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<strong>Determ<strong>in</strong>ation</strong> <strong>of</strong> <strong>Soot</strong> <strong>Volume</strong> <strong>Fraction</strong> <strong>and</strong> <strong>Primary</strong> <strong>Particle</strong> <strong>Size</strong> <strong>in</strong> Lam<strong>in</strong>ar<br />

Non-Premixed Hydrocarbon Flames under Microgravity Us<strong>in</strong>g Laser-Induced<br />

Inc<strong>and</strong>escence<br />

Monika Wendler ∗ , Rol<strong>and</strong> Sommer, <strong>and</strong> Alfred Leipertz<br />

Lehrstuhl für Technische Thermodynamik<br />

Universität Erlangen-Nürnberg<br />

Erlangen, Germany<br />

Abstract<br />

Time-resolved laser-<strong>in</strong>duced <strong>in</strong>c<strong>and</strong>escence (TIRE-LII) has been applied to measure the volume concentration <strong>and</strong><br />

the primary particle sizes <strong>of</strong> soot under different gravity levels dur<strong>in</strong>g parabolic flights. This has been carried out<br />

for lam<strong>in</strong>ar non-premixed ethene <strong>and</strong> methane flames for different fuel flow <strong>and</strong> air co-flow conditions. It could be<br />

shown that there is a strong <strong>in</strong>fluence <strong>of</strong> the amount <strong>of</strong> air co-flow on soot volume concentration but only a m<strong>in</strong>or<br />

<strong>in</strong>fluence on primary particle size under microgravity. This is <strong>in</strong> contrast to normal gravity <strong>and</strong> 1.8 g, <strong>in</strong> which no<br />

<strong>in</strong>fluence <strong>of</strong> the amount <strong>of</strong> co-flow could be found, neither on soot volume concentration nor on primary paricle<br />

size. Under microgravity, <strong>in</strong> ethene flames the primary particle sizes are about double the size <strong>of</strong> those at normal<br />

gravity. Methane flames show all-over smaller primary particle sizes than ethene flames.<br />

Introduction<br />

<strong>Soot</strong> formation is one <strong>of</strong> the most important<br />

processes <strong>in</strong> combustion systems, but it is still not<br />

fully understood [1, 2]. Under normal gravity these<br />

processes are ma<strong>in</strong>ly dom<strong>in</strong>ated by the natural convective<br />

flows <strong>and</strong> other processes. Diffusion effects, however,<br />

have nearly no <strong>in</strong>fluence. This is different under<br />

microgravity. Microgravity generally <strong>of</strong>fers unique<br />

prospects for the underst<strong>and</strong><strong>in</strong>g <strong>and</strong> improvement <strong>of</strong><br />

combustion processes, as the absence <strong>of</strong> buoyancy allows<br />

measurements with low-speed flows result<strong>in</strong>g <strong>in</strong><br />

an enlargement <strong>of</strong> spatial <strong>and</strong> temporal scales. The<br />

possibilities <strong>of</strong> a full control <strong>of</strong> residence times <strong>and</strong> <strong>of</strong><br />

an observation <strong>of</strong> basic combustion phenomena without<br />

buoyancy-<strong>in</strong>duced flow superimposed, make it also<br />

possible to establish <strong>and</strong> improve models for soot formation.<br />

The mathematical treatment <strong>of</strong> combustion<br />

processes is simplified [3], <strong>and</strong> therefore they are studied<br />

<strong>in</strong> different microgravity facilities like drop towers,<br />

parabolic flights with aircrafts or <strong>in</strong> space [4].<br />

Lam<strong>in</strong>ar non-premixed flames have been <strong>of</strong> special<br />

