aeronautic

The flame

From what it burns to what the eye sees.

What the flame radiates follows from what it burns: Debnath et al.'s Eq. 1, I = ṁ Hc F ε / 4π, measured for MTV1 as one number, 179 W s/(sr g) between 1.8 and 2.6 µm, a seeker's band. Over the burn it radiates 179 J/sr in that band for each gram, 45 kJ/sr in all.

That is in the infrared. The flame's temperature carries it to the eye. An MTV flame is 2000 to 2200 K, emissivity about 0.95: as a graybody at 2100 K, its luminance over its radiance in the band is the candela each W/sr of the band brings. The band's intensity over its radiance is the flame's area, a disc about 60 cm across as it lights.

So an MJU-7 is about 250,000 cd as it lights, and fades as its grain shrinks. Its colour is the Planckian locus's at 2100 K, a warm white.

The graybody is checked against the old candela: a blackbody at platinum's freezing point, 2042 K, was 60 cd/cm², and the integral over the CIE photopic curve gives that.

In the airstream

Static tests measure the flame still. Thrown at hundreds of metres a second, the airstream sweeps its hot products off the grain before they have radiated, and cools them: the flame at the grain gives less, and what was swept off glows on behind it as a trail.

Radiating competes with being carried off, at a rate that grows with the speed through the air, so the share left at the grain is 1 / (1 + v / v½). The trail gives part of the rest, its light falling off by e every v × τ metres as the products cool, so it is long at release and shrinks as the flare slows:

atat the graintrail's e-fold
250 m/s, released38 %12.5 m
60 m/s, after 1 s71 %3 m
20 m/s, falling88 %1 m

The form is the physics'; the numbers are estimates. No measured curve of an MTV flare's intensity against airspeed is published openly, so v½ is 150 m/s, τ is 0.05 s, about how long micron-sized oxide stays white-hot in cold air, and the trail gives half of what is swept off. All three are dials on flare: halfLightMPerS, glowTimeS, trailShare.

What carries the products off is the air's mass flux, ρ v, not its speed: v½ is sea level's, and grows as the air thins. At 250 m/s the grain keeps 37 % of its light at sea level, 53 % at 6 km and 70 % at 12 km.

Higher up

MTV's burn rate goes with the pressure to a small power: r = 9.39 p^0.094 mm/s, p in MPa, from strand-burner tests between 0.15 and 1.15 MPa (Nihon University). The flare's rate is sea level's, and thinner air slows it, so it burns longer:

altitudepressureburns
0101 kPa2.93 s
1 km90 kPa2.96 s
6 km47 kPa3.15 s
12 km19 kPa3.42 s

Its light a second is what it burns a second, so it is that much dimmer for that much longer. The dial is pressureExponent.

Lighting

The cartridge's impulse cartridge fires the flare out, and its igniter lights the grain a moment later: it leaves dark and lights a few metres behind. No figure for the MJU-7 is published openly; 0.1 s is an estimate, ignitionDelayS.

The trail cooling

The swept products cool as they go, and redden. Where the trail's light has fallen by e^-f, they are as hot as a graybody whose luminance has, so the trail is drawn in that one's colour: 2100 K at the grain, about 1700 K three e-folds back.

Left out

  • Altitude and the flame's temperature: thinner air feeds the flame's afterburning in the air less. It is drawn at 2100 K at every altitude.

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