TY - JOUR
T1 - Ozonolysis of mixed oleic-acid/stearic-acid particles
T2 - Reaction kinetics and chemical morphology
AU - Katrib, Y.
AU - Biskos, G.
AU - Buseck, P R
AU - Davidovits, P.
AU - Jayne, J. T.
AU - Mochida, M.
AU - Wise, M. E.
AU - Worsnop, D. R.
AU - Martin, S. T.
PY - 2005/12/8
Y1 - 2005/12/8
N2 - The ozonolysis of mixed oleic-acid/stearic-acid (OL/SA) aerosol particles from 0/100 to 100/0 wt % composition is studied. The magnitude of the divergence of the particle beam inside an aerosol mass spectrometer shows that, in the concentration range 100/0 to 60/40, the mixed OL/SA particles are liquid prior to reaction. Upon ozonolysis, particles having compositions of 75/25 and 60/40 change shape, indicating that they have solidified during reaction. Transmission electron micrographs show that SA(s) forms needles. For particles having compositions of 75/25, 60/40, and greater SA content, the reaction kinetics exhibit an initial fast decay of OL for low O 3 exposure with no further loss of OL at higher O 3 exposures. For compositions from 50/50 to 10/90, the residual OL concentration remains at 28 ± 2% of its initial value. The initial reactive uptake coefficient for O 3, as determined by OL loss, decreases linearly from 1.25 (±0.2) × 10 -3 to 0.60 (±0.15) × 10 -3 for composition changes of 100/0 to 60/40. At 50/50 composition, the uptake coefficient drops abruptly to 0.15 (±0.1) × 10 -3, and there are no further changes with increased SA content. These observations can be explained with a combination of three postulates: (1) Unreacted mixed particles remain as supersaturated liquids up to 60/40 composition, and the OL in this form rapidly reacts with O 3. (2) SA, as it solidifies, locks into its crystal structure a significant amount of OL, and this OL is completely inaccessible to O 3. (3) Accompanying crystallization, some stearic acid molecules connect as a filamentous network to form a semipermeable gel containing liquid OL but with a reduced uptake coefficient because of the decrease in molecular diffusivity in the gel. An individual particle of 50/50 to 90/10 is hypothesized as a combination of SA crystals having OL impurities (postulate 2) that are partially enveloped by an SA/OL gel (postulate 3) to explain (a) the abrupt drop in the uptake coefficient from 60/40 to 50/50 and (b) the residual OL content even after high ozone exposure. The results of this study, pointing out the important effects of particle phase, composition, and morphology on chemical reactivity, contribute to an improved understanding of the aging processes of atmospheric aerosol particles.
AB - The ozonolysis of mixed oleic-acid/stearic-acid (OL/SA) aerosol particles from 0/100 to 100/0 wt % composition is studied. The magnitude of the divergence of the particle beam inside an aerosol mass spectrometer shows that, in the concentration range 100/0 to 60/40, the mixed OL/SA particles are liquid prior to reaction. Upon ozonolysis, particles having compositions of 75/25 and 60/40 change shape, indicating that they have solidified during reaction. Transmission electron micrographs show that SA(s) forms needles. For particles having compositions of 75/25, 60/40, and greater SA content, the reaction kinetics exhibit an initial fast decay of OL for low O 3 exposure with no further loss of OL at higher O 3 exposures. For compositions from 50/50 to 10/90, the residual OL concentration remains at 28 ± 2% of its initial value. The initial reactive uptake coefficient for O 3, as determined by OL loss, decreases linearly from 1.25 (±0.2) × 10 -3 to 0.60 (±0.15) × 10 -3 for composition changes of 100/0 to 60/40. At 50/50 composition, the uptake coefficient drops abruptly to 0.15 (±0.1) × 10 -3, and there are no further changes with increased SA content. These observations can be explained with a combination of three postulates: (1) Unreacted mixed particles remain as supersaturated liquids up to 60/40 composition, and the OL in this form rapidly reacts with O 3. (2) SA, as it solidifies, locks into its crystal structure a significant amount of OL, and this OL is completely inaccessible to O 3. (3) Accompanying crystallization, some stearic acid molecules connect as a filamentous network to form a semipermeable gel containing liquid OL but with a reduced uptake coefficient because of the decrease in molecular diffusivity in the gel. An individual particle of 50/50 to 90/10 is hypothesized as a combination of SA crystals having OL impurities (postulate 2) that are partially enveloped by an SA/OL gel (postulate 3) to explain (a) the abrupt drop in the uptake coefficient from 60/40 to 50/50 and (b) the residual OL content even after high ozone exposure. The results of this study, pointing out the important effects of particle phase, composition, and morphology on chemical reactivity, contribute to an improved understanding of the aging processes of atmospheric aerosol particles.
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U2 - 10.1021/jp054714d
DO - 10.1021/jp054714d
M3 - Article
C2 - 16331935
AN - SCOPUS:29444456362
SN - 1089-5639
VL - 109
SP - 10910
EP - 10919
JO - Journal of Physical Chemistry A
JF - Journal of Physical Chemistry A
IS - 48
ER -