<strong>in</strong>terest <strong>in</strong> microgravity combustion research as they<br />

provide a good model system for numerical studies.<br />

For that reason, they have also been chosen for the experiments<br />

presented <strong>in</strong> this paper. For an assessment<br />

<strong>of</strong> particle growth, which is essential for a detailed<br />

comprehension <strong>and</strong> modell<strong>in</strong>g <strong>of</strong> soot formation, not<br />

only soot concentration pr<strong>of</strong>iles but also primary particle<br />

sizes have to be determ<strong>in</strong>ed. A measurement technique<br />

which is able to measure both quantities simultaneously<br />

is time-resolved laser-<strong>in</strong>duced <strong>in</strong>c<strong>and</strong>escence<br />

(TIRE-LII) [5, 6, 7].<br />

∗ Correspond<strong>in</strong>g author: mwe@ltt.uni-erlangen.de<br />

Associated Web site: http://www.ltt.uni-erlangen.de<br />

Proceed<strong>in</strong>gs <strong>of</strong> the European Combustion Meet<strong>in</strong>g<br />

The basic pr<strong>in</strong>ciple <strong>of</strong> laser-<strong>in</strong>duced <strong>in</strong>c<strong>and</strong>escence<br />

(LII) is to heat up particles with a short laser pulse <strong>of</strong><br />

high energy up to their vaporization temperature, followed<br />

by the detection <strong>of</strong> the enhanced thermal radiation<br />

[8]. The heated particles release the absorbed energy<br />

via three paths: vaporisation, heat conduction to<br />

the surround<strong>in</strong>g medium <strong>and</strong> thermal radiation. For the<br />

whole process, the energy balance is set up which leads<br />

to a differential equation which can be solved numerically<br />

for obta<strong>in</strong><strong>in</strong>g the temporal behaviour <strong>of</strong> the LII<br />

signal [6, 9].<br />

It has been shown that the <strong>in</strong>tensity <strong>in</strong> the moment<br />

<strong>of</strong> the laser pulse is nearly proportional to soot volume<br />

concentration which has also been proven <strong>in</strong> several<br />

experiments, see, e.g., [10, 11]. Moreover, the evaluation<br />

<strong>of</strong> the temporal signal decay provides primary<br />

particle sizes [5, 7, 12], because later than 100 ns after<br />

the laser pulse conductive heat loss to the surround<strong>in</strong>g<br />

gas is the dom<strong>in</strong>ant cool<strong>in</strong>g process. This is ma<strong>in</strong>ly<br />

governed by the particles’ specific surface area, i.e.,<br />

smaller particles cool down faster correspond<strong>in</strong>g to a<br />

faster decreas<strong>in</strong>g signal. <strong>Primary</strong> particle size is determ<strong>in</strong>ed<br />

by comparison <strong>of</strong> experimental decay rates with<br />

calculated model signal decay rates. For the determ<strong>in</strong>ation<br />

<strong>of</strong> a two-dimensional distribution <strong>of</strong> primary particle<br />

size the signal is measured at two different moments<br />

after the laser pulse. From the ratio <strong>of</strong> these two signals<br />

the primary particle size can be calculated. Renounc<strong>in</strong>g<br />

spatial resolution the whole signal decay can be evaluated<br />

which results <strong>in</strong> improved statistics.<br />

Some studies concern<strong>in</strong>g soot volume concentrations<br />

<strong>in</strong> flames under microgravity us<strong>in</strong>g LII have al-


eady been done [13, 14]. In the present work, not only<br />

soot volume concentrations but also primary particle<br />

sizes have been measured spatially resolved <strong>in</strong> lam<strong>in</strong>ar<br />

non-premixed ethene <strong>and</strong> methane flames. A special<br />

<strong>in</strong>terest was set on the <strong>in</strong>fluence <strong>of</strong> the variation <strong>of</strong> air<br />

co-flow on soot parameters under different gravity conditions.<br />

The emphasis <strong>of</strong> this paper is the description<br />

<strong>of</strong> the phenomena discovered. Only some <strong>of</strong> the results<br />

obta<strong>in</strong>ed could have been expla<strong>in</strong>ed so far <strong>and</strong> will be<br />

