A33M-04:
Online Measurements of Highly Oxidized Organics in the Gas and Particle phase during SOAS and SENEX
Wednesday, 17 December 2014: 2:25 PM
Felipe Lopez-Hilfiker1, Ben H Lee2, Claudia Mohr1, Mikael Ehn3, Florian Rubach4, Thomas F Mentel5, Einhard Kleist4 and Joel A Thornton2, (1)University of Washington Seattle Campus, Seattle, WA, United States, (2)Univ Washington - Seattle, Seattle, WA, United States, (3)University of Helsinki, Helsinki, Finland, (4)Forschungszentrum Jülich, Jülich, Germany, (5)IEK-8-Troposphere, Juelich, Germany
Abstract:
We present measurements of a large suite of gas and particle phase organic compounds made with a Filter Inlet for Gas and AEROsol (FIGAERO) coupled to a high resolution time of flight chemical ionization mass spectrometer (HR-ToF-CIMS) developed at the University of Washington and with airborne HR-ToF-CIMS measurements. The FIGAERO instrument was deployed on the Jülich Plant Atmosphere Chamber to study α-pinene oxidation, and subsequently at the SMEAR II forest station in Hyytiälä, Finland and the SOAS ground site, in Brent Alabama. During the Southern Atmosphere Study, a gas-phase only version of the HR-ToF-CIMS was deployed on the NOAA WP-3 aircraft as part of SENEX. We focus here on highly oxygenated organic compounds derived from monoterpene oxidation detected both aloft during SENEX and at the ground-based site during SOAS. In both chamber and the atmosphere, many highly oxidized, low volatility compounds were observed in the gas and particles and many of the same compositions detected in the gas-phase were detected in the particles upon temperature programmed thermal desorption. The fraction of a given compound measured in the particle phase follows expected trends with elemental composition such as O/C ratios, but many compounds would not be well described by an absorptive partitioning model assuming unity activity coefficients. The detailed structure in the thermograms reveals a significant contribution from large molecular weight organics and/or oligomers in both chamber and ambient aerosol samples. Approximately 50% of the measured organics in the particle phase are associated with compounds having effective vapour pressures 4 or more orders of magnitude lower than commonly measured monoterpene oxidation products. We discuss the implications of these findings for measurements of gas-particle partitioning and for evaluating the contribution of monoterpene oxidation to organic aerosol formation and growth. We also use the aircraft measurements and a steady state model to estimate the yield of such highly oxidized compounds from monoterpene oxidation.