Abstract In order to investigate the distribution patterns of in situ stress in the main coal seams (3# and 15#) of the Qinshui coalfield, an in-depth analysis was conducted on the in situ stress measurement results obtained from 139 measurement points across 46 mines within the mining area. The findings indicate that the maximum horizontal principal stress in the coal mining area of both seams is generally higher than the vertical principal stress. The stress field exhibits characteristics of a tectonic stress field, while deeper regions display features of a vertical stress field. The in situ stress values in the mining area of coal seam 3# are predominantly characterized by moderate stress field zones, while those in the mining area of coal seam 15# are mainly composed of low to moderate stress field zones. The maximum horizontal principal stress in the Yangquan and Changzhi mining areas for both coal Seams 3# and 15# is concentrated in the NE direction, whereas in the Jincheng mining area, it is predominantly concentrated in the NW direction, indicating a clear directionality. With increasing depth, the following trends can be observed approximately: the maximum and minimum horizontal principal stress values generally exhibit an increasing trend, and the geological structures throughout the mining area are primarily dominated by horizontal tectonic movements; the lateral pressure ratio gradually decreases and tends to concentrate near the value of 1; the relative difference between the maximum and minimum principal stresses tends to increase, with the horizontal principal stress difference ratio concentrating near 0.5. The relationship between the average horizontal principal stress ratio (k) and vertical principal stress at different depths within the measured area follows Hawke-Brown’s general law for this relationship curve. The research results have important guiding significance for the design of coal mining engineering in this area.
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