First Arrival Picking on Microseismic Signals Based on K-Means with a ReliefF Algorithm

被引:6
|
作者
Li, Yijia [1 ]
Wang, Zhengfang [1 ]
Wang, Jing [1 ]
Sui, Qingmei [1 ]
Li, Shufan [2 ]
Wang, Hanpeng [3 ]
Cao, Zhiguo [4 ]
机构
[1] Shandong Univ, Sch Control Sci & Engn, Jinan 250061, Peoples R China
[2] Shandong Univ, Inst Marine Sci & Technol, Qingdao 266237, Peoples R China
[3] Shandong Univ, Sch Qilu Transportat, Jinan 250002, Peoples R China
[4] Natl Energy Investment Grp Corp, Beijing 100021, Peoples R China
来源
SYMMETRY-BASEL | 2021年 / 13卷 / 05期
基金
中国国家自然科学基金;
关键词
microseismic signals; first arrival picking; reliefF algorithm; k-means; TIME-FREQUENCY ANALYSIS; HYDROPOWER STATION; EVENT DETECTION; P-PHASE;
D O I
10.3390/sym13050790
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The quick and accurate picking of the first arrival on microseismic signals is one of the critical processing steps of microseismic monitoring. This study proposed a first arrival picking method for application to microseismic data with a low signal-to-noise ratio (SNR). This approach consisted of two steps: feature selection and clustering. First of all, the optimal feature was searched automatically using the ReliefF algorithm according to the weight distribution of the signal features, and without manual design. On that basis, a k-means clustering method was adopted to classify the microseismic data with symmetry (0-1), and the first arrival times were accurately picked. The proposed method was validated using the synthetic data with different noise levels and real microseismic data. The comparative study results indicated that the proposed method had obviously outperformed the classical STA/LTA and the k-means without feature selection. Finally, the microseismic localization of the first arrivals picked using the various methods were compared. The positioning errors were analyzed using box plots with symmetric effect, and those of the proposed method were the smallest, and stable (all of which were less than 0.5 m), which further verified the superiority of this study's proposed method and its potential in processing complicated microseismic datasets.
引用
收藏
页数:20
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