Electrical response and dynamic monitoring of overburden failure in thin bedrock working face
ZHANG Jun
LIU Shengdong
YANG Cai
CHEN Ge
FANG Jinwei
DONG Ya
Abstract:Coal seam mining under thin bedrock with thick unconsolidated layers can lead to hydraulic connections between the working face and the overlying unconsolidated aquifer,potentially inducing water inrush and sand outburst disasters that severely threaten mine safety.Therefore,accurately characterizing the development of overburden failure is crucial.Using the 16041 working face in the Jiaozuo mining area of Henan Province as a case study,we combined numer-ical mining dynamics simulation,physical modeling with electrical similarity,and field monitoring to investigate the elec-trical response characteristics and dynamic monitoring techniques for overburden failure in thin-bedrock working faces.Both the numerical and physical modeling results clearly revealed the development patterns and typical electrical response characteristics of the caved zone and water-conducting fracture zone.During field monitoring,we utilized underground three-dimensional parallel electrical methods to determine the spatial distribution of bedrock thickness,which guided the layout of monitoring boreholes.We then applied a remote parallel electrical monitoring system to synchronously acquire both active and passive geo-electrical parameters.To overcome poor borehole formation and insufficient monitoring height near the bedrock interface,we developed a resistivity variation based dynamic imaging technique integrated with advanced detection.This method extended the effective monitoring height to 75 m,overcame the physical blind zone of the boreholes,and enabled cross-validation through full-space inversion.Field monitoring showed that the caving zone be-came compacted and stabilized during the mid-mining stage,with a measured height of approximately 18.5 m,terminat-ing within the sandy mudstone above the No.21 coal seam roof.The water-conducting fracture zone continued to propag-ate upward during the late mining stage,reaching a maximum height of 46 m,penetrating the entire thin bedrock layer and extending to the base of the Quaternary clay layer,potentially forming a direct water inrush pathway.The electrical re-sponse analysis indicates a distinct staged evolution during overburden failure:pre-mining damage caused an overall in-crease in apparent resistivity;the strong disturbance zone,corresponding to the caving zone,showed the largest resistivity variation and mid-term stability;the weak disturbance zone,corresponding to the water-conducting fracture zone,exhib-ited smaller resistivity variations but a clearly defined range and late-stage stabilization.These results are consistent with the staged overburden evolution characterized by mid-term compaction of the caving zone and late-stage upward expan-sion of the fracture zone.We developed an integrated monitoring approach combining pre-mining static detection,using three-dimensional electrical methods to determine bedrock thickness,with mid-mining dynamic monitoring,employing advanced borehole probing to extend beyond blind zones.This approach addresses the challenges of overburden failure monitoring in thin-bedrock working faces.Field application demonstrated that the method can accurately reveal the devel-opmental height and spatial morphology of the caving zone and the water-conducting fracture zone,and support the as-sessment of potential water inrush risks,providing key technical guidance for water hazard prevention and safe mining in coal mines under similar hydrogeological conditions in East China.
Keywords:thin bedrock with thick unconsolidated layersoverburden failureelectrical responsedynamic monitoringwater-sand inrush risk
Publication Date:2025-11-30
Online Publishing Date:2025-12-19(First online date of this platform, not the publication date of the document)
Pages:14( 5068-5081 )
