A. L. Vlasenko
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Featured researches published by A. L. Vlasenko.
Journal of Physical Chemistry A | 2008
A. L. Vlasenko; I. J. George; Jonathan P. D. Abbatt
The yield of volatile organic compounds (VOCs) from the heterogeneous oxidation of condensed-phase organic and hydrocarbon soot films by gas-phase OH has been studied in a coated-wall flow tube at room temperature. Simultaneously, OH concentrations are measured using a chemical-ionization mass spectrometer (CIMS) operated in negative ion mode and VOCs are measured using a commercial proton-transfer-reaction mass spectrometer (PTR-MS). It is observed that a variety of aldehydes/carbonyls and carboxylic acids are formed. Specifically, detailed experiments were conducted with stearic acid, where products are observed that contain as many as 13 carbon atoms with the average carbon number of the products between 3 and 5. The yield of VOCs, relative to the loss of OH radicals, is strongly dependent on the partial pressure of O2 in the carrier gas, ranging from 0.08 +/- 0.03 in a nominally pure He carrier gas to 0.34 +/- 0.14 in 6 Torr of pure O2. Yields from other organics are somewhat lower than those from stearic acid, ranging in conditions of pure O2 from 0.10 +/- 0.04 for BES (bis(ethylhexyl)sebacate), to 0.03 +/- 0.01 for n-hexane soot, to 0.01 +/- 0.005 for pyrene. Under atmospheric conditions, OH oxidation of select organics may be an efficient source of small VOCs. In particular, formic acid is formed in significant yield from all the surfaces.
Environmental Science & Technology | 2013
Jeremy J. B. Wentzell; John Liggio; Shao-Meng Li; A. L. Vlasenko; Ralf M. Staebler; Gang Lu; Marie-Josée Poitras; Tak W. Chan; Jeffrey R. Brook
Gas-phase acids in light duty diesel (LDD) vehicle exhaust were measured using chemical ionization mass spectrometry (CIMS). Fuel based emission factors (EF) and NOx ratios for these species were determined under differing steady state engine operating conditions. The derived HONO and HNO3 EFs agree well with literature values, with HONO being the single most important acidic emission. Of particular importance is the quantification of the EF for the toxic species, isocyanic acid (HNCO). The emission factors for HNCO ranged from 0.69 to 3.96 mg kgfuel(-1), and were significantly higher than previous biomass burning emission estimates. Further ambient urban measurements of HNCO demonstrated a clear relationship with the known traffic markers of benzene and toluene, demonstrating for the first time that urban commuter traffic is a source of HNCO. Estimates based upon the HNCO-benzene relationship indicate that upward of 23 tonnes of HNCO are released annually from commuter traffic in the Greater Toronto Area, far exceeding the amount possible from LDD alone. Nationally, 250 to 770 tonnes of HNCO may be emitted annually from on-road vehicles, likely representing the dominant source of exposure in urban areas, and with emissions comparable to that of biomass burning.
Environmental Science & Technology | 2011
John Liggio; Shao-Meng Li; A. L. Vlasenko; Craig Stroud; Paul A. Makar
The neutralization of acidic aerosols by ammonia has been studied through experiments which combine ambient air with laboratory generated sulfuric acid aerosol. Results indicated that acidic aerosol mixed with organic free air and ammonia was neutralized on a time scale<1 min, consistent with expectations. However, in the presence of ambient organic gases and ammonia, the rate of aerosol neutralization is significantly reduced. This reduction in ammonia uptake was concurrent with an increase in the amount of particle phase organics. A steady state in the NH4+/SO4(2-) in the presence of organic gases was established on time scales of 10 min to several hours, corresponding to NH3 uptake coefficients in the range of 4×10(-3)-2×10(-4). The degree to which neutralization was slowed was dependent upon the initial ammonia concentration and the organic mass added to the aerosols. These results suggest that inorganic equilibrium thermodynamic models may overestimate the rate of ammonia uptake and that ambient particles may remain acidic for longer than previously expected.
