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<article language="en">
	<journal>
		<journal_title>Atmospheric Measurement Techniques</journal_title>
		<journal_url>www.atmos-meas-tech.net</journal_url>
		<issn>1867-1381</issn>
		<eissn>1867-8548</eissn>
		<volume_number>2</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/amt-2-231-2009</doi>
	<article_url>http://www.atmos-meas-tech.net/2/231/2009/</article_url>
	<abstract_html>http://www.atmos-meas-tech.net/2/231/2009/amt-2-231-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-meas-tech.net/2/231/2009/amt-2-231-2009.pdf</fulltext_pdf>
	<start_page>231</start_page>
	<end_page>242</end_page>
	<publication_date>2009-06-16</publication_date>
	<article_title content_type="html">An experimental technique for the direct measurement of N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; reactivity on ambient particles</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>T. H. Bertram</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>J. A. Thornton</name>
			<email>thornton@atmos.washington.edu</email>
		</author>
		<author numeration="3" affiliations="1,2">
			<name>T. P. Riedel</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA</affiliation>
		<affiliation numeration="2" content_type="html">Department of Chemistry, University of Washington, Seattle, WA, USA</affiliation>
	</affiliations>
	<abstract content_type="html">An experimental approach for the direct measurement of trace gas reactivity
on ambient aerosol particles has been developed. The method utilizes a newly
designed entrained aerosol flow reactor coupled to a custom-built chemical
ionization mass spectrometer. The experimental method is described via
application to the measurement of the N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt; reaction probability,
γ (N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;). Laboratory investigations on well characterized
aerosol particles show that measurements of γ (N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;) observed
with this technique are in agreement with previous observations, using
conventional flow tube methods, to within &amp;plusmn;20% at atmospherically
relevant particle surface area concentrations
(0–1000 &amp;mu;m&lt;sup&gt;2&lt;/sup&gt; cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt;). Uncertainty in the measured
γ (N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;) is discussed in the context of fluctuations in
potential ambient biases (e.g., temperature, relative humidity and trace gas
loadings). Under ambient operating conditions we estimate a single-point
uncertainty in γ (N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;) that ranges between
&amp;plusmn; (1.3&amp;times;10&lt;sup&gt;-2&lt;/sup&gt; + 0.2&amp;times;&amp;gamma; (N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;)), and
&amp;plusmn; (1.3&amp;times;10&lt;sup&gt;-3&lt;/sup&gt; + 0.2&amp;times;&amp;gamma; (N&lt;sub&gt;2&lt;/sub&gt;O&lt;sub&gt;5&lt;/sub&gt;)) for
particle surface area concentrations of 100 to 1000 &amp;mu;m&lt;sup&gt;2&lt;/sup&gt; cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt;,
respectively. Examples from both laboratory investigations and field
observations are included alongside discussion of future applications for the
reactivity measurement and optimal deployment locations and conditions.</abstract>
	<references>
		<reference numeration="1" content_type="text"> Abbatt, J. P. D. and Waschewsky, G. C. G.: Heterogeneous interactions of HOBr, HNO&lt;sub&gt;3&lt;/sub&gt;, O&lt;sub&gt;3&lt;/sub&gt;, and NO&lt;sub&gt;2&lt;/sub&gt; with deliquescent NaCl aerosols at room temperature, J. Phys. Chem. A, 102, 3719–3725, 1998. </reference>
		<reference numeration="2" content_type="text"> Atkinson, R. and Arey, J.: Gas-phase tropospheric chemistry of biogenic volatile organic compounds: a review, Atmos. Environ., 37, S197–S219, 2003. </reference>
		<reference numeration="3" content_type="text"> Badger, C. L., Griffiths, P. T., George, I., Abbatt, J. P. D., and Cox, R. A.: Reactive uptake of N&lt;sub&gt;2&lt;/sub&gt;O$_5$ by aerosol particles containing mixtures of humic acid and ammonium sulfate, J. Phys. Chem. A, 110, 6986–6994, 2006. </reference>
		<reference numeration="4" content_type="text"> Behnke, W. and Zetzsch, C.: Heterogeneous formation of chlorine atoms from various aerosols in the presence of O&lt;sub&gt;3&lt;/sub&gt; and HCl, J. Aerosol Sci., 20, 1167–1170, 1989. </reference>
		<reference numeration="5" content_type="text"> Boulter, J. E., Cziczo, D. J., Middlebrook, A. M., Thomson, D. S., and Murphy, D. M.: Design and performance of a pumped counterflow virtual impactor, Aerosp. Sci. Technol., 40, 969–976, 2006. </reference>
		<reference numeration="6" content_type="text"> Braban, C. F. and Abbatt, J. P. D.: A study of the phase transition behavior of internally mixed ammonium sulfate – malonic acid aerosols, Atmos. Chem. Phys., 4, 1451–1459, 2004. </reference>
		<reference numeration="7" content_type="text"> Broekhuizen, K. E., Thornberry, T., Kumar, P. P., and Abbatt, J. P. D.: Formation of cloud condensation nuclei by oxidative processing: Unsaturated fatty acids, J. Geophys. Res., 109, D24206, doi:10.1029/2004JD005298, 2004. </reference>
		<reference numeration="8" content_type="text"> Brown, R. L.: Tubular Flow Reactors with 1st-Order Kinetics, J. Res. Nat. Bur. Stand., 83, 1–8, 1978. </reference>
		<reference numeration="9" content_type="text"> Brown, S. S., Ryerson, T. B., Wollny, A. G., Brock, C. A., Peltier, R., Sullivan, A. P., Weber, R. J., Dube, W. P., Trainer, M., Meagher, J. F., Fehsenfeld, F. C., and Ravishankara, A. R.: Variability in nocturnal nitrogen oxide processing and its role in regional air quality, Science, 311, 67–70, 2006. </reference>
		<reference numeration="10" content_type="text"> Calvert, J. G., Lazrus, A., Kok, G. L., Heikes, B. G., Walega, J. G., Lind, J., and Cantrell, C. A.: Chemical Mechanisms of Acid Generation in the Troposphere, Nature, 317, 27–35, 1985. </reference>
		<reference numeration="11" content_type="text"> Cosman, L. M. and Bertram, A. K.: Reactive uptake of N&lt;sub&gt;2&lt;/sub&gt;O$_5$ on aqueous H&lt;sub&gt;2&lt;/sub&gt;SO&lt;sub&gt;4&lt;/sub&gt; solutions coated with 1-component and 2-component monolayers, J. Phys. Chem. A, 112, 4625–4635, 2008. </reference>
		<reference numeration="12" content_type="text"> Cosman, L. M., Knopf, D. A., and Bertram, A. K.: N&lt;sub&gt;2&lt;/sub&gt;O$_5$ reactive uptake on aqueous sulfuric acid solutions coated with branched and straight-chain insoluble organic surfactants, J. Phys. Chem. A, 112, 2386–2396, 2008. </reference>
		<reference numeration="13" content_type="text"> Dentener, F. J. and Crutzen, P. J.: Reaction of N&lt;sub&gt;2&lt;/sub&gt;O$_5$ on tropospheric aerosols – Impact on the global distributions of NO&lt;sub&gt;x&lt;/sub&gt;, O&lt;sub&gt;3&lt;/sub&gt;, and OH, J. Geophys. Res., 98, 7149–7163, 1993. </reference>
		<reference numeration="14" content_type="text"> Evans, M. J. and Jacob, D. J.: Impact of new laboratory studies of N&lt;sub&gt;2&lt;/sub&gt;O$_5$ hydrolysis on global model budgets of tropospheric nitrogen oxides, ozone, and OH, Geophys. Res. Lett., 32, L09813, doi:10.1029/2005GL022469, 2005. </reference>
		<reference numeration="15" content_type="text"> Finlayson-Pitts, B. J., Ezell, M. J., and Pitts, J. N.: Formation of chemically active chlorine compounds by reactions of atmospheric NaCl particles with gaseous N&lt;sub&gt;2&lt;/sub&gt;O$_5$ and ClONO&lt;sub&gt;2&lt;/sub&gt;, Nature, 337, 241–244, 1989. </reference>
		<reference numeration="16" content_type="text"> Folkers, M., Mentel, T. F., and Wahner, A.: Influence of an organic coating on the reactivity of aqueous aerosols probed by the heterogeneous hydrolysis of N&lt;sub&gt;2&lt;/sub&gt;O$_5$, Geophys. Res. Lett., 30(12), 1644, doi:10.1029/2003GL017168, 2003. </reference>
		<reference numeration="17" content_type="text"> Fried, A., Henry, B. E., Calvert, J. G., and Mozurkewich, M.: The reaction probability of N&lt;sub&gt;2&lt;/sub&gt;O$_5$ with sulfuric-acid aerosols at stratospheric temperatures and compositions, J. Geophys. Res., 99, 3517–3532, 1994. </reference>
