Hi everyone,
we're often using FEFLOW to estimate groundwater inflow and drawdown related to excavations in fractured bedrock (eg.: tunnels). To do so, we use hydraulic conductivity values obtained from packer tests and/or long duration pump tests.
Often, our groundwater inflow estimates are used to guide contractors in pump selection. The long term steady-state estimates from numerical might be OK.
However, such estimates probably represent significant underestimate of the initial heading inflow rate coming from narrow zones of higher permeability that contractors may have to deal with.
Now, the actual question. How do you deal with the initial heading inflow rate estimates? Is this the kind of estimate we should try to derive from numerical modelling? Do the the progressive excavation schedule (and geometry) of the excavations and discrete nature of fractures prevent us to provide realistic and timely estimates of these transient groundwater infiltration?
Are Heuer-like empirical equations the best approach for flush flow estimates?
Any thoughts greatly welcome.
Best regards,
Thomas