A transient poroelastic formulation based on the Biot consolidation th
eory is presented to study the impact of underground longwall mining o
f coal on strata deformation and the subsequent modification of hydrog
eological properties. A finite-element model is used where the geometr
ic conditions may be complex. The important parameters in this model a
re identified as pore pressure ratio, alpha1 and relative compressibil
ity, alpha2 with the latter exerting far greater influence on the resu
lting fluid pressure field than the former. This study indicates that
the fluid pressure distribution is strongly controlled by the stress d
istribution, or the strata deformation induced by mining has a great i
mpact on the change in hydrogeological environment in the mining regio
n.