Fluxes of Atmospheric Greenhouse-Gases in Maryland (FLAGG-MD): Emissions of Carbon Dioxide in the Baltimore, MD-Washington, D.C. area.

To study emissions of CO2 in the Baltimore, MD-Washington, D.C. (Balt-Wash) area, an aircraft campaign was conducted in February 2015, as part of the FLAGG-MD (Fluxes of Atmospheric Greenhouse-Gases in Maryland) project. During the campaign, elevated mole fractions of CO2 were observed downwind of the urban center and local power plants. Upwind flight data and HYSPLIT (Hybrid Single Particle Lagrangian Integrated Trajectory) model analyses help account for the impact of emissions outside the Balt-Wash area. The accuracy, precision, and sensitivity of CO2 emissions estimates based on the mass balance approach were assessed for both power plants and cities. Our estimates of CