从 SinoProbe Magnetotelluric Impedances 估测华北地磁风暴期间的地电场

IF 3.7 2区 地球科学 Space Weather Pub Date : 2024-03-28 DOI:10.1029/2023sw003758
Qihe Shao, Ying Liu, Yinhe Luo, Graham Heinson, Yixian Xu, Jinsong Du, Chao Chen
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摘要

评估地磁扰动对电网基础设施的影响对于降低地磁感应电流(GIC)带来的风险至关重要。本文根据 2015 年 3 月 17 日重大地磁暴期间记录的 SinoProbe Magnotelluric(MT)阻抗数据和 INTERMAGNET 六个站点的地磁观测数据,估算了华北地区的地电场和感应电压分布。119 个 SinoProbe MT 站点测得的阻抗与地磁观测站数据进行了卷积,以考虑地球复杂的三维电阻率结构。由此产生的地电场被用于模拟华北区域输电网络的感应电压分布。由于 "中国探地 MT "项目的站点间距较大,得出的地电场大多是均匀的,只有鄂尔多斯盆地的地电场呈现极化现象,且造山带的地电场幅度较大。在风暴期间,由于高电阻率岩石圈导致地球上的电压梯度较大,华北太行-吕梁、燕山和鲁西造山带的估计地电场较大(>1 V/km)。然而,就主要输电线路的位置而言,只有华北中部地区的感应电压超过 100 V。
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Geoelectric Field Estimations During Geomagnetic Storm in North China From SinoProbe Magnetotelluric Impedances
Evaluating the impact of geomagnetic disturbances on power grid infrastructure is critical to mitigate the risk posed by geomagnetically induced currents (GICs). In this paper, the geoelectric field and induced voltage distribution in North China were estimated from the SinoProbe magnetotelluric (MT) impedance data together with the geomagnetic observatory data of six INTERMAGNET stations recorded during the significant geomagnetic storm of 17th March 2015. The measured impedances from 119 SinoProbe MT sites were convolved with geomagnetic observatory data to account for the Earth's complex three-dimensional electrical resistivity structure. The resultant geoelectric field was then used to model the induced voltage distribution across the regional power transmission network in North China. Due to the large inter-site distances of the SinoProbe MT program, the derived geoelectric field is mostly homogeneous, except in the Ordos Basin that displays a polarization of the geoelectric field, and with higher magnitudes in the orogenic belts. The estimated geoelectric fields in Taihang-Lvliang, Yanshan, and Luxi orogenic belts of North China were large (>1 V/km) during the storm, due to high-resistivity lithosphere resulting in large voltage gradients in the Earth. However, in relation to locations of major power transmission lines, only the central part of North China experienced induced voltages exceeding 100 V.
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