		<reference numeration="18" content_type="text"> George, I. J., Vlasenko, A., Slowik, J. G., Broekhuizen, K., and Abbatt, J. P. D.: Heterogeneous oxidation of saturated organic aerosols by hydroxyl radicals: uptake kinetics, condensed-phase products, and particle size change, Atmos. Chem. Phys., 7, 4187–4201, 2007. </reference>
		<reference numeration="19" content_type="text"> Gross, S. and Bertram, A. K.: Reactive uptake of NO&lt;sub&gt;3&lt;/sub&gt;, N&lt;sub&gt;2&lt;/sub&gt;O$_5$, NO&lt;sub&gt;2&lt;/sub&gt;, HNO&lt;sub&gt;3&lt;/sub&gt;, and O&lt;sub&gt;3&lt;/sub&gt; on three types of polycyclic aromatic hydrocarbon surfaces, J. Phys. Chem. A, 112, 3104–3113, 2008. </reference>
		<reference numeration="20" content_type="text"> Hanson, D. and Kosciuch, E.: The NH&lt;sub&gt;3&lt;/sub&gt; mass accommodation coefficient for uptake onto sulfuric acid solutions, J. Phys. Chem. A, 107, 2199–2208, 2003. </reference>
		<reference numeration="21" content_type="text"> Hu, J. H. and Abbatt, J. P. D.: Reaction probabilities for N&lt;sub&gt;2&lt;/sub&gt;O$_5$ hydrolysis on sulfuric acid and ammonium sulfate aerosols at room temperature, J. Phys. Chem. A, 101, 871–878, 1997. </reference>
		<reference numeration="22" content_type="text"> Jang, M. S., Czoschke, N. M., Lee, S., and Kamens, R. M.: Heterogeneous atmospheric aerosol production by acid-catalyzed particle-phase reactions, Science, 298, 814–817, 2002. </reference>
		<reference numeration="23" content_type="text"> Jayne, J. T., Leard, D. C., Zhang, X. F., Davidovits, P., Smith, K. A., Kolb, C. E., and Worsnop, D. R.: Development of an aerosol mass spectrometer for size and composition analysis of submicron particles, Aer. Sci. Technol., 33, 49–70, 2000. </reference>
		<reference numeration="24" content_type="text"> Kercher, J. P., Riedel, T. P., and Thornton, J. A.: Chlorine activation by \chemN_2O_5: simultaneous, in situ detection of \chemClNO_2 and \chemN_2O_5 by chemical ionization mass spectrometry, Atmos. Meas. Tech., 2, 193–204, 2009. </reference>
		<reference numeration="25" content_type="text"> Kroll, J. H. and Seinfeld, J. H.: Representation of secondary organic aerosol laboratory chamber data for the interpretation of mechanisms of particle growth, Environ. Sci. Technol., 39, 4159–4165, 2005. </reference>
		<reference numeration="26" content_type="text"> Laskin, A., Wang, H., Robertson, W. H., Cowin, J. P., Ezell, M. J., and Finlayson-Pitts, B. J.: A new approach to determining gas-particle reaction probabilities and application to the heterogeneous reaction of deliquesced sodium chloride particles with gas-phase hydroxyl radicals, J. Phys. Chem. A, 110, 10 619–10 627, 2006. </reference>
		<reference numeration="27" content_type="text"> Mak, J., Gross, S., and Bertram, A. K.: Uptake of NO&lt;sub&gt;3&lt;/sub&gt; on soot and pyrene surfaces, Geophys. Res. Lett., 34, L10804, doi:10.1029/2007GL029756, 2007. </reference>
		<reference numeration="28" content_type="text"> Martin, S. T., Rosenoern, T., Chen, Q., and Collins, D. R.: Phase Changes of Ambient Particles in the Southern Great Plains of Oklahoma, USA, J. Geophys. Res., 35, L22801, doi:10.1029/2008GL035650, 2008. </reference>
		<reference numeration="29" content_type="text"> McNeill, V. F., Patterson, J., Wolfe, G. M., and Thornton, J. A.: The effect of varying levels of surfactant on the reactive uptake of \chemN_2O_5 to aqueous aerosol, Atmos. Chem. Phys., 6, 1635–1644, 2006. </reference>
		<reference numeration="30" content_type="text"> McNeill, V. F., Yatavelli, R. L. N., Stipe, C. B., and Landgrebe, O.: Heterogeneous OH oxidation of palmitic acid in single component and internally mixed aerosol particles: vaporization and the role of particle phase, Atmos. Chem. Phys., 8, 5465–5476, 2008. </reference>
		<reference numeration="31" content_type="text"> Mentel, T. F., Sohn, M., and Wahner, A.: Nitrate effect in the heterogeneous hydrolysis of dinitrogen pentoxide on aqueous aerosols, Phys. Chem. Chem. Phys., 1, 5451–5457, 1999. </reference>
