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Vaporization of JP-8 Jet Fuel in a Simulated Aircraft Fuel Tank ...

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pump that could draw samples from altitudes as high as 35,000 feet. However, when<br />

sampl<strong>in</strong>g from altitudes lower than 35,000 feet, the pump would draw more than the<br />

necessary amount required by the FID, which would just be wasted by dump<strong>in</strong>g <strong>in</strong>to the<br />

laboratory air. Also, by draw<strong>in</strong>g a cont<strong>in</strong>uous sample at a high flow rate, hydrocarbon-<br />

free air would be drawn <strong>in</strong> to the ullage through the vents, which would dilute the sample<br />

and cause the FID read<strong>in</strong>gs to be false. It was for these reasons that an <strong>in</strong>termittent<br />

sampl<strong>in</strong>g method was devised for tests to be performed at sub-atmospheric pressures.<br />

The FID had a very high response time <strong>of</strong> 0.2 seconds, so a sample time <strong>of</strong> 30 seconds<br />

every ten m<strong>in</strong>utes was agreed upon tak<strong>in</strong>g <strong>in</strong>to consideration the analyzer response time,<br />

the flow rate <strong>of</strong> the sample pump and the length <strong>of</strong> the sample l<strong>in</strong>es.<br />

4.2 Flight Pr<strong>of</strong>iles<br />

A flight pr<strong>of</strong>ile is the temporal pressure and temperature variation for the duration <strong>of</strong> the<br />

test. Before a flight pr<strong>of</strong>ile test was run the fuel was loaded <strong>in</strong>to the tank and allowed to<br />

equilibrate. A flight scenario was created that simulated an airplane on the ground for<br />

about an hour at ambient sea level temperature and pressure with heat<strong>in</strong>g <strong>of</strong> the fuel tank<br />

to about 30°F above the <strong>in</strong>itial liquid temperature. Quasi-steady equilibrium was atta<strong>in</strong>ed<br />

after about an hour, then the airplane began ascent at 1,000 feet per m<strong>in</strong>ute until the<br />

cruis<strong>in</strong>g altitude was reached. The airplane would cruise at altitude for an hour then<br />

beg<strong>in</strong> decent at –1,000 feet per m<strong>in</strong>ute. The test was complete after the airplane was back<br />

on the ground. Ambient temperatures at high altitudes were obta<strong>in</strong>ed from Unisys<br />

weather constant height plots. Ambient temperatures <strong>of</strong> 20°F, -10°F, and -50°F were<br />

used at altitudes <strong>of</strong> 10,000 feet, 20,000 feet, and 30,000 feet, respectively. A l<strong>in</strong>ear<br />

30

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