰(GMD)对美国散装电力系统的可靠性构成了威胁。 NERD可靠性标准TPL-007需要传输规划者,以评估其服务领域的潜在问题,因为包括变压器热评估包括变压器热评估。如果评估表明漏洞,标准要求开发纠正措施计划以解决潜在问题。 GIC计算精度对评估至关重要。在本文中,通过与2017年9月07日至08日发生的地磁风暴的观察相比,评价各种地质电场计算方法对计算GIC的准确性的影响。越来越大的GIC计算进行了速度计算电力系统模型和与观察的比较表明,使用磁通传递函数实现了更好的结果,该函数包含3-D接地电导率的影响。结果还表明在原始调查站点位置之间插入转移函数导出的电子字段时的比较的改进。

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