Understanding your instruments and their calibration.
About
ten years ago and near Johannesburg which is up at an altitude of
around 5000ft or 1524m, I came across a recently installed cold
store with dimensions approximately 40m by 20m and designed for
bulk storage of pre-cooled plastic bottled drinks. The complaint
was that this store had never been able to properly maintain the
designed 2°C store temperature except occasionally for very short
periods during some of the cooler mornings; typical mid afternoon
room temperature was seen to be around 4°C. The owner explained
how apparently he understood the refrigeration plant was selected
with a total capacity very closely matching the very accurate load
calculations used by the designer. The refrigeration plant comprised
four MT160 Maneurope condensing units with matching blowers running
on R22 each with a design capacity of 26.1kW. The design saturated
temperatures were -5°C evaporating and 45°C condensing with short
pipe runs having negligible pressure drops.
At the time I felt that observing the refrigeration systems operating
readings as occurring within design cold store and ambient temperatures
would bring me closer to any clues useful. I also wanted to do this
without making any prior adjustments. A hindrance here of course
with this particular site was that the very problem with the system
I was trying to identify would not provide for the coincidence of
design room and ambient temperatures. I had to visit site first
thing in the early morning when it was said the cold store temperature
would briefly be at the designed temperature of 2°C. Then all I
had to do was partially restrict the condensers airflow to raise
the saturated condensing temperature to the designed 45°C. On the
morning I also positioned my airflow restrictor, a swimming towel,
to maintain condenser leaving liquid temperatures above the designed
ambient temperature of 32°C. If I allowed liquid temperatures to
drop nearer the cooler morning ambient temperatures then the resulting
increased refrigerant's net refrigeration capacity would have the
effect of lowering saturated suction pressure since less refrigerant
would be needed in circulation to establish the TEV's superheat
setting.
Now
that I had eliminated liquid pressure, liquid temperature and room
temperature from the list of system performance effecting variables,
I could look to the suction side for clues as to the cause of apparent
performance loss. Of course, we know very well that lower saturated
suction temperatures and higher suction superheats adversely effect
system performance, I only wanted to eliminate them next in a positively
methodical manner before moving on, if moving on was going to be
necessary.
As is routinely done I attached my suction gauge to the evaporator
coil header pressure tapping and my surface temperature probe to
the same header. I found that saturated suction temperature was
nearly 2K below design while suction superheat was about the same
too high. Interestingly, this is to say that the evaporators suction
header surface temperature was in fact at the expected design temperature,
4K above the design saturated evaporating temperature.
At this point while I was asking myself "Why, despite the many
return visits apparently made in an attempt to rectify this problem,
everyone visiting seemed to have overlooked the obvious high TEV
superheat settings found on all four systems?" But within the same
train of thought I remembered that, to the best of my knowledge,
I calibrated my service gauges different to every other technician.
The key was that I adjusted my gauges to compensate for altitude
allowing me to see the lower than required saturated suction temperatures
when others simply could not.
ike every other service engineers system analyser, mine's gauges
used the "Bourdon Tube" principle. Within the gauge a 'C' shaped
tube, the "Bourdon Tube", will tend to open or close its 'C' shape
depending on whether the internal pressure was greater or lesser
than the surrounding (atmospheric) pressure. The problem with this
principle is that it does not automatically compensate for change
in altitude as would say a diaphragm gauge. A bourdon gauge calibrated
to show zero at sea level will still show zero when transported
unadjusted up to 5000ft altitude. However, relative to sea level
the atmospheric pressure at 5000ft is already a partial vacuum of
about 4.95" Mercury. Yet, as already mentioned, every other service
engineer I knew would leave their gauges at the factory calibration
of 0" Mercury vacuum or 0psi atmospheric pressure.
The approximate atmospheric pressure at that altitude is 12.27psi
or 84.6kPa. If atmospheric pressure at sea level would hold a column
of mercury against a vacuum a height of 29.92" or 760mm then at
an altitude of 5000ft atmospheric pressure could only hold that
mercury column 12.27/14.7 x 29.92 = 24.97" or 634mm.
The result of this calibration anomaly was that while the visiting
service engineers thought they were seeing the systems saturated
evaporating temperatures at the designed -5°C in reality I found
the systems operating with saturated evaporating temperatures even
lower than the predicted un-calibrated offset temperature of -6.2°C.
Where the MT160 condensing units had a design rated capacity of
26.1kW at -5°C they were in fact achieving only 24.5kW, approximately
6% less than the accurately predicted design capacity.
Convinced
I understood the reason for this systems underperformance I went
ahead and reduced the four TEV superheat settings by the appropriate
amount. With the resulting increased refrigerant feed increasing
the evaporator duties there was the needed rise in saturated suction
temperature and compressor duties. The subsequent rise in saturated
condensing temperature needed to meet the increased total heat rejection
naturally increased head pressures so that now finally too the valves
were seeing better liquid feed pressures allowing them to better
meet their designed capacities.
Clearly they were not exaggerating when they claimed plant selection
closely matched calculated load.
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