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Finite Element Calculation of Geomagnetic Induced CurrentBased on a Three-dimensional Earth Conductivity Model
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Cheng QIAN1, Qiao MA2, *, Lei YANG3, Xiao-yan TAN1, Guo-ping FU1, Kai-long MIN1, Chun-yu LU1
Science Technology and Engineering | 2025, 25(1) : 201 - 209
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Science Technology and Engineering | 2025, 25(1): 201-209
Papers·Electrical Technology
Finite Element Calculation of Geomagnetic Induced CurrentBased on a Three-dimensional Earth Conductivity Model
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Cheng QIAN1, Qiao MA2, *, Lei YANG3, Xiao-yan TAN1, Guo-ping FU1, Kai-long MIN1, Chun-yu LU1
Affiliations
  • 1. The Ultra High Voltage Branch Company of State Grid Xinjiang Electric Power Co., Ltd., Urumqi 830063, China
  • 2. China National Heavy Machinery Research Institute Co., Ltd., Xi’an 710018, China
  • 3. School of Electric Engineering, Xi’an University of Technology, Xi’an 710048, China
Published: 2025-01-08 doi: 10.12404/j.issn.1671-1815.2401932
Outline
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A geomagnetic storm is a periodic natural disaster in which the changing geomagnetic field can induce an induced geoelectric field. A geomagnetic induced current (GIC) loop is formed between the transmission line and the earth conductor through the neutral points of grounding transformers. GIC seriously threatens the safe and stable operation of extra-high and ultra-high voltage AC transmission systems. There are many types of terrain and complex structures in our country, which makes the influence of geological landforms on induced geoelectric fields very significant. A finite element calculation method for GIC was proposed based on a three-dimensional earth conductivity model to address the difficulties in modeling and calculating GIC. Firstly, a three-dimensional earth conductivity model was established considering the anisotropy of geological structures. Meanwhile, a calculation model for electromagnetic field penetration depth under multi-layer geological conditions was given. Secondly, a mathematical model based on time-varying electromagnetic fields was established. Combined with the topology of the power grid, an equivalent calculation model for the power grid GIC was derived. Finally, taking the Shache-Turpan 750 kV transmission line in Xinjiang area as an example, a corresponding physical model was built in COMSOL Multiphysics finite element simulation software. The three-dimensional distribution of the induced ground electric field in the power grid was obtained through geometric modeling, boundary condition setting, grid division, and iterative solution. Furthermore, the GIC flowing through the neutral point of the 750 kV transformer was obtained. The research results indicatethat the overall level of GIC obtained by the 3D model is higher than that of the 2D model. Besides, the 3D model considers the geometric angle between the transmission line and different terrains, which can provide a more detailed distribution of induced geoelectric fields. The research results verify the effectiveness of the method proposed, which provides a reference basis for scientific planning of ultra-high and ultra-high voltage transmission corridors.

geomagnetic storms  /  earth conductivity  /  induced geoelectric field  /  geomagnetic induced current  /  finite element analysis
Cheng QIAN, Qiao MA, Lei YANG, Xiao-yan TAN, Guo-ping FU, Kai-long MIN, Chun-yu LU. Finite Element Calculation of Geomagnetic Induced CurrentBased on a Three-dimensional Earth Conductivity Model[J]. Science Technology and Engineering, 2025 , 25 (1) : 201 -209 . DOI: 10.12404/j.issn.1671-1815.2401932
Year 2025 volume 25 Issue 1
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Article Info
doi: 10.12404/j.issn.1671-1815.2401932
  • Receive Date:2024-03-18
  • Online Date:2025-07-29
  • Published:2025-01-08
Article Data
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History
  • Received:2024-03-18
  • Revised:2024-10-11
Funding
Affiliations
    1. The Ultra High Voltage Branch Company of State Grid Xinjiang Electric Power Co., Ltd., Urumqi 830063, China
    2. China National Heavy Machinery Research Institute Co., Ltd., Xi’an 710018, China
    3. School of Electric Engineering, Xi’an University of Technology, Xi’an 710048, China
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表12种不同金属材料的力学参数

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鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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