Environmental Science & Technology | 2018
Matthew M. Coggon; Brian C. McDonald; A. L. Vlasenko; P. R. Veres; François Bernard; Abigail Koss; Bin Yuan; J. B. Gilman; J. Peischl; K. C. Aikin; Justin DuRant; Carsten Warneke; Shao-Meng Li; Joost A. de Gouw
Decamethylcyclopentasiloxane (D5) is a cyclic volatile methyl siloxane (cVMS) that is widely used in consumer products and commonly observed in urban air. This study quantifies the ambient mixing ratios of D5 from ground sites in two North American cities (Boulder, CO, USA, and Toronto, ON, CA). From these data, we estimate the diurnal emission profile of D5 in Boulder, CO. Ambient mixing ratios were consistent with those measured at other urban locations; however, the diurnal pattern exhibited similarities with those of traffic-related compounds such as benzene. Mobile measurements and vehicle experiments demonstrate that emissions of D5 from personal care products are coincident in time and place with emissions of benzene from motor vehicles. During peak commuter times, the D5/benzene ratio (w/w) is in excess of 0.3, suggesting that the mass emission rate of D5 from personal care product usage is comparable to that of benzene due to traffic. The diurnal emission pattern of D5 is estimated using the measured D5/benzene ratio and inventory estimates of benzene emission rates in Boulder. The hourly D5 emission rate is observed to peak between 6:00 and 7:00 AM and subsequently follow an exponential decay with a time constant of 9.2 h. This profile could be used by models to constrain temporal emission patterns of personal care products.
Atmospheric Chemistry and Physics | 2011
Jeffrey R. Pierce; W. R. Leaitch; John Liggio; D. M. Westervelt; C. D. Wainwright; J. P. D. Abbatt; Lars Ahlm; W. Al-Basheer; Daniel J. Cziczo; K. L. Hayden; Alex K. Y. Lee; S.-M. Li; Lynn M. Russell; Steve Sjostedt; K. B. Strawbridge; M. Travis; A. L. Vlasenko; Jeremy J. B. Wentzell; H. A. Wiebe; J. P. S. Wong; A. M. Macdonald
Atmospheric Chemistry and Physics | 2013
T. P. Riedel; Glenn M. Wolfe; K. T. Danas; J. B. Gilman; William C. Kuster; D. M. Bon; A. L. Vlasenko; S.-M. Li; Eric J. Williams; P. R. Veres; James M. Roberts; John S. Holloway; Barry Lefer; Steven S. Brown; Judith Thornton
Journal of Geophysical Research | 2012
Nicholas L. Wagner; T. P. Riedel; James M. Roberts; Joel A. Thornton; Wayne M. Angevine; Eric J. Williams; A. L. Vlasenko; S.-M. Li; William P. Dubé; D. J. Coffman; D. M. Bon; J. A. de Gouw; William C. Kuster; J. B. Gilman; Steven S. Brown
Atmospheric Environment | 2011
W. Richard Leaitch; A. M. Macdonald; Peter C. Brickell; John Liggio; Steve Sjostedt; A. L. Vlasenko; J. W. Bottenheim; Lin Huang; Shao-Meng Li; Peter S. Liu; Desiree Toom-Sauntry; K. Hayden; Sangeeta Sharma; Nicole C. Shantz; H. Allan Wiebe; Wendy Zhang; Jonathan P. D. Abbatt; Jay G. Slowik; Rachel Chang; Lynn M. Russell; Rachel E. Schwartz; Satoshi Takahama; John T. Jayne; Nga L. Ng
Atmospheric Chemistry and Physics | 2013
S. Zhou; L. Gonzalez; Amy Leithead; Z. Finewax; Ryan Thalman; A. L. Vlasenko; S. Vagle; Lisa A. Miller; S.-M. Li; S. Bureekul; Hiroshi Furutani; Mitsuo Uematsu; R. Volkamer; J. P. D. Abbatt
Journal of Geophysical Research | 2010
John Liggio; Shao-Meng Li; A. L. Vlasenko; Steve Sjostedt; Rachel Chang; Nicole C. Shantz; Jonathan P. D. Abbatt; Jay G. Slowik; J. W. Bottenheim; P. C. Brickell; Craig Stroud; W. Richard Leaitch