
As most of the energy sources,
hydropower origins from the sun’s
energy radiated on earth.
By processes of evaporation,
(wind)transport and precipitation on an elevated area, water
in this area has obtained potential energy. This potential energy
accounts Spot = mgh,
where h is the height difference compared
to sea level (other symbols see end of section).
NORMAL RIVERFLOW
While streaming downward (runoff), this potential energy, converts
gradually to pressure energy (water submerged under the water
surface) and velocity energy (E = mgh + mp/p + $mv2j. In a river
the pressure energy (mp/p) remains quite constant like the water
depth does, except when, for example,
a reservoir or lake is con-
cerned. Also the velocity energy (fmv2) remains nearly constant.
While the water streams down the release of energy by the decrease
of potential energy (mgh by lowering h) is comnletely absorbed
by friction between water particles and between water and riverbed,
producing heat.
This hardly measurable increase of temperature
then is transmitted to the surrounding, and, is lost.
ENERGY OUT OF HEADS
To adapt energy from water either potential, pressure, velocity
or combined energy may be drawn on. In the process of adapting,
however, also energy conversions from one feature to an other
may occur. To visualize the type of energy, the presented formula
can be divided by mg : e = h + p/og + v2/2g, where e is now the
energy of water per unity of weight, and is expressed in meters,
while the right hand terms are head, pressure head and velocity
head respectively.
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