Downward Continuation Method Using Equivalent Source Technique with Full-Parameter Joint Estimation
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摘要: 水下地磁导航性能高度依赖于高精度地磁参考图,利用航空或海面磁测数据通过向下延拓技术获取水下磁场信息是最经济可行的途径。传统向下延拓方法基于固定等效源位置假设,该先验约束与复杂地质构造真实分布存在本质偏差,在深水区域引入显著系统误差。针对此问题,提出了一种基于全参数联合估计的等效源向下延拓方法。该方法通过等效源位置与磁矩的协同优化,使等效源分布自适应于真实场源特征。采用磁偶极子作为基本单元,利用自动微分技术实现参数联合梯度计算,通过自适应优化算法迭代求解最优配置。仿真实验结果表明,该方法相较于单层固定源法和多层固定源法,延拓精度提升1个数量级以上。该方法为高精度地磁导航参考图生成提供了可靠技术支撑。Abstract: To address accuracy limitations in equivalent source-based downward continuation arising from fixed equivalent source positioning, a novel magnetic field continuation technique dynamically optimizing equivalent source parameters is proposed. Traditional approaches utilizing predefined subsurface equivalent source configurations exhibit inherent deviations from geological realities, resulting in substantial errors during deep magnetic field characterization. In contrast, simultaneous three-dimensional dynamic optimization of both equivalent source positions and magnetic moments yields enhanced structural congruence with geological formations. Simulation results demonstrate that the proposed method improves the continuation accuracy by more than one order of magnitude compared to the single-layer and multi-layer fixed-source methods. This advancement provides enhanced precision for critical applications including deep-sea mineral exploration, crustal fault identification, and geomagnetic navigation systems.
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