Full-waveform Based Microseismic Event Detection and Signal Enhancement: The Subspace Approach

Microseismic monitoring has proven to be an invaluable tool for optimizing hydraulic fracturing stimulations and monitoring reservoir changes. The signal to noise ratio (SNR) of the recorded microseismic data varies enormously from one dataset to another, and it can often be very low especially for...

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Main Authors: Song, Fuxian, Warpinski, Norm R., Toksoz, M. Nafi, Kuleli, Huseyin Sadi
Other Authors: Massachusetts Institute of Technology. Earth Resources Laboratory
Format: Technical Report
Language:en_US
Published: Massachusetts Institute of Technology. Earth Resources Laboratory 2014
Subjects:
Online Access:http://hdl.handle.net/1721.1/90526
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author Song, Fuxian
Warpinski, Norm R.
Toksoz, M. Nafi
Kuleli, Huseyin Sadi
author2 Massachusetts Institute of Technology. Earth Resources Laboratory
author_facet Massachusetts Institute of Technology. Earth Resources Laboratory
Song, Fuxian
Warpinski, Norm R.
Toksoz, M. Nafi
Kuleli, Huseyin Sadi
author_sort Song, Fuxian
collection MIT
description Microseismic monitoring has proven to be an invaluable tool for optimizing hydraulic fracturing stimulations and monitoring reservoir changes. The signal to noise ratio (SNR) of the recorded microseismic data varies enormously from one dataset to another, and it can often be very low especially for surface monitoring scenarios. Moreover, the data are often contaminated by correlated noises such as borehole waves in the downhole monitoring case. These issues pose a significant challenge for microseismic event detection. On the other hand, in the downhole monitoring scenario, the location of microseismic events relies on the accurate polarization analysis of the often weak P-wave to determine the event azimuth. Therefore, enhancing the microseismic signal, especially the low SNR P-wave data, has become an important task. In this study, a statistical approach based on the binary hypothesis test is developed to detect the weak events embedded in high noise. The method constructs a vector space, known as the signal subspace, from previously detected events to represent similar, yet significantly variable microseismic signals from specific source regions. Empirical procedures are presented for building the signal subspace from clusters of events. The distribution of the detection statistics is analyzed to determine the parameters of the subspace detector including the signal subspace dimension and detection threshold. The effect of correlated noise is corrected in the statistical analysis. The subspace design and detection approach is illustrated on a dual-array hydrofracture monitoring dataset. The comparison between the subspace approach, array correlation method, and array short-time average/long-time average (STA/ LTA) detector is performed on the data from the far monitoring well. It is shown that, at the same expected false alarm rate, the subspace detector gives fewer false alarms than the array STA/LTA detector and more event detections than the array correlation detector. The additionally detected events from the subspace detector are further validated using the data from the nearby monitoring well. The comparison demonstrates the potential benefit of using the subspace approach to improve the microseismic viewing distance. Following event detection, a novel method based on subspace projection is proposed to enhance weak microseismic signals. Examples on field data are presented indicating the effectiveness of this subspace-projection-based signal enhancement procedure.
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spelling mit-1721.1/905262019-04-12T22:15:05Z Full-waveform Based Microseismic Event Detection and Signal Enhancement: The Subspace Approach Song, Fuxian Warpinski, Norm R. Toksoz, M. Nafi Kuleli, Huseyin Sadi Massachusetts Institute of Technology. Earth Resources Laboratory Microseismic Inversion Microseismic monitoring has proven to be an invaluable tool for optimizing hydraulic fracturing stimulations and monitoring reservoir changes. The signal to noise ratio (SNR) of the recorded microseismic data varies enormously from one dataset to another, and it can often be very low especially for surface monitoring scenarios. Moreover, the data are often contaminated by correlated noises such as borehole waves in the downhole monitoring case. These issues pose a significant challenge for microseismic event detection. On the other hand, in the downhole monitoring scenario, the location of microseismic events relies on the accurate polarization analysis of the often weak P-wave to determine the event azimuth. Therefore, enhancing the microseismic signal, especially the low SNR P-wave data, has become an important task. In this study, a statistical approach based on the binary hypothesis test is developed to detect the weak events embedded in high noise. The method constructs a vector space, known as the signal subspace, from previously detected events to represent similar, yet significantly variable microseismic signals from specific source regions. Empirical procedures are presented for building the signal subspace from clusters of events. The distribution of the detection statistics is analyzed to determine the parameters of the subspace detector including the signal subspace dimension and detection threshold. The effect of correlated noise is corrected in the statistical analysis. The subspace design and detection approach is illustrated on a dual-array hydrofracture monitoring dataset. The comparison between the subspace approach, array correlation method, and array short-time average/long-time average (STA/ LTA) detector is performed on the data from the far monitoring well. It is shown that, at the same expected false alarm rate, the subspace detector gives fewer false alarms than the array STA/LTA detector and more event detections than the array correlation detector. The additionally detected events from the subspace detector are further validated using the data from the nearby monitoring well. The comparison demonstrates the potential benefit of using the subspace approach to improve the microseismic viewing distance. Following event detection, a novel method based on subspace projection is proposed to enhance weak microseismic signals. Examples on field data are presented indicating the effectiveness of this subspace-projection-based signal enhancement procedure. Halliburton Company 2014-10-02T14:30:32Z 2014-10-02T14:30:32Z 2013 Technical Report http://hdl.handle.net/1721.1/90526 en_US Earth Resources Laboratory Industry Consortia Annual Report;2013-19 application/pdf Massachusetts Institute of Technology. Earth Resources Laboratory
spellingShingle Microseismic
Inversion
Song, Fuxian
Warpinski, Norm R.
Toksoz, M. Nafi
Kuleli, Huseyin Sadi
Full-waveform Based Microseismic Event Detection and Signal Enhancement: The Subspace Approach
title Full-waveform Based Microseismic Event Detection and Signal Enhancement: The Subspace Approach
title_full Full-waveform Based Microseismic Event Detection and Signal Enhancement: The Subspace Approach
title_fullStr Full-waveform Based Microseismic Event Detection and Signal Enhancement: The Subspace Approach
title_full_unstemmed Full-waveform Based Microseismic Event Detection and Signal Enhancement: The Subspace Approach
title_short Full-waveform Based Microseismic Event Detection and Signal Enhancement: The Subspace Approach
title_sort full waveform based microseismic event detection and signal enhancement the subspace approach
topic Microseismic
Inversion
url http://hdl.handle.net/1721.1/90526
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AT kulelihuseyinsadi fullwaveformbasedmicroseismiceventdetectionandsignalenhancementthesubspaceapproach