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Aviation and the Global Atmosphere

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<strong>Aviation</strong> <strong>and</strong> <strong>the</strong> <strong>Global</strong> <strong>Atmosphere</strong><br />

Burtscher, 1992). In <strong>the</strong> jet regime, some recent models indicate that CIs effectively promote formation <strong>and</strong> growth of electrically charged droplets containing H 2 SO 4<br />

<strong>and</strong> H 2 O (Yu <strong>and</strong> Turco, 1997). In addition, CIs may contribute to <strong>the</strong> activation of exhaust soot. Positive ions include H3O+ <strong>and</strong> organic molecules like CHO+, C3H3+,<br />

<strong>and</strong> larger molecules (Calcote, 1983), whereas <strong>the</strong> free electrons rapidly attach to o<strong>the</strong>r molecules to form negative ions with sulfate <strong>and</strong> nitrate cores. Measurements<br />

of positive CIs in exhaust plumes are not available, <strong>and</strong> only very few in situ measurements of negative CIs are available to date.<br />

Arnold et al. (1998a) measured a total negative CI concentration of 3 x 10 7 cm -3 (about 3 x 1015/kg fuel) at plume ages of around 10 ms in <strong>the</strong> exhaust of a jet engine<br />

on <strong>the</strong> ground, consistent with approximately 10 9 cm -3 at a plume age of 1 ms (Yu et al., 1998).<br />

That concentration represents a lower bound from diffusion losses of <strong>the</strong>se particles within sampling devices prior to detection <strong>and</strong> <strong>the</strong> limited detection range of <strong>the</strong><br />

employed mass spectrometer. The fact that <strong>the</strong>se measurements yielded only a fraction of CIs in <strong>the</strong> plume has been partially confirmed by in-flight measurements<br />

(Arnold et al., 1998b) showing smaller total CI count rates for high-sulfur fuel compared with low-sulfur fuel. Therefore, current CI data are consistent with a CI<br />

emission index of about 2-4 x 1017/kg, corresponding to a concentration of about 2 x 10 9 cm -3 at <strong>the</strong> engine exit. This value has been estimated numerically based on<br />

coupled ion-ion recombination kinetics <strong>and</strong> plume mixing (Yu <strong>and</strong> Turco, 1997; Kärcher et al., 1998b; Yu et al.,1998). Although not directly comparable, CIs have been<br />

observed in hydrocarbon flames at concentrations of about 10 8 to 10 11 cm -3 (Keil et al., 1984), supporting <strong>the</strong> estimated concentration of negative CIs.<br />

3.2.1.4 Nitrogen Species<br />

The primary nitrogen emission from aircraft is in <strong>the</strong> form of NOx (Chapter 2). In reactions of NOx with OH in <strong>the</strong> plume, gaseous HNO2 <strong>and</strong> HNO3 are formed. Despite<br />

larger reaction rates, less HNO3 is formed than HNO2 because <strong>the</strong> ratio of NO2 to NO at <strong>the</strong> engine exit is small (< 0.2) (e.g., Schulte et al., 1997) (see Chapter 7).<br />

HNO3 can also form in <strong>the</strong> plume even in <strong>the</strong> absence of NO2 emissions (Kärcher et al., 1996a). In situ measurements in young plumes revealed both HNO2 <strong>and</strong><br />

HNO3 concentrations above background levels (Arnold et al., 1992, 1994; Tremmel et al., 1998). HNO3 can be more abundant in plumes than H2SO4 , especially for<br />

low EI(S) values. These acids (especially HNO3 ) are important because <strong>the</strong>y can be taken up by water-soluble exhaust particles <strong>and</strong> form stable condensed phases<br />

such as nitric acid trihydrate (NAT = HNO3•3H2O) <strong>and</strong> liquid ternary (H2O/H2SO4 /HNO3 ) solutions under cold <strong>and</strong> humid plume conditions (Arnold et al., 1992;<br />

Kärcher, 1996).<br />

3.2.1.5. Hydrocarbons<br />

Aircraft engines emit non-methane hydrocarbons (NMHCs) as a result of incomplete fuel combustion. These species include alkenes (mostly e<strong>the</strong>ne), aldehydes<br />

(mostly formaldehyde), alkines (mostly ethine), <strong>and</strong> a few aromates. A few (8 to 10) species were found to account for up to 80% of NMHC emissions (Spicer et al.,<br />

1992, 1994). High levels of carbonyl compound emissions (on <strong>the</strong> order of 0.2 ppmv) also have been observed in a combustor (Wahl et al., 1997). Some in-flight data<br />

indicate that NMHCs with up to 8 carbon atoms have EIs in <strong>the</strong> range 0.05 to 0.2 g C/kg fuel <strong>and</strong> represent approximately 70% of total NMHC emissions (Slemr et al.,<br />

1998). However, <strong>the</strong> current database on NMHC emissions <strong>and</strong> on partitioning between individual compounds is small <strong>and</strong> perhaps not representative for all engine<br />

types. Some emitted NMHCs might act as aerosol-forming agents in nascent plumes <strong>and</strong> may be adsorbed or dissolved in plume particles, <strong>the</strong>reby possibly<br />

contributing to <strong>the</strong> total amount of volatile aerosol found in plumes (Kärcher et al., 1998b). In addition, <strong>the</strong> presence of trace NMHCs amounts may facilitate nucleation<br />

(e.g., Katz et al., 1977) <strong>and</strong> alter <strong>the</strong> hygroscopic behavior <strong>and</strong> growth rates of particles (Saxena et al., 1995; Cruz <strong>and</strong> P<strong>and</strong>is, 1997). Engines also may emit volatile<br />

particles containing engine oils or o<strong>the</strong>r lubricants, but this effect has not been quantified.<br />

http://www.ipcc.ch/ipccreports/sres/aviation/034.htm (3 von 9)08.05.2008 02:41:56

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