Abstract

The automatic location of the microseismic source is still a challenging endeavor in the microseismic field. Due to the complexity of the mining environment, the microseismic records collected by different channels vary, and generally have a low signal-to-noise ratio (SNR). Therefore, the automatic location algorithm is required to be robust and accurate. For microseismic records with low SNR, the stack-based method does not need to pick arrival, thus avoiding the large location error caused by picking arrival. However, the traditional stack-based method does not consider the influence of the waveform quality of different stations, which can bring some errors to the location result. In this paper, in order to improve the location accuracy of the traditional stack-based method, we propose a method for weighted STA/LTA traces stacking. First, we established evaluation indicators of waveform quality based on microseismic records. Then, the STA/LTA traces are given weight to stack according to the evaluation indicators. Finally, the maximum value of the stacking function is solved in the four-dimensional space to obtain the source coordinates. In the process of calculation, we use the weighted differential evolution (WDE) optimal algorithm instead of the full grid search method, which greatly improves the calculation efficiency. The blasting experiment and engineering application show that the proposed method is stable and effective, and the location accuracy is higher than the traditional stack-based method and the arrival-based method.

Highlights

  • In recent decades, microseismic monitoring technology has been widely used to reduce casualties and ensure safety in mining engineering [1,2,3,4,5]

  • There are a lot of different types of noise in microseismic signals collected in mining

  • short-time average to long-time average ratio (STA/LTA) is a classic algorithm for arrival picking, so we use the average value of the amplitude after STA/LTA normalization to represent the apparent degree of the P-wave first arrival

Read more

Summary

Introduction

Microseismic monitoring technology has been widely used to reduce casualties and ensure safety in mining engineering [1,2,3,4,5]. The microseismic records are the basis of the source location. Geiger proposed a location method in the early 20th century [8]. The Geiger method first needs to solve the partial derivative and inverse matrix of the arrival time function, and derive the iterative formula. Many scholars combine the Geiger method with other methods to improve the accuracy of the location. In 2000, Waldhauser and Ellsworth [11] developed a double-difference (DD) location method that is currently widely used for seismic source location. On this basis, Zhang [12] developed double-difference tomography, relocation, and simultaneous correction of velocity models

Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call