Journal
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING
Volume 60, Issue -, Pages -Publisher
IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
DOI: 10.1109/TGRS.2021.3098054
Keywords
Stress; Coal; Receivers; Rocks; Seismic waves; Layout; Tomography; Categorical assessment; comparative analysis; influence factor; seismic tomography; stress field; underground panel
Categories
Funding
- National Natural Science Foundation of China [41774128, 41704115]
- National Key Research Project of China [2018YFB0605601]
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This study conducted a comparative experiment to discuss the detectability and influencing factors of heterogeneous stress field distributions in underground coal mines in North China. The results showed that curvature variations and mined-out voids are the dominant factors affecting the uneven distribution of stress fields in coal mine panels.
A comparative experiment was carried out to discuss the detectability and influence factors on heterogeneous distributions of the stress field for underground panels in North China. The panels are situated in the center and the eastern margin of the North China plate, having similar layouts and stress states. Seismic surveys were performed before coal extractions, and travel-time topographies for refracted P-waves from stiff roofs were computed with a ray-based inversion. The tomographic distributions of P-wave velocity were interpreted by a K-means clustering to categorize the stress fields. The estimated high-stress anomalies show strong correlations with the monitored dynamic roof ruptures and high-energy microseisms. Besides, the relationship among high-stress areas, geological factors, and mined-out voids is also discussed through feature comparisons, Monte-Carlo simulations, and point process statistics. Our results show that the curvature variations and the mined-out voids are dominant factors that affect the heterogeneous distribution of the stress field in the panels. However, the leading causes of the curvature variations in the small-scale panels are different, but they do follow the large-scale regional patterns of the geological regime.
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