the subject <strong>of</strong> future experimental an theoretical work.<br />

Experimental Setup<br />

The experiments have been carried out dur<strong>in</strong>g an<br />

ESA parabolic flight campaign aboard an Airbus A300<br />

aircraft. Each parabola was <strong>in</strong>itiated <strong>and</strong> closed by a<br />

time period <strong>of</strong> <strong>in</strong>creased gravity (1.8 g), embedd<strong>in</strong>g an<br />

about 20 second period <strong>of</strong> microgravity. Thus, <strong>in</strong>clud<strong>in</strong>g<br />

the time between two parabolas, the flames could be<br />

observed under three different gravity conditions. Due<br />

to safety reasons aboard the aircraft, the setup had to<br />

be completely <strong>in</strong>tegrated <strong>in</strong> a rack, as shown <strong>in</strong> Fig. 1.<br />

The burner was <strong>in</strong>stalled <strong>in</strong>side a chamber connected<br />

to the exhaust l<strong>in</strong>e <strong>of</strong> the overboard ventilation system.<br />

The burner chamber was equipped with four optical<br />

w<strong>in</strong>dows for the access to the measurement location.<br />

Magnetic <strong>and</strong> flame-non-return valves were <strong>in</strong>stalled to<br />

ensure a safe operation <strong>of</strong> the gas supply, <strong>and</strong> all relevant<br />

parameters were controlled automatically, especially<br />

the amount <strong>of</strong> fuel <strong>and</strong> air co-flow, which was varied<br />

systematically to determ<strong>in</strong>e the <strong>in</strong>fluence <strong>of</strong> these<br />

parameters on soot formation under microgravity. The<br />

burner itself consisted <strong>of</strong> two concentric tubes, the <strong>in</strong>ner<br />

one (2.2 mm <strong>in</strong> diameter) for fuel (ethene or methane)<br />

the outer one (30 mm <strong>in</strong> diameter) for air co-flow (synthetic<br />

air 20.5 % O2, 79.5 % N2). Besides, a second air<br />

co-flow was <strong>in</strong>tegrated to prevent the dimm<strong>in</strong>g <strong>of</strong> the<br />

optical w<strong>in</strong>dows by condensed vapour.<br />

Laser power supply<br />

Laser head<br />

Monitor #1 Monitor #2<br />

Electronics Camera controller #1 Camera controller #2<br />

ICCD camera #2<br />

burner<br />

chamber<br />

Figure 1: Schematical draw<strong>in</strong>g <strong>of</strong> the experimental setup<br />

The setup was chosen as a result <strong>of</strong> the experience<br />

<strong>of</strong> an earlier campaign with a different burner<br />

configuration, where the flame structures had been disturbed<br />

by short periods <strong>of</strong> negative gravity forces dur<strong>in</strong>g<br />

the parabolas, result<strong>in</strong>g <strong>in</strong> a complete collapse <strong>of</strong> the<br />

ICCD camera #1<br />

2<br />

flames. The actual layout was constructed to be able to<br />

<strong>in</strong>crease the gas flows, provid<strong>in</strong>g more stable flames.<br />

Nevertheless, also <strong>in</strong> this new experimental approach<br />

the flame shape was affected by g-jitter which<br />

will be described <strong>in</strong> detail later. The soot particles were<br />

heated up to their vaporisation temperature by us<strong>in</strong>g<br />

a frequency-doubled Nd:YAG laser with a pulse frequency<br />

<strong>of</strong> 10 Hz <strong>and</strong> a pulse duration <strong>of</strong> 6 ns. The beam<br />

was formed to a light sheet with a width <strong>of</strong> 3 cm <strong>and</strong><br />

a thickness <strong>of</strong> 0.5 cm which leads to an irradiance <strong>of</strong><br />

1·10 8 W/cm 2 for a typical pulse energy <strong>of</strong> 75 mJ. Modifications<br />

