A Coupled FEM-BEM Methodology to Calculate 3-D Earth Surface Potentials Caused by HVDC Return Currents
In the ground-return mode of high-voltage direct current (HVDC) transmissions, a large dc injected current in the earth will result in a rise in the earth surface potential (ESP), causing a dc bias in the power transformer and a dysfunction of the relay protection. Nevertheless, the accurate ESP cal...
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| Published in | IEEE transactions on magnetics Vol. 60; no. 3; pp. 1 - 4 |
|---|---|
| Main Authors | , , |
| Format | Journal Article |
| Language | English |
| Published |
New York
IEEE
01.03.2024
The Institute of Electrical and Electronics Engineers, Inc. (IEEE) |
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| Online Access | Get full text |
| ISSN | 0018-9464 1941-0069 |
| DOI | 10.1109/TMAG.2023.3309388 |
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| Abstract | In the ground-return mode of high-voltage direct current (HVDC) transmissions, a large dc injected current in the earth will result in a rise in the earth surface potential (ESP), causing a dc bias in the power transformer and a dysfunction of the relay protection. Nevertheless, the accurate ESP calculation using the existing approaches will face challenges such as an extremely complex soil structure with inhomogenous mediums and a large-scale problem including an extremely small dimension of electrodes. To address the aforementioned issues, a novel coupled finite element-boundary element (BEM) method-based methodology is developed for the efficient and accurate calculation of 3-D ESP. In the proposed methodology, the finite element method (FEM) is used to solve the inhomogenous soil region while the BEM method is employed to solve the remaining layered homogeneous ones. An iterative solution methodology is proposed to implement the coupling of the two methods. Numerical examples on a case study are presented, illustrating the performance and advantages of the proposed method and its potentialities in engineering applications. |
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| AbstractList | In the ground-return mode of high-voltage direct current (HVDC) transmissions, a large dc injected current in the earth will result in a rise in the earth surface potential (ESP), causing a dc bias in the power transformer and a dysfunction of the relay protection. Nevertheless, the accurate ESP calculation using the existing approaches will face challenges such as an extremely complex soil structure with inhomogenous mediums and a large-scale problem including an extremely small dimension of electrodes. To address the aforementioned issues, a novel coupled finite element-boundary element (BEM) method-based methodology is developed for the efficient and accurate calculation of 3-D ESP. In the proposed methodology, the finite element method (FEM) is used to solve the inhomogenous soil region while the BEM method is employed to solve the remaining layered homogeneous ones. An iterative solution methodology is proposed to implement the coupling of the two methods. Numerical examples on a case study are presented, illustrating the performance and advantages of the proposed method and its potentialities in engineering applications. |
| Author | Yang, Shiyou Xu, Xiaowen Li, Yiying |
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| Cites_doi | 10.1109/TEMC.2021.3062441 10.1007/978-0-387-21738-3 10.1002/nme.4984 10.1190/1.1440975 10.1109/ACCESS.2019.2953914 10.1016/j.compstruc.2012.04.010 10.1109/PES.2007.385516 10.1016/c2014-0-01297-x 10.1016/j.epsr.2020.106478 10.1109/ICEMS.2019.8921456 10.1109/TPWRD.2016.2610443 10.1016/j.engstruct.2014.03.036 10.1109/TPWRD.2003.809741 10.1155/2012/472457 |
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| SubjectTerms | Boundary element method (BEM) Boundary-element methods Conductivity Direct current Earth surface earth surface potential (ESP) Electric potential Electrodes Finite element analysis Finite element method finite element method (FEM) high-voltage direct current (HVDC) HVDC transmission Iterative methods Iterative solution Mathematical analysis Mathematical models Methodology Methods Numerical methods Soil measurements Soil structure Three-dimensional displays |
| Title | A Coupled FEM-BEM Methodology to Calculate 3-D Earth Surface Potentials Caused by HVDC Return Currents |
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