Xie, J.; Ning, S.; Qu, Q.; Zhu, W.; Zhao, B.; Xu, J. A Carbon Nanocomposite Material Used in the Physical Modelling of the Overburden Subsidence Process. Nanomaterials2023, 13, 2962.
Xie, J.; Ning, S.; Qu, Q.; Zhu, W.; Zhao, B.; Xu, J. A Carbon Nanocomposite Material Used in the Physical Modelling of the Overburden Subsidence Process. Nanomaterials 2023, 13, 2962.
Xie, J.; Ning, S.; Qu, Q.; Zhu, W.; Zhao, B.; Xu, J. A Carbon Nanocomposite Material Used in the Physical Modelling of the Overburden Subsidence Process. Nanomaterials2023, 13, 2962.
Xie, J.; Ning, S.; Qu, Q.; Zhu, W.; Zhao, B.; Xu, J. A Carbon Nanocomposite Material Used in the Physical Modelling of the Overburden Subsidence Process. Nanomaterials 2023, 13, 2962.
Abstract
Carbon nanomaterial is widely used in structural health monitoring due to the advantage of sensitivity and good mechanical properties. This study presents a novel approach employing carbon nanocomposite materials (CNM) to characterize deformation and damage evolution in physical modelling. As the primary measurement method, the CNM is used to investigate the deformation characteristics of a 200-400 m thick sandstone bed at a 1 km deep longwall mine. The sandstone unit is identified as an ultra-thick key stratum (UTKS), with its thicknesses varying across different mining panels of the UTKS. The results of CNM monitoring show that the UTKS remains stable even after a consecutive excavation of 900 m in width. This stability impedes the upward propagation of overlying strata failure, leading to minimal surface subsidence. The study demonstrates the huge potential of CNM in the mining area, which can be useful for investigating material damage in physical modelling studies. The findings suggest that the cumulative extraction width in individual mining areas of the mine should be controlled to avoid a sudden collapse of the UTKS, and that special attention should be paid to where the UTKS's thickness changes substantially. The substantial variation in UTKS thickness significantly impacts the pattern of overburden subsidence.
Copyright:
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