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A New Theoretical Method to Predict Strata Movement and Surface Subsidence due to Inclined Coal Seam Mining

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Abstract

The mining-induced strata movement and surface subsidence are closely related to the dip angle of coal seam. However, most surface subsidence prediction methods are empirical, and only suitable for nearly flat coal seam mining. In this paper, a new theoretical method is proposed to predict the strata movement boundary and surface subsidence caused by inclined coal seam mining, which considers the influence of key strata, rock quality and coal seam dip angle. The strata movement caused by inclined coal seam mining is generalized and described by three models: analogous hyperbola model (AHM), analogous hyperbola-funnel model (AHFM), and analogous funnel model (AFM). Considering the rock quality of roof and floor strata, the rock mass rating system is adopted to calculate the surface maximum subsidence and its location. Additionally, the distinct element method was used to assess the performance of the theoretical models. The numerical simulation results match well with theoretical predictions of strata movement boundary and surface subsidence. It is discovered that the appearance of surface subsidence troughs is obviously asymmetric. As the dip angle increases, the surface maximum subsidence decreases and its location is laterally displaced. When the dip angle is greater than 50°, the double subsidence troughs can be visualized clearly. Furthermore, the theoretical predictions of surface subsidence are verified by field measurements of two cases. As a result, the theoretical predictions of surface subsidence are greatly improved by comparing with the empirical method.

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Abbreviations

E :

Young’s modulus [GPa]

γ :

Volumetric weights [kg/m3]

[σ t]:

Tensile strength [MPa]

c :

Cohesion [MPa]

M :

Thickness of coal seam [m]

h PKS :

Thickness of PKS [m]

L PKS :

Length of broken PKS blocks [m]

H PKS :

Depth of primary key stratum [m]

W s :

Surface subsidence [m]

W max :

Maximum subsidence of PKS [m]

β lower :

Dip angle of lower sliding plane [°]

β upper :

Dip angle of upper sliding plane [°]

θ upper :

Upper goaf angle [°]

θ lower :

Lower goaf angle [°]

β f :

Dip angle of floor sliding plane [°]

S r/f :

Cavity area of roof/floor [m2]

ks:

Shear stiffness [GPa/m]

kn:

Normal stiffness [GPa/m]

U :

Water force acting on sliding plane [kN]

H b :

Strata thickness between PKS and coal seam [m]

η r /f :

Roof/floor convergence factors due to dip angle [-]

κ r /f :

Roof/floor rock mass quality factors [-]

r/f :

Laterally displaced distance of roof/floor maximum subsidence [m]

h :

Thickness of rock layer [m]

L :

Length of broken block [m]

q :

Load on rock layer [kN/m]

φ :

Friction angle [°]

α :

Dip angle of coal seam [°]

H 0 :

Average depth of mining face [m]

d :

Excavation width [m]

W :

Weight of sliding rock masses [kN]

A :

Area of potential sliding plane [m2]

F s :

Safety factor [-]

ρ :

Density [kg/m3]

ψ :

Dilation angle [°]

φ m :

Friction angle of coal seam [°]

θ 0 :

Goaf angle due to horizontal mining [°]

θ r :

Influence transfer angle of roof strata [°]

K p :

Bulking factor [–]

υ :

Poisson’s ratio [–]

q s :

Subsidence coefficient [–]

V :

Water force acting in tension crack [kN]

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Acknowledgements

This study was funded by the Beijing Outstanding Young Scientist Program (BJJWZYJH01201911413037), National Natural Science Foundation of China (Grants No: 52004287; 51622404; 41877257), and Shannxi Coal Group Key Project (2018SMHKJ-A-J-03).

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Correspondence to Jianping Zuo.

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All the authors in this paper declare that they have no confict of interest.

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Sun, Y., Zuo, J., Karakus, M. et al. A New Theoretical Method to Predict Strata Movement and Surface Subsidence due to Inclined Coal Seam Mining. Rock Mech Rock Eng 54, 2723–2740 (2021). https://doi.org/10.1007/s00603-021-02424-z

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  • DOI: https://doi.org/10.1007/s00603-021-02424-z

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