直流接地极近区三维大地电阻率模型建立方法
Three-Dimensional Earth Resistivity Structure Modelling Around DC Ground Electrode
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摘要: 大地电阻率模型不准确是造成对直流输电接地极极址周边地面、地下导电体以及交流电网影响评估不准确的主要原因。根据接地极电流产生的地表电位(earth surface potential,ESP)具有以接地极为中心类同心圆分布的特点,利用地壳/上地幔历史电磁测深数据、资料和直流接地极工程选址设计电磁测深数据、资料,提出评估接地极近区ESP分布的大地电阻率三维模型建立方法。利用?800 k V天中直流输电工程哈密接地极周边交流电网直流偏磁电流(DC biasing current,DCBC)的实测数据,证明利用大地电阻率三维模型计算的电网DCBC准确、可靠,所建模型对接地极选址设计和电网DCBC治理方案优化都有重要意义。Abstract: The imprecise earth resistivity model is the main reason for the inaccurate impact assessment of the conductors on ground or underground and AC networks around DC ground electrode.Earth surface potential(ESP) produced by ground current has the characteristic of concentric circle distribution with the center of the ground electrode.Based on the engineering data of ground electrode and the historical magnetotelluric sounding data of the crust and upper mantle,a three-dimensional earth resistivity model was proposed to evaluate the distribution of ESP around DC ground electrode.It was proved that DC biasing current(DCBC) calculated by three-dimensional earth resistivity model is accurate and reliable by comparing measured data of DCBC in AC networks around Hami DC ground electrode of ±800 kV Tian-Zhong UHVDC project with the modeling result.The model has great significance to the site selection and design of ground electrode and the optimization of DCBC control scheme.