		<reference numeration="32" content_type="text"> Molina, M. J., Ivanov, A. V., Trakhtenberg, S., and Molina, L. T.: Atmospheric evolution of organic aerosol, Geophys. Res. Lett., 31, L22104, doi:10.1029/2004GL020910, 2004. </reference>
		<reference numeration="33" content_type="text"> Mozurkewich, M. and Calvert, J. G.: Reaction probability of N&lt;sub&gt;2&lt;/sub&gt;O$_5$ on aqueous aerosols, J. Geophys. Res., 93, 15 889–15 896, 1988. </reference>
		<reference numeration="34" content_type="text"> Murphy, D. M. and Thomson, D. S.: Laser Ionization Mass-Spectroscopy of Single Aerosol-Particles, Aerosol. Sci. Tech., 22, 237–249, 1995. </reference>
		<reference numeration="35" content_type="text"> Osthoff, H. D., Roberts, J. M., Ravishankara, A. R., Williams, E. J., Lerner, B. M., Sommariva, R., Bates, T. S., Coffman, D., Quinn, P. K., Dibb, J. E., Stark, H., Burkholder, J. B., Talukdar, R. K., Meagher, J., Fehsenfeld, F. C., and Brown, S. S.: High levels of nitryl chloride in the polluted subtropical marine boundary layer, Nat. Geosci., 1, 324–328, 2008. </reference>
		<reference numeration="36" content_type="text"> Park, S. C., Burden, D. K., and Nathanson, G. M.: The inhibition of N&lt;sub&gt;2&lt;/sub&gt;O$_5$ hydrolysis in sulfuric acid by 1-butanol and 1-hexanol surfactant coatings, J. Phys. Chem. A, 111, 2921–2929, 2007. </reference>
		<reference numeration="37" content_type="text"> Ravishankara, A. R.: Heterogeneous and multiphase chemistry in the troposphere, Science, 276, 1058–1065, 1997. </reference>
		<reference numeration="38" content_type="text"> Robinson, G. N., Worsnop, D. R., Jayne, J. T., Kolb, C. E., and Davidovits, P.: Heterogeneous uptake of ClONO&lt;sub&gt;2&lt;/sub&gt; and N&lt;sub&gt;2&lt;/sub&gt;O$_5$ by sulfuric acid solutions, J. Geophys. Res., 102, 3583–3601, 1997. </reference>
		<reference numeration="39" content_type="text"> Sioutas, C., Koutrakis, P., Ferguson, S. T., and Burton, R. M.: Development and Evaluation of a Prototype Ambient Particle Concentrator for Inhalation Exposure Studies, Inhal. Toxicol., 7, 633–644, 1995. </reference>
		<reference numeration="40" content_type="text"> Thornton, J. and Abbatt, J. P. D.: Measurements of HO&lt;sub&gt;2&lt;/sub&gt; uptake to aqueous aerosol: Mass accommodation coefficients and net reactive loss, J. Geophys. Res., 110, D08309, doi:10.1029/2004JD005402, 2005a. </reference>
		<reference numeration="41" content_type="text"> Thornton, J. A. and Abbatt, J. P. D.: N&lt;sub&gt;2&lt;/sub&gt;O$_5$ reaction on submicron sea salt aerosol: Kinetics, products, and the effect of surface active organics, J. Phys. Chem. A, 109, 10 004–10 012, 2005b. </reference>
		<reference numeration="42" content_type="text"> Thornton, J. A., Braban, C. F., and Abbatt, J. P. D.: N&lt;sub&gt;2&lt;/sub&gt;O$_5$ hydrolysis on sub-micron organic aerosols: the effect of relative humidity, particle phase, and particle size, Phys. Chem. Chem. Phys., 5, 4593–4603, 2003. </reference>
		<reference numeration="43" content_type="text"> Vlasenko, A., George, I. J., and Abbatt, J. P. D.: Formation of volatile organic compounds in the heterogeneous oxidation of condensed-phase organic films by gas-phase OH, J. Phys. Chem. A, 112, 1552–1560, 2008. </reference>
		<reference numeration="44" content_type="text"> Vogt, R. and Finlayson-Pitts, B. J.: A Diffuse-Reflectance Infrared Fourier-Transform Spectroscopic (Drifts) Study of the Surface-Reaction of NaCl with Gaseous NO&lt;sub&gt;2&lt;/sub&gt; and HNO&lt;sub&gt;3&lt;/sub&gt;, J. Phys. Chem., 98, 3747–3755, 1994. </reference>
		<reference numeration="45" content_type="text"> Wahner, A., Mentel, T. F., Sohn, M., and Stier, J.: Heterogeneous reaction of N&lt;sub&gt;2&lt;/sub&gt;O$_5$ on sodium nitrate aerosol, J. Geophys. Res., 103, 31 103–31 112, 1998. </reference>
		<reference numeration="46" content_type="text"> Wang, J., Hoffmann, A. A., Park, R. J., Jacob, D. J., and Martin, S. T.: Global distribution of solid and aqueous sulfate aerosols: Effect of the hysteresis of particle phase transitions, J. Geophys. Res., 113, D11206, doi:10.1029/2007JD009367, 2008. </reference>
	</references>
</article>

