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On the Formation of Nitrogen Oxides During the Combustion of ...

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4 Numerical Modeling and Simulation<br />

since not only vaporization but also burning rates are relevant. Besides, <strong>the</strong><br />

impact <strong>of</strong> chemistry can also be included in this step <strong>of</strong> <strong>the</strong> validation process.<br />

In an early, still ground-based work, Hall and Diederichsen [164] experimentally<br />

investigated <strong>the</strong> burning characteristics <strong>of</strong> free and suspended droplets<br />

<strong>of</strong> alkanes and alcohols for a pressure range <strong>of</strong> 1 to 20 bar. Law and Williams<br />

[237] derive a burning rate <strong>of</strong> k = 0.93 mm 2 s −1 from those experiments for a n-<br />

decane droplet <strong>of</strong> D 0 = 1.10 mm (with T ∞ = 293 K and p g = 1bar). Their own<br />

model predicts values <strong>of</strong> 0.79 and 0.66 mm 2 s −1 for <strong>the</strong> respective cases with<br />

and without natural convection. The work <strong>of</strong> Shaw et al. [394] represents one<br />

<strong>of</strong> <strong>the</strong> first investigations conducted under microgravity conditions that is relevant<br />

to <strong>the</strong> present study. Shaw et al. measured <strong>the</strong> quasi-steady burning rate<br />

k <strong>of</strong> n-decane droplets in air at room temperature and atmospheric pressure,<br />

ignited by a spark-ignition system. The reported k-values spread over a wide<br />

range, and results are shown as subdivided into minimum, maximum, and orthogonal<br />

least-square values – probably due to scattering. In later work, Shaw<br />

and Dee [392] measured k = 0.78mm 2 s −1 for a burning C 10 H 22 droplet with<br />

D 0 = 1.12mm at T ∞ = 298K. They also report unsteady flame stand-<strong>of</strong>f ratios<br />

for an ambient oxygen mole fraction <strong>of</strong> 0.21 combined with different diluents.<br />

In <strong>the</strong> experimental work <strong>of</strong> Nakaya et al. [307, 309], an averaged k-value <strong>of</strong><br />

k = 0.72mm 2 s −1 is obtained for similar conditions. The corresponding instantaneous<br />

burning rate fluctuates between values <strong>of</strong> 0.5 and 1.0 mm 2 s −1 .<br />

Dietrich et al. [102] also performed microgravity experiments plus numerical<br />

modeling. However, most experimental results are retrieved from atmospheres<br />

with reduced pressure. Jackson and Avedisian [192] report a decreasing<br />

tendency <strong>of</strong> <strong>the</strong> k-value with an increase in <strong>the</strong> initial droplet diameter for<br />

n-heptane and 1-chloro-octane, both for suspended as well as free-floating<br />

droplets. Xu et al. [465] extend this observation for n-decane towards an inverse<br />

influence <strong>of</strong> <strong>the</strong> initial droplet diameter on <strong>the</strong> vaporization and burning<br />

rates in cold and hot ambiences. The effects <strong>of</strong> flame radiation and soot<br />

formation as well as soot oxidation are discussed in detail, including <strong>the</strong>ir impact<br />

on <strong>the</strong> burning rates <strong>of</strong> droplets <strong>of</strong> different diameter. <strong>On</strong> <strong>the</strong> one hand,<br />

<strong>the</strong> work <strong>of</strong> Xu et al. [465] naturally covers a wide range <strong>of</strong> ambient temperatures<br />

and is <strong>the</strong>refore considered for validating <strong>the</strong> single droplet model <strong>of</strong><br />

<strong>the</strong> present study (cf. Tab. 4.1). <strong>On</strong> <strong>the</strong> o<strong>the</strong>r hand, <strong>the</strong> mentioned effects <strong>of</strong><br />

radiation and soot formation are not captured with <strong>the</strong> present model. Consequently,<br />

a certain deviation from <strong>the</strong> measurements has to be expected. Fur-<br />

148

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