The uptake of O3 by myristic acid- oleic acid mixed particles : evidence for solid surface layers

• Published in: Physical chemistry chemical physics : PCCP 2006-10, Vol.8 (38), p.4468-4475
• Main Authors: NASH, David G, TOLOCKA, Michael P, BAER, Tomas
• Format: Article
• Language: English
• Subjects: Chemistry; Colloidal state and disperse state; Crystallization; Exact sciences and technology; General and physical chemistry; Mass Spectrometry - instrumentation; Mass Spectrometry - methods; Myristic Acid - chemistry; Oleic Acid - chemistry; Ozone - chemistry; Particle Size; Physical and chemical studies. Granulometry. Electrokinetic phenomena; Sensitivity and Specificity; Surface Properties; Time Factors
• ISSN: 1463-9076; 1463-9084
• DOI: 10.1039/b609855j

The oleic acid ozonolysis in mixed oleic and myristic acid particles was studied in a flow tube reactor using single particle mass spectrometry. The change in reactivity was investigated as a function of the myristic acid concentration in these 2 micron particles. For pure oleic acid aerosol, the reactive ozone uptake coefficient, gamma, was found to be 3.4 (+/-0.3) x 10(-4) after taking secondary reactions into account. At the myristic acid crystallization point, where only 2.5% of the particle is in the solid phase, the uptake coefficient was reduced to 9.7 (+/-1.0) x 10(-5). This dramatic drop in the uptake coefficient is explained by the presence of a crystalline monolayer of myristic acid, through which ozone diffusion is reduced by several orders of magnitude, relative to liquid oleic acid. Scanning electron microscope images of the mixed particles confirm that the particle surface is crystalline when the myristic acid mole fraction exceeds 0.125. The findings of these experiments illustrate that particle morphology is important to understanding the reactivity of species in a mixed particle. The decay of myristic acid during the course of ozonolysis is explained in terms of a reaction with stabilized Criegee intermediates, which attack the acidic groups of the oleic and myristic acids with equal rate constants.