基于仿真的水下点源目标物磁异常特征及其磁法可测性预测研究

Research on Magnetic Anomaly Characteristics and Magnetic Detectability Prediction of Underwater Point Source Targets Based on Simulation

  • 摘要: 为全面了解水下点源目标物的磁异常特征及其影响因素,科学合理地制定针对性的磁法探测方案,采用重磁位场的泊松方程推导了水下点磁源总场磁异常的计算模型,并通过仿真分析了相关参数对磁异常特征的影响效果。在此基础上,提出了水下点源目标物的磁法可测性预测问题,根据磁异常幅度大小将可测性分为不可测、弱、中等和强四个等级。提出应根据已知的目标物参数、背景地磁参数和水深环境信息等采用仿真计算对目标物磁异常特征进行预测,并顾及可测性和观测平面控制难度两方面因素,制定最优的磁法测线布设方案。水下点源目标物磁法测线方案应采用“网格”布设方式,最优主测线方向应与地磁偏角方向一致,最优主测线间距为垂直主剖面方向上磁异常区跨度的三分之一。定义了“定位分位”(Pfra),用于准确判定目标物在磁异常等值线图或主剖面磁异常曲线上的对应位置,其仅与地磁倾角负相关,给出了Pfra基于地磁倾角的拟合公式,可根据测区位置计算Pfra以便于在探测过程中对目标物位置实现快速、准确地判定。

     

    Abstract: The feasibility and effectiveness of the detection scheme are critical issues determining operational success rates and efficiency. To address these challenges during scheme design, establishing a theoretical model for underwater target magnetic anomaly and applying forward modeling to simulate target detectability and magnetic anomaly characteristics represents the preferred methodology. Using Poisson's Equation for gravity and magnetic potential fields, we derived a model for calculating the total-field magnetic anomaly of an underwater point source target, ignoring remanence. Simulation analyses quantified how key parameters influence magnetic anomaly characteristics. Building on this foundation, we established a framework for predicting underwater target magnetic detectability. This framework requires predicting a target's magnetic anomaly characteristics using known target parameters, ambient geomagnetic field conditions, and water depth. We further propose an optimized magnetic survey line design that balances detectability constraints with operational challenges in observation plane control (specifically magnetometer towfish altitude). We classify magnetic detectability of underwater point source targets into four levels based on anomaly amplitude: undetectable (0–3 nT), weak (3–10 nT), medium (10–50 nT), and strong (> 50 nT). Crucially, aside from objective factors, observation altitude (R) represents a major operator-adjustable parameter governing detectability. For magnetic surveys targeting underwater point sources, a grid-like layout is optimal. The main survey lines should be oriented at D. Optimal line spacing equals one-third the width of the magnetic anomaly zone perpendicular to the main survey direction. To precisely locate targets on magnetic anomaly contour maps or main profiles, we define a positioning quantile (Pfra). This parameter exhibits an inverse correlation solely with geomagnetic inclination (I), for which we provide a fitting formula. Pfra can be calculated from the survey area's geographic coordinates, enabling rapid target localization during over-water detection.

     

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