A method of using geomagnetic anomaly to recognize objects based on HOG and 2D-AVMD
Source abstract
Abstract
In order to identify the shape of underground small magnetic anomaly objects, we use Support Vector Machines (SVM) to identify the underground magnetic anomaly targets. Firstly, as the SVM needs a lot of training data, and we also need to make full use of the magnetic field signal, nine component signals including total magnetic intensity (TMI) and five independent components of tensor are calculated from the original detected magnetic signal. Secondly, the nine component signals are subjected respectively to two-dimensional adaptively variational mode decomposition (2D-AVMD), which is advanced based on the two indicators, namely Mutual information (MI) and empirical entropy (EE), and we can get the nine primary signals from the decomposition results of nine component signals called the Intrinsic Mode Function (IMF). Then, the Histogram of Oriented Gradients (HOG) of the nine primary signals is extracted, and the feature data would be constructed into feature vectors. In the end, Support Vector Machines (SVM) are adopted to process these feature vectors. The output of the SVM can indicate the result of small objects’ shape recognition under the ground. Experiments prove that the shape recognition accuracy of underground small magnetic anomaly object recognition reaches 90%.
Source: crossref · Quality: baseline
Research context
OpenAlex topics: Geophysical and Geoelectrical Methods · Geophysical Methods and Applications · NMR spectroscopy and applications
SciVX discovery tags are terminology-based. OpenAlex topics are source-provided classifications.
Affiliations
The Army Engineering University of PLA Shijiazhuan Campus 1 , Shijiazhuan 050003, China
High Speed Institute of China Aerodynamics Research and Development Center 2 , Mianyang, Sichuan 621000 China
References (38)
Show source-provided references
1. New methods for interpretation of magnetic vector and gradient tensor data I: Eigenvector analysis and the normalised source strength10.1071/eg12020 ↗
2. A closed-form formula for magnetic dipole localization by measurement of its magnetic field and spatial gradients10.1109/tmag.2006.879151 ↗
3. Geometric invariants of magnetic dipole gradient tensor and its application
4. Interpretation of magnetic gradient tensor for automatic locating adipole source10.1071/aseg2012ab228 ↗
5. Moore–Penrose generalized inverse of the gradient tensor in Euler’s equation for locating a magnetic dipole10.1063/1.4869066 ↗
6. Estimating source location using normalized magnetic source strength calculated from magnetic gradient tensor data10.1190/geo2011-0437.1 ↗
7. Implementation of an unshielded SQUID as a geomagnetic sensor
8. Full magnetic gradient tensor from triaxial aeromagnetic gradient measurements: Calculation and application10.1007/s11770-015-0508-y ↗
9. Gravity and Magnetic Exploration (Principles, Practices, and Applications)
10. Comment on ‘depth estimation of simple causative sources from gravity gradient tensor invariants and vertical component’ by B. Oruç10.1007/s00024-011-0302-6 ↗
11. Pure and Applied Geophysics · 2010 · 167 · 125910.1007/s00024-009-0021-4 ↗
12. R. Stolz, V. Zakosarenko, M. Schulz et al., “Magnetic full tensor SQUID gradiometer system for geophysical applications,” Seg Technical Program Expanded, 2006.10.1190/1.2172308 ↗
13. On the application of Euler deconvolution to the analytic signal10.1190/1.2360204 ↗
14. Preferential filtering for gravity anomaly separation10.1016/j.cageo.2012.09.012 ↗
15. A Support Vector Clustering Method
16. A fuzzy support vector machine algorithm for classification based on a novel PIM fuzzy clustering method10.1016/j.neucom.2012.07.049 ↗
17. A tutorial on support vector machines for pattern recognition10.1023/a:1009715923555 ↗
18. LPiTrack: Eye movement pattern recognition algorithm and application to biometric identification10.1007/s10994-017-5649-1 ↗
19. Pattern recognition of geophysical data10.1016/j.geoderma.2009.09.008 ↗
20. Statistical pattern recognition technique to enhance anomalies in magnetic surveys10.1016/s0926-9851(96)00059-6 ↗
21. Image processing of aeromagnetic data and integration with Landsat images for improved structural interpretation10.1190/1.1442358 ↗
22. Evaluation of adaptive boosting and neural network in earthquake damage levels detection10.5120/17507-8058 ↗
23. EMD based on recursive high-pass filter and its application on seismic signal analysis
24. Two-dimensional nonlinear geophysical data filtering using the multidimensional EEMD method10.1016/j.jappgeo.2014.10.015 ↗
25. Multiscale fractures characterization based on ant colony optimization and two-dimensional variational mode decomposition10.1109/jstars.2018.2837222 ↗
26. Histograms of oriented gradients for human detection
27. Finding people in images and videos
28. Two-dimensional variational mode decomposition10.1007/978-3-319-14612-6_15 ↗
29. A new model for quantifying anisotropic scale invariance and for decomposition of mixing patterns10.1023/b:matg.0000028441.62108.8a ↗
30. Identification of REE mineralization-related geochemical anomalies using fractal/multifractal methods in the nanling belt, South China10.1007/s12665-014-3385-4 ↗
31. Cardiogenic oscillations extraction in inductive plethysmography: Ensemble empirical mode decomposition
32. Multi-scale inversion of density structure from gravity anomalies in Tarim Basin10.1007/s11430-011-4169-2 ↗
33. Preferential filtering for gravity anomaly separation10.1016/j.cageo.2012.09.012 ↗
34. A Complete Ensemble Empirical Mode Decomposition with Adaptive Noise
35. R. K. Mcconnell, Method of and apparatus for pattern recognition, U.S. patent, 1986.
36. Optimal feature selection for support vector machines10.1016/j.patcog.2009.09.003 ↗
37. Feature selection for text classification with Naïve Bayes10.1016/j.eswa.2008.06.054 ↗
38. Feature subset selection in large dimensionality domains10.1016/j.patcog.2009.06.009 ↗