Although previous work suggests that a volume of
water running through a water turbine would generate
more voltage than the same volume of water impacting
a piezoelectric sensor in drop form, we found that the
average voltage produced by each for a 0.2 ml (one
drop) volume was similar. The average amount of voltage
generated for each was so similar in fact that there was
only a 0.03 difference between the two methods, and so
it can be said that neither method is better for harnessing
water’s kinetic energy based solely on the voltage output.
The average voltage produced by the hydroelectric
turbine was 2.35 μV, whereas the drops impacting the
piezoelectric turbine averaged a voltage of 2.38 μV.
The data generated from the trials showed no
significant difference between the voltage outputs
between the two systems. It is possible that this lack of
a greater voltage being produced by the turbine over the
piezoelectric film was caused by a design flaw or lack
of consideration for the difference in complexity of the
two separate experiments. The turbine system is notably
more mechanically complex than the piezoelectric
system, which involved only a sensor and an impact.
The difference in electrical complexity between the two
systems could account for some of the difference in
voltage generated. With the turbine, much of the voltage
generated could have been lost through friction before
it was measured, or some of the volume of water may
not have ever contributed to the spinning of the turbine
and therefore the generating of voltage, which would
result in a loss of voltage. The electrical and mechanical
complexity of the turbine system is created by the
additional resistors that could have been implemented
during the trials. If the resistors were in use, they
would have caused less voltage generation. It is likely
this difference in complexity and therefore, efficiency,
between the two systems that accounts for a large
portion of the difference in voltage outputs recorded
here.
Following the trials (15 trials for the turbine and 35
for the piezo), it seemed to be clear that the amount of voltage produced by the raindrops hitting the
piezoelectric sensor was equal to the voltage produced
by water running through the hydroelectric turbine.
Though it was promising that the drop system performed
in a comparable manner to the flow system, it was also
troubling because it countered previous findings. This
conundrum led us to reexamine the experiment in search
of possible errors and to investigate what it would take to
implement this system on a large scale.
It seems that several errors may have contributed
to the results shown here. These include the lack of a
consistent flow rate for the turbine trial, as we had no
means of controlling flow rate. By neglecting the flow rate
in each trial, the results became distorted and therefore
do not honestly reflect the actual voltage output of that
system. In order to prevent this error if further testing
were to occur, a component might be purchased to
control or measure flow rate in order to keep it consistent
throughout. It was also noted that due to the lack of a
consistent flow rate, the comparison between the two
systems’ output is also skewed as it is based on an
“effective drop volume,” which relies on the assumption
that the kinetic energy of the water used in each system
is the same, which had not been proven before testing
occurred.
Another possible source of error was in neglecting
to test the water drop system with differently modeled
piezoelectric sensors. Based on their size and structure,
different piezoelectric sensors may register impact, and
generate voltage differently. By neglecting to take this
fact into account, the results may not convey the furthest
extent that the piezoelectric sensors can perform in
terms of generating the greatest amount of voltage
possible.
If this research were to continue, we would work to
limit the errors mentioned previously in order to make
the data comparison more controlled. As a continuation
of this work, it would be interesting to investigate the
other physical forms of water that have natural potential
to kinetic energy, like snow flakes falling, and compare
the amount of voltage they could produce from impact or
some other method using only their kinetic energy.
As with all small-scale experiments, this experiment had to confront the issue of scaling. If the piezoelectric
system, in particular, was ever to be implemented in
real world applications as a way of producing electrical
energy, it would have to be both cost effective and
functional, among other necessary criteria. In order
to demonstrate that this system is cost effective, we
employed a theoretical model system, the football field
in Gillette Stadium in Foxborough, Massachusetts.
Using the standard measurements of a football field,
we calculated the area of the field to be 5351.2151 m2.
Based on this information, we calculated the number
of each of our systems that could fit on that surface
area. We found that 138,239.9999 of the turbines, and
7,170,903.597 of the piezoelectric sensors could fit on
the field. Knowing this, we calculated that, based on the
information gathered from our trials and data regarding
the average rainfall in Foxborough, Massachusetts
over the past thirty years , the hydroelectric turbines
would produce 1,305,872.063 V as compared to the
68,604,070.57 V produced by the piezos. When that is
taken into account and coupled with the cost of each
component (that is, one whole hydroelectric turbine as
purchased and one piezoelectric sensor as purchased)
we found that generating one volt would cost $1.04 using
the hydroelectric turbine field, but only $0.31 using the
piezoelectric field. This is, of course, not proper scaling,
and much more is involved in properly doing so, but
based on this simplistic attempt at scaling this system,
it appears that the piezoelectric sensor system is more
cost effective than the turbine system which, in and of
itself, would seem to say that piezoelectric sensors are
worth investigating further as a source of renewable
energy.