<strong>of</strong> the laser were done by the manufacturer<br />

to ensure functionality under microgravity conditions.<br />

Thus, a variation <strong>of</strong> laser output was not expected <strong>and</strong><br />

there was no cont<strong>in</strong>uous control <strong>of</strong> pulse energy dur<strong>in</strong>g<br />

the flight <strong>in</strong>stalled. It was only measured prior <strong>and</strong> after<br />

every flight <strong>in</strong>dicat<strong>in</strong>g no differences. In the course <strong>of</strong><br />

the data evaluation, however, <strong>in</strong>dications for laser pulse<br />

energy fluctuations appeared. This poses an uncerta<strong>in</strong>ty<br />

especially on the results <strong>of</strong> the primary particle size determ<strong>in</strong>ation.<br />

The reason for this unreliable behaviour<br />

<strong>of</strong> the laser under microgravity has not been found yet.<br />

The LII signal was detected by us<strong>in</strong>g two ICCD cameras,<br />

placed opposite each other, perpendicular to the<br />

laser beam, as it can be seen <strong>in</strong> Fig. 1. It turned out<br />

that the camera sensitivity varied up to 25 % between<br />

two follow<strong>in</strong>g images. In addition, the extent <strong>of</strong> this effect<br />

was dependent on the chosen <strong>in</strong>tensifier ga<strong>in</strong> value.<br />

Thus, the results for ethene flames <strong>and</strong> methane flames<br />

cannot be compared quantitatively as different ga<strong>in</strong> values<br />

had to be used due to lower soot concentrations <strong>in</strong><br />

the methane flame. Nevertheless, a lot <strong>of</strong> valuable <strong>in</strong>formation<br />

could be acquired, which will be presented<br />

hereafter.<br />

The maximum signal was captured by one <strong>of</strong> the<br />

cameras <strong>and</strong> compared later to a s<strong>in</strong>gle l<strong>in</strong>e-<strong>of</strong>-sight ext<strong>in</strong>ction<br />

measurement for calibration <strong>in</strong> order to get <strong>in</strong>formation<br />

on the absolute soot volume concentration.<br />

For the determ<strong>in</strong>ation <strong>of</strong> the primary particle sizes the<br />

LII signal decay was evaluated by detect<strong>in</strong>g at two different<br />

times, 100 ns <strong>and</strong> 400 ns after the laser pulse.<br />

From the signal ratio the signal decay time constant<br />

can be calculated. Tak<strong>in</strong>g <strong>in</strong>to consideration the ambient<br />

temperature this ratio is unambiguously related<br />

to the primary particle size. Unfortunately, due to experimental<br />

problems, we have no <strong>in</strong>formation about the<br />

temperature distribution <strong>in</strong> the exam<strong>in</strong>ed flames. Therefore,<br />

temperature <strong>in</strong>formation from measurements performed<br />

at the ZARM drop tower <strong>in</strong> Bremen, Germany,<br />

by project partners us<strong>in</strong>g the same burner configuration,<br />

fuel <strong>and</strong> air co-flow parameters were used for data evaluation.<br />

Results <strong>and</strong> Discussion<br />

Flame behaviour Dur<strong>in</strong>g most <strong>of</strong> the parabolas the<br />

<strong>in</strong>fluence <strong>of</strong> reduced gravity <strong>and</strong> the typical behaviour


under microgravity could be observed [15, 16]. All <strong>in</strong>vestigated<br />

flames were broadened under microgravity<br />

<strong>and</strong> longer as their counterparts under normal gravity.<br />

However, the change <strong>of</strong> flame shape under µg was dependent<br />

on the chosen gas <strong>and</strong> air flows. Some ethene<br />

flames show no open tip under microgravity (see Fig. 3<br />

<strong>and</strong> Fig. 4).<br />

Figure 2: Sequence <strong>of</strong> LII-Signals dur<strong>in</strong>g a collapse <strong>of</strong> a<br />

flame due to g-jitter<br />

Nevertheless, <strong>in</strong> some cases, short periods <strong>of</strong> negative<br />

g-forces <strong>in</strong>duced a fast breakdown <strong>of</strong> the flame.<br />

Fig. 2 shows the LII-signal <strong>of</strong> an ethene flame <strong>in</strong> an exemplary<br />

case. Unfortunately, even without flame breakdown,<br />

the exact evaluation <strong>of</strong> the measurements still reveals<br />

a strong <strong>in</strong>fluence <strong>of</strong> fluctuations <strong>in</strong> the quality<br />

<strong>of</strong> microgravity on the flame shape. The behaviour <strong>of</strong><br />

the flame dur<strong>in</strong>g the parabolas is not only determ<strong>in</strong>ed<br />

by the absolute value <strong>of</strong> rema<strong>in</strong><strong>in</strong>g gravity, but depends<br />

also on the course <strong>of</strong> the g-level dur<strong>in</strong>g the beg<strong>in</strong>n<strong>in</strong>g <strong>of</strong><br />

the parabola. Thus, a steep gradient with a slight overturn<br />

<strong>in</strong>to the region <strong>of</strong> negative accelerations causes a<br />

different flame shape than a smooth beg<strong>in</strong>n<strong>in</strong>g <strong>of</strong> the<br />

µg-phase with some time <strong>of</strong> negative g. The latter behaviour<br />

results more <strong>of</strong>ten <strong>in</strong> a collaps<strong>in</strong>g flame. As<br />

the effect <strong>of</strong> g-jtter is stronger <strong>in</strong> flames with low flow<br />

rates, <strong>in</strong> future campaigns a compromise must be found<br />

<strong>in</strong> chos<strong>in</strong>g flow rates both lead<strong>in</strong>g to stable flames <strong>and</strong><br />

show<strong>in</strong>g the effects <strong>of</strong> microgravity.<br />

3<br />

<strong>Soot</strong> volume concentration Figures 3 <strong>and</strong> 4 show<br />

the soot volume concentration for ethene flames under<br />

variation <strong>of</strong> air co-flow rate <strong>and</strong> ethene flow rate respectively.<br />

Figure 3: <strong>Soot</strong> volume concentration for different ethene<br />

flow rates (<strong>in</strong> ppmv): 75 scm3 /m<strong>in</strong> (a <strong>and</strong> c) <strong>and</strong><br />

100 scm3 /m<strong>in</strong> (b <strong>and</strong> d); air co-flow rate: 10 sl/m<strong>in</strong><br />

Figure 4: <strong>Soot</strong> volume concentration for different air co-flow<br />

rates (<strong>in</strong> ppmv): 15 sl/m<strong>in</strong> (a <strong>and</strong> d), 10 sl/m<strong>in</strong> (b <strong>and</strong> e),<br />

<strong>and</strong> 8 sl/m<strong>in</strong> (c <strong>and</strong> f); ethene flow rate: 75 scm3 /m<strong>in</strong><br />

For the variation <strong>of</strong> air co-flow <strong>in</strong> ethene flames a<br />

rather strong <strong>in</strong>fluence <strong>of</strong> the amount <strong>of</strong> air co-flow on<br />

soot volume fraction <strong>and</strong> its distribution <strong>in</strong> the flame<br />

can be observed under microgravity. As it can be seen<br />

<strong>in</strong> Fig. 4, soot volume concentration <strong>in</strong>creases with<br />

ris<strong>in</strong>g ethene flow rate <strong>in</strong> outer flame regions <strong>and</strong> decreases<br />

with fall<strong>in</strong>g air co-flow <strong>in</strong> the <strong>in</strong>ner flame regions<br />

result<strong>in</strong>g <strong>in</strong> an <strong>in</strong>creased soot formation <strong>in</strong> a narrow<br />

b<strong>and</strong> at the outer regions. This is <strong>in</strong> contrast to<br />

observations under normal gravity. A variation <strong>of</strong> air<br />

co-flow has no significant <strong>in</strong>fluence on the amount <strong>of</strong><br />

soot produced <strong>in</strong> the exam<strong>in</strong>ed flames under buoyant<br />

conditions.<br />

The <strong>in</strong>fluence <strong>of</strong> the variation <strong>of</strong> ethene flow rate is<br />

shown <strong>in</strong> Fig. 3. Under normal gravity, only the amount<br />

<strong>of</strong> soot produced rises with an <strong>in</strong>crease <strong>of</strong> ethene flow<br />

rate, the distribution <strong>of</strong> soot <strong>in</strong> the flames rema<strong>in</strong>s extensively<br />

constant. In contrast to that, there is a decrease<br />

<strong>of</strong> soot volume concentration <strong>in</strong> <strong>in</strong>ner flame regions <strong>and</strong><br />

an <strong>in</strong>crease <strong>in</strong> outer flame regions. The results obta<strong>in</strong>ed<br />

dur<strong>in</strong>g the 1.8 g phase are not shown, as the flames behave<br />

similar to the 1 g flames. An explanation for this<br />

difference <strong>in</strong> soot distribution between 1 g <strong>and</strong> µg can<br />

be found <strong>in</strong> the temperature distribution <strong>in</strong> the flames<br />

which is several hundred degrees lower <strong>in</strong> the micro-


gravity flames than at normal gravity, result<strong>in</strong>g <strong>in</strong> overall,<br />

but also local larger soot production.<br />

The results <strong>of</strong> the experiments with methane reveal<br />

a different soot distribution under microgravity than<br />

for the ethene flames (see Fig. 5). The soot distribution<br />

is more concentrated <strong>in</strong> the <strong>in</strong>ner flame regions<br />

<strong>and</strong> nearly <strong>in</strong>dependent <strong>of</strong> the magnitude <strong>of</strong> the air c<strong>of</strong>low.<br />

The soot concentration is overall lower than <strong>in</strong><br />

ethene flames. Regard<strong>in</strong>g the <strong>in</strong>fluence <strong>of</strong> the variation<br />

<strong>of</strong> the air co-flow no difference between the 1 g <strong>and</strong><br />

1.8 g phase could be observed.<br />

Figure 5: <strong>Soot</strong> volume concentration (<strong>in</strong> a. u.) for methane<br />

flames under microgravity (left) <strong>and</strong> normal gravity<br />

(right)<br />

<strong>Primary</strong> particle sizes Furthermore, the primary<br />

particle size distribution has been determ<strong>in</strong>ed <strong>in</strong>side the<br />

flame for different fuels <strong>and</strong> air co-flow rates. As mentioned<br />

above, there were <strong>in</strong>dications for unstable laser<br />

operation dur<strong>in</strong>g the µg phase result<strong>in</strong>g <strong>in</strong> a clearly<br />

lower pulse energies. The presented results are based<br />

on the assumption <strong>of</strong> an irradiance <strong>of</strong> 5 MW/cm 2 . A temperature<br />

distribution with a temperature gradient from<br />

1700 K to 1400 K <strong>in</strong> microgravity was chosen <strong>in</strong> agreement<br />

with drop-tower measurements, <strong>and</strong> an uniform<br />

temperature <strong>of</strong> 1800 K for 1 g (obta<strong>in</strong>ed <strong>in</strong> previous<br />

ground-based measurements with the same setup).<br />

The reduced flame temperature under microgravity<br />

can be expected due to the larger residence time <strong>of</strong> particles<br />

<strong>in</strong> the flame <strong>and</strong> the <strong>in</strong>creased radiation losses.<br />

Figure 6: <strong>Primary</strong> particle sizes (<strong>in</strong> nm) for different air c<strong>of</strong>low<br />

rates: 8 sl/m<strong>in</strong> (a, d), 7 sl/m<strong>in</strong> (b, e), 5 sl/m<strong>in</strong> (c, f);<br />

fuel flow rate: 75 scm3 /m<strong>in</strong> under microgravity (a-c)<br />

<strong>and</strong> 1 g (d-e)<br />

It can be seen <strong>in</strong> Fig. 6 that there is only a m<strong>in</strong>or<br />

