Microseismic signal of a spring gravimeter

2007 ◽  
Vol 50 (3) ◽  
pp. 302-307 ◽  
Author(s):  
V. P. Dedov ◽  
V. M. Dorokhin ◽  
A. I. Kalenitskii ◽  
B. P. Filimonov
2013 ◽  
Vol 846-847 ◽  
pp. 531-534
Author(s):  
Fan Gyan Bai ◽  
Ming San Ouyang

A new type of mine microseismic monitoring is introduced. The microseismic signal by these downhole sensors collecting, through the differential amplification circuit and filter processing circuit, enhance the potential to voltage A/D conversion chip required. The conversion result is read by ARM controller. The controller processes those data using wavelet denoising, and uses the Ethernet control circuit using TCP/IP protocol transmitte themto the PC. On the trap circuit, Butterworth low-pass filter circuit, wavelet threshold denoising have been simulated, the experimental results basically reached the design requirements.


2018 ◽  
Vol 66 (5) ◽  
pp. 945-957 ◽  
Author(s):  
Ruiqing Hu ◽  
Yanchun Wang

2020 ◽  
Vol 10 (18) ◽  
pp. 6621
Author(s):  
Hang Zhang ◽  
Chunchi Ma ◽  
Veronica Pazzi ◽  
Yulin Zou ◽  
Nicola Casagli

Denoising methods are a highly desired component of signal processing, and they can separate the signal of interest from noise to improve the subsequent signal analyses. In this paper, an advanced denoising method based on a fully convolutional encoder–decoder neural network is proposed. The method simultaneously learns the sparse features in the time–frequency domain, and the mask-related mapping function for signal separation. The results show that the proposed method has an impressive performance on denoising microseismic signals containing various types and intensities of noise. Furthermore, the method works well even when a similar frequency band is shared between the microseismic signals and the noises. The proposed method, compared to the existing methods, significantly improves the signal–noise ratio thanks to minor changes of the microseismic signal (less distortion in the waveform). Additionally, the proposed methods preserve the shape and amplitude characteristics so that it allows better recovery of the real waveform. This method is exceedingly useful for the automatic processing of the microseismic signal. Further, it has excellent potential to be extended to the study of exploration seismology and earthquakes.


2020 ◽  
Vol 177 (12) ◽  
pp. 5781-5797
Author(s):  
Hang Zhang ◽  
Chunchi Ma ◽  
Veronica Pazzi ◽  
Tianbin Li ◽  
Nicola Casagli

2020 ◽  
Author(s):  
Hang Zhang ◽  
Chunchi Ma ◽  
Yupeng Jiang ◽  
Veronica Pazzi ◽  
Nicola Casagli

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