Javascript must be enabled to continue!
A novel polarity correction method for the waveform stacking location of microseismic events
View through CrossRef
ABSTRACT
Microseismic events play a crucial role in mapping fault and fracture distributions in natural and induced earthquakes. Detecting and localizing microseismic events is challenging due to low signal-to-noise ratios. Waveform stacking imaging location is a practical approach for automatically detecting and localizing microseismic events, assuming that the traveltime-corrected seismic waveforms will stack and enhance coherently. However, coherent stack enhancement is susceptible to polarity reversal caused by the nonexplosive components of the source mechanism, which can lead to an unfocused source image, making it difficult to retrieve the optimal location accurately. In this study, we develop a new polarity correction method to address this issue based on the fact that the instantaneous phase difference between two seismic signals with opposite polarity is ±π. First, the Hilbert transform is applied to the original seismic record to obtain the instantaneous amplitude A(t) and phase φ(t). Then, a new signal is constructed by multiplying A(t) with cos[2φ(t)]. The constructed signals for different receivers have the same polarity; therefore, they can be used to refocus the source image. Furthermore, they preserve positive and negative amplitudes, which contributes to noise suppression. Synthetic tests show that our method can effectively achieve polarity correction and noise suppression, enabling a high-resolution source image. Application to real hydraulic fracturing data demonstrates that our method can detect and locate more microseismic events at the fracturing depths, suggesting its effectiveness and potential advantage in microseismic data processing. Because the polarity correction is performed in the data domain without relying on specific receiver layouts, the method is computationally efficient and could be applied to real-time microseismic monitoring across various sites, such as hydraulic fracturing and volcano monitoring.
Society of Exploration Geophysicists
Title: A novel polarity correction method for the waveform stacking location of microseismic events
Description:
ABSTRACT
Microseismic events play a crucial role in mapping fault and fracture distributions in natural and induced earthquakes.
Detecting and localizing microseismic events is challenging due to low signal-to-noise ratios.
Waveform stacking imaging location is a practical approach for automatically detecting and localizing microseismic events, assuming that the traveltime-corrected seismic waveforms will stack and enhance coherently.
However, coherent stack enhancement is susceptible to polarity reversal caused by the nonexplosive components of the source mechanism, which can lead to an unfocused source image, making it difficult to retrieve the optimal location accurately.
In this study, we develop a new polarity correction method to address this issue based on the fact that the instantaneous phase difference between two seismic signals with opposite polarity is ±π.
First, the Hilbert transform is applied to the original seismic record to obtain the instantaneous amplitude A(t) and phase φ(t).
Then, a new signal is constructed by multiplying A(t) with cos[2φ(t)].
The constructed signals for different receivers have the same polarity; therefore, they can be used to refocus the source image.
Furthermore, they preserve positive and negative amplitudes, which contributes to noise suppression.
Synthetic tests show that our method can effectively achieve polarity correction and noise suppression, enabling a high-resolution source image.
Application to real hydraulic fracturing data demonstrates that our method can detect and locate more microseismic events at the fracturing depths, suggesting its effectiveness and potential advantage in microseismic data processing.
Because the polarity correction is performed in the data domain without relying on specific receiver layouts, the method is computationally efficient and could be applied to real-time microseismic monitoring across various sites, such as hydraulic fracturing and volcano monitoring.
Related Results
Ground Monitoring of Microseismic Based on Low Signal-to-Noise Ratio
Ground Monitoring of Microseismic Based on Low Signal-to-Noise Ratio
At present, the principle, data acquisition, data processing, and/or interpretation of many microseismic monitoring methods around the world are far from the requirements of micros...
Correlation and Interpretation of Microseismic Responses using Pressure Measurements in Offset Observation Wells
Correlation and Interpretation of Microseismic Responses using Pressure Measurements in Offset Observation Wells
Abstract
Interpretation of the microseismic data acquired during hydraulic fracture treatments is based on a variety of techniques that make use of the locations, ti...
Conditional Diffusion Model for Robust 3-D Microseismic Event Localization from Noisy Waveforms
Conditional Diffusion Model for Robust 3-D Microseismic Event Localization from Noisy Waveforms
Locating microseismic events is crucial to monitoring fracking
activities, CO2 injection, and reservoirs in general. However, the
process of locating such events is challenging, es...
Photonic microwave waveform generation based on polarization delay interference
Photonic microwave waveform generation based on polarization delay interference
Techniques for generating microwave waveform such as square or triangle waveform have been a topic of general interest recently. Because they are important for applications in rada...
Sea Surface Height Estimation from Improved Modified, and Decontaminated Sub-Waveform Retracking Methods over Coastal Areas
Sea Surface Height Estimation from Improved Modified, and Decontaminated Sub-Waveform Retracking Methods over Coastal Areas
Coastal zones are challenging areas for sensing by satellite altimeters because reflected signals from non-water surfaces and from calm sea surfaces in small bays and ports inside ...
Hydraulic Fracture Geometry, Morphology, and Parent-Child Interactions: Bakken Case Study
Hydraulic Fracture Geometry, Morphology, and Parent-Child Interactions: Bakken Case Study
Abstract
Until recently, microseismic has been the primary diagnostic for estimating "bulk" or stage-level fracture geometry, including asymmetry due to parent-child...
Critical care nurses' knowledge and attitudes toward using ventilator waveform monitoring to detect patient-ventilator asynchrony: A cross-sectional online survey
Critical care nurses' knowledge and attitudes toward using ventilator waveform monitoring to detect patient-ventilator asynchrony: A cross-sectional online survey
Abstract
Background
Most mechanically ventilated patients will be exposed to some asynchrony with the ventilator. Inability to detect and manage patient-ventilator asynchr...
Research on a microseismic signal picking algorithm based on GTOA clustering
Research on a microseismic signal picking algorithm based on GTOA clustering
Abstract. Clustering is one of the challenging problems in machine learning. Adopting clustering methods for the picking of microseismic signals has emerged as a new approach. Howe...