<strong>in</strong>fluence <strong>of</strong> air co-flow at 1 g as well as at 0 g. Under<br />

4<br />

microgravity, the largest particles can be found <strong>in</strong> the<br />

same narrow b<strong>and</strong> at outer flame regions where large<br />

soot concentrations have been measured (see Fig. 3 <strong>and</strong><br />

Fig. 4). Compared to microgravity, under normal gravity<br />

the maximum primary particle sizes are about half<br />

the values which have been found under microgravity.<br />

This may be due to the extended residence time <strong>of</strong> particles<br />

<strong>in</strong> the flame under microgravity <strong>and</strong> the lower surround<strong>in</strong>g<br />

gas temperatures.<br />

For the methane flame, the results under microgravity<br />

are displayed <strong>in</strong> Fig. 7. The particles are smaller<br />

than <strong>in</strong> the ethene flames <strong>and</strong> more equally distributed<br />

over the flame body which has also been found for the<br />

soot volume concentration (Fig. 5). Aga<strong>in</strong>, the <strong>in</strong>fluence<br />

<strong>of</strong> air co-flow on primary particle sizes is very<br />

low. Under normal gravity, the soot volume concentration<br />

was too low to measure particle sizes.<br />

Figure 7: <strong>Primary</strong> particle sizes (<strong>in</strong> nm) <strong>in</strong> methane flames<br />

under microgravity for different air co-flow rates:<br />

a) 15 sl/m<strong>in</strong>, b) 10 sl/m<strong>in</strong>; methane flow rate: 110 scm3 /m<strong>in</strong><br />

Conclusions<br />

Experiments on ethene <strong>and</strong> methane flames <strong>in</strong> different<br />

gravity environments have been performed. In<br />

ethene flames, under microgravity soot volume fraction<br />

<strong>in</strong>creases with ris<strong>in</strong>g fuel flow rates <strong>and</strong> decreases with<br />

fall<strong>in</strong>g air co-flow <strong>in</strong> <strong>in</strong>ner flame regions result<strong>in</strong>g <strong>in</strong> an<br />

<strong>in</strong>creased soot formation <strong>in</strong> a narrow b<strong>and</strong> <strong>in</strong> the outer<br />

regions. The <strong>in</strong>fluence <strong>of</strong> a variation <strong>of</strong> air co-flow on<br />

primary particle sizes is rather low, compared to 1 g,<br />

primary particle sizes are roughly doubled under µg.<br />

Neither under normal gravity nor under <strong>in</strong>creased gravity<br />

any <strong>in</strong>fluence <strong>of</strong> air co-flow on the soot<strong>in</strong>g behaviour<br />

could be found, the flames are <strong>in</strong> general very similar<br />

under 1 g <strong>and</strong> 1.8 g. In methane flames, the soot volume<br />

concentration showed a different behaviour under<br />

microgravity than <strong>in</strong> ethene flames, be<strong>in</strong>g more concentrated<br />

<strong>in</strong> the <strong>in</strong>ner regions <strong>of</strong> the flame <strong>and</strong> nearly<br />

<strong>in</strong>dependent on the air co-flow. The absolute values<br />

were overall lower than <strong>in</strong> ethene flames, <strong>and</strong> significantly<br />

smaller particle sizes have been found. TIRE-LII<br />

has been proven to be a suitable non-<strong>in</strong>vasive technique<br />

for measur<strong>in</strong>g the soot<strong>in</strong>g characteristics <strong>of</strong> flames under<br />

microgravity, provid<strong>in</strong>g spatially resolved <strong>in</strong>forma-


tion on soot volume concentration <strong>and</strong> primary particle<br />

sizes.<br />

Acknowledgements<br />

The authors gratefully acknowledge f<strong>in</strong>ancial support<br />

for parts <strong>of</strong> the work by the European Space<br />

Agency (ESA) <strong>and</strong> by the German National Science<br />

Foundation (DFG).<br />

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