A Deep Learning-Based Denoising Method for Airborne Electromagnetic Data

Airborne electromagnetic (AEM) measurements are vulnerable to mixed environmental noise, and rapid signal decay hampers weak transient recovery. We propose WL-CNN-BiLSTM, integrating dual-stage wavelet filtering, parallel multi-scale convolutions, residual skip connections, bidirectional recurrent units, and a hybrid reconstruction objective for complex TEM waveforms. On the archived 20,000-trace benchmark’s 3000-trace test subset, it achieved an aggregate physical-domain SNR 17.53 dB (RMSE 1.48 × 10−10 T; PCC 0.989), versus 11.49 dB for PC-BiLSTMNet, 11.76 dB for validation-selected Median filtering, and 13.04 dB for VMD; the per-trace SNR P10 was −3.41 dB (minimum −25.45 dB). These archived results characterize stored numerical targets, not independently verified AEM responses. On an independent 1000-trace blind test, a separately trained layered-earth configuration using training-only scalers achieved a median SNR of 5.91 dB versus 0.39 dB (Median) and −0.05 dB (VMD), but poorer lower-tail SNR (P10 −43.93 dB) and a median of NRMSE 7.402 over 101–1001 μs. Proprietary iFTEM-II windows showed waveform changes versus the engineering curve, but unavailable proxy provenance/calibration made this qualitative evidence, not field-accuracy validation. A matched p = 0 comparison, three-seed ablations, complete training-only-scaler retraining, and out-of-distribution diagnostics delineate distributional dependencies; temporal feature weighting is an implemented design component, not a demonstrated late-time enhancer. It shows aggregate reconstruction gains within the benchmark and characterizes dataset- and protocol-dependent limitations.

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Publication Details

Journal
Sensors
Published
2026-11-06
DOI
https://doi.org/10.3390/s26217021
Primary Topic
Geophysical and Geoelectrical Methods
Type
article
Field-Weighted Citation Impact
0.00

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article

A Deep Learning-Based Denoising Method for Airborne Electromagnetic Data

Qingtian Lü, Chong Zhang, Wei Huang, Yuhang Li
3 links
Sensors
Geophysical and Geoelectrical Methods
article

A Deep Learning-Based Denoising Method for Airborne Electromagnetic Data

Qingtian Lü, Chong Zhang, Wei Huang, Yuhang Li
article en

Abstract

Airborne electromagnetic (AEM) measurements are vulnerable to mixed environmental noise, and rapid signal decay hampers weak transient recovery. We propose WL-CNN-BiLSTM, integrating dual-stage wavelet filtering, parallel multi-scale convolutions, residual skip connections, bidirectional recurrent units, and a hybrid reconstruction objective for complex TEM waveforms. On the archived 20,000-trace benchmark’s 3000-trace test subset, it achieved an aggregate physical-domain SNR 17.53 dB (RMSE 1.48 × 10−10 T; PCC 0.989), versus 11.49 dB for PC-BiLSTMNet, 11.76 dB for validation-selected Median filtering, and 13.04 dB for VMD; the per-trace SNR P10 was −3.41 dB (minimum −25.45 dB). These archived results characterize stored numerical targets, not independently verified AEM responses. On an independent 1000-trace blind test, a separately trained layered-earth configuration using training-only scalers achieved a median SNR of 5.91 dB versus 0.39 dB (Median) and −0.05 dB (VMD), but poorer lower-tail SNR (P10 −43.93 dB) and a median of NRMSE 7.402 over 101–1001 μs. Proprietary iFTEM-II windows showed waveform changes versus the engineering curve, but unavailable proxy provenance/calibration made this qualitative evidence, not field-accuracy validation. A matched p = 0 comparison, three-seed ablations, complete training-only-scaler retraining, and out-of-distribution diagnostics delineate distributional dependencies; temporal feature weighting is an implemented design component, not a demonstrated late-time enhancer. It shows aggregate reconstruction gains within the benchmark and characterizes dataset- and protocol-dependent limitations.

SensorsVol. 26(21)
Chinese Academy of Geological Sciences (CN)
National Natural Science Foundation of China, Chinese Academy of Geological Sciences
Openalex Percentile: Top 21%
Geophysical and Geoelectrical Methods
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