There are four generating
methods on hydroelectricity to generates power.
Most hydroelectric power comes from the potential energy of
dammed water driving a water turbine and generator. The power extracted from
the water depends on the volume and on the difference in height between the
source and the water's outflow. This height difference is called the head. The
amount of potential energy in water is proportional to the head. To deliver
water to a turbine while maintaining pressure arising from the head, a large
pipe called a penstock may be used.
This method produces
electricity to supply high peak demands by moving water between reservoirs at
different elevations. At times of low electrical demand, excess generation
capacity is used to pump water into the higher reservoir. When there is higher
demand, water is released back into the lower reservoir through a turbine.
Pumped-storage schemes currently provide the most commercially important means
of large-scale grid energy storage and improve the daily capacity factor of the
generation system.
Run-of-the-river
hydroelectric stations are those with smaller reservoir capacities, thus making
it impossible to store water.
A tidal power plant makes use
of the daily rise and fall of water due to tides; such sources are highly
predictable, and if conditions permit construction of reservoirs, can also be
dispatchable to generate power during high demand periods. Less common types of
hydro schemes use water's kinetic energy or undammed sources such as undershot
waterwheels.