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An efficient method for processing scalar magnetic gradiometer signals

机译:一种处理标量磁梯度仪信号的有效方法

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The work is devoted to the detection and analysis of scalar magnetic gradiometer survey signals caused by the presence of magnetostatic dipole in the vicinity of the survey line. A set of five orthonormal functions obtained with the aid of Gram-Schmidt procedure was found sufficient for an accurate signal description in a wide range of distances between the gradiometer and the dipole. Processing of the acquired signal can be carried out by correlating it with the mentioned five orthonormal functions. In the special case of short-base gradiometer the dipole signal can be expressed by four orthonormal functions. The present work main contribution is in showing that these four orthonormal functions are sufficient and effective for a survey signal processing even when the gradiometer base is not small. The effectiveness of the magnetic anomaly detection procedure is demonstrated for extracting signals in the presence of an additive noise. The practical contribution of such approach is the development of more robust and less time-consuming detection procedures that are vital for successful real-time data processing. (C) 2004 Elsevier B.V. All rights reserved.
机译:这项工作致力于检测和分析由测量线附近的静磁偶极子引起的标量磁梯度仪测量信号。发现通过格拉姆-施密特(Gram-Schmidt)程序获得的一组五个正交函数足以在梯度仪和偶极子之间的较宽距离范围内准确描述信号。可以通过将获取到的信号与提到的五个正交函数相关联来进行处理。在短基梯度计的特殊情况下,偶极子信号可以用四个正交函数表示。本工作的主要贡献在于,即使梯度计的基数不小,这四个正交函数对于调查信号处理也是足够且有效的。磁异常检测程序的有效性已证明可在存在附加噪声的情况下提取信号。这种方法的实际贡献是开发了更强大且耗时更少的检测程序,这对于成功进行实时数据处理至关重要。 (C)2004 Elsevier B.V.保留所有权利。

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