This transformative presentation takes 10 minutes -- or
less. It was ahead of its time over 20
years ago and it still is.
This paper is Nukiyama in microscale over the pressure
range from 200 to 6000 PSI. Nukiyama
used a platinum wire simultaneously as a heat transfer element and a resistance
thermometer.
Here is my Nukiyama element: diameter 7.5 microns, length
1.15 millimeters.
It is installed in the lower end of an upright tube that is filled with pressurized water, pure and degasified at about 20 Centigrade. The steel tube is used for these pool boiling runs at higher pressures.
The benchtop apparatus has the pool boiling tube, the
pressurizing pump, the junction box and programmed power supply, a PC with
Excel for data logging, and in the back, a Rosemount recording pressure
transducer.
A run takes about 11 seconds and data is recorded every
tenth of a second. Heat flux is smoothly
increased and then decreased. In this
run at 1000 PSI with the water at about 20 Centigrade, the peak was over 4000
Watts per square centimeter. The average
power is about one half watt, so the energy is about 6 watt-seconds, or less
than two calories for the 11 second run.
So, the temperature of a local gram of water increases by less than two
Centigrade.
Following is the reduced data for the 1000 PSI run. It doesn’t get any better than this although
it gets more exciting. The transition to
phase change, I call it the Nukiyama point, is at about 2100 watts per square
centimeter. This transition is extremely
sharp, there is no sluggishness. That is
also the case at the turnaround at 4100.
I want to increase the recording rate to every millisecond in further
runs. Note that the return is on the
same path as the rise. Clearly, the
local temperature stays very close to 20 Centigrade, otherwise the return would
not overlay.
Here are several runs, three subcritical, one
transcritical, and four supercritical. You have seen the dissection of the 1000
psi run; the 200 and 2500 of this plot are similar. The dotted line is the transcritical run at
3000. The four supercritical runs range
from 3600 to 6000.
Here are the 3600 and 6000 runs. The 6000 has a narrower spread between the
power up and the power down.
The 3,000 transcritical run is superimposed on the runs
you have just seen. I want to expand
this territory with runs having millisecond data collection.
The supercritical runs are all well-behaved in this
plot. Even the transcritical falls in
its proper place.
The point of the following plot of the subcritical runs is that at
200 psi the Nukiyama point is 65 Centigrade beyond saturation while at 2500 and
above, that delta T is very narrow.
With the permission of Professor Victor Yagov of Moscow, following
is his recent analysis. At 200 psi he reports substantial Delta T’s, at 3000,
the Delta T’s are vanishing. Multiply Yagov’s
values by 100 to get to my units.
This is the transcritical run. Again, I want millisecond data recording next
time in the search for the aspects of the jump.
Note that saturation temperature is very close to critical.
Here is limited data.
With a somewhat larger microscale element the heat fluxes at the
Nukiyama points are reduced, however the temperature of the points is
unchanged. The transcritical
characteristic is the same even though the pressure is 100 psi less; the
saturation temperature is still very near critical.
I think this is sensational. The procedure is to pressurize the apparatus
to about 6000 psi, apply a substantial heat flux in one step, and maintain that
heat flux as pressure is smoothly reduced over about 20 seconds, turn off power
at about 200 psi. Note the gradual
increase in temperature as pressure is reduced, then the upward jump of over
200 Centigrade at around 3700 psi, followed by a smooth increase of another 100
Centigrade to the critical pressure, then a smooth decrease of nearly 200
Centigrade, then a downward jump of about 150 centigrade to the critical
temperature. At that point the subcritical boiling begins and continues until
the power is turned off. At the lowest heat flux there is a smooth continuous
plot over the entire pressure range with no intervening steps. The four plots
at increasing heat fluxes are neatly nested.
Here are the data points.
I captured one point during the upward jump in two runs. Of course, runs
are needed with millisecond recording, etc.
Here are the plots of subcritical phase change only. The plots are very close; however the heat
fluxes are distinct. As was measured in
the constant pressure runs at subcritical pressures and also calculated by
Professor Yagov, the delta T from phase change to saturation increases as the
pressure is reduced.
This shows the impact of nitrogen saturation at 1000
psi. I never reduced these plots to heat
flux and temperature; I did not need to in order to get the patent. Nitrogen
reduces the heat transfer coefficient during natural circulation; however phase
change heat transfer begins at a somewhat lower temperature and heat flux. I filed this patent during 1995 and it issued
during 1997, the year that Berkeley started its microscale journal.
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