The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences
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Articles | Volume XLI-B8
Int. Arch. Photogramm. Remote Sens. Spatial Inf. Sci., XLI-B8, 449–452, 2016
https://doi.org/10.5194/isprs-archives-XLI-B8-449-2016
Int. Arch. Photogramm. Remote Sens. Spatial Inf. Sci., XLI-B8, 449–452, 2016
https://doi.org/10.5194/isprs-archives-XLI-B8-449-2016

  23 Jun 2016

23 Jun 2016

ANOMALY IDENTIFICATION FROM SUPER-LOW FREQUENCY ELECTROMAGNETIC DATA FOR THE COALBED METHANE DETECTION

S. S. Zhao, N. Wang, J. Hui, X. Ye, and Q. Qin S. S. Zhao et al.
  • Institute of Remote Sensing and Geographic Information System, School of Earth and Space Sciences, Peking University, Beijing, China

Keywords: Electromagnetic, Super Low Frequency, Coalbed Methane, non-Gaussian, Class B model, Least Square Gradient, Adaptive filter

Abstract. Natural source Super Low Frequency(SLF) electromagnetic prospecting methods have become an increasingly promising way in the resource detection. The capacity estimation of the reservoirs is of great importance to evaluate their exploitation potency. In this paper, we built a signal-estimate model for SLF electromagnetic signal and processed the monitored data with adaptive filter. The non-normal distribution test showed that the distribution of the signal was obviously different from Gaussian probability distribution, and Class B instantaneous amplitude probability model can well describe the statistical properties of SLF electromagnetic data. The Class B model parameter estimation is very complicated because its kernel function is confluent hypergeometric function. The parameters of the model were estimated based on property spectral function using Least Square Gradient Method(LSGM). The simulation of this estimation method was carried out, and the results of simulation demonstrated that the LGSM estimation method can reflect important information of the Class B signal model, of which the Gaussian component was considered to be the systematic noise and random noise, and the Intermediate Event Component was considered to be the background ground and human activity noise. Then the observation data was processed using adaptive noise cancellation filter. With the noise components subtracted out adaptively, the remaining part is the signal of interest, i.e., the anomaly information. It was considered to be relevant to the reservoir position of the coalbed methane stratum.