Power can be generated from groundwater by pumping water from one or m
ore bores and passing this discharge to a hydro power station located
at an elevation below the bore water level. Given a suitable hydrogeol
ogical environment, a small groundwater power system should be more ro
bust against dry periods than a stream-based scheme of the same size.
This is relevant, for example, for isolated islands where no single st
ream may provide a sufficiently large and consistent discharge for nor
mal hydropower generation. Large groundwater power schemes may be poss
ible in particular topographic and geological configurations in high-r
ainfall environments. The aquifer here plays the role of a storage lak
e so land inudation can be avoided. Potential groundwater power sites
will have to be evaluated on a case-by-case basis using numerical mode
ls, but simple expressions for preliminary power estimates can be deri
ved for situations where the Dupuit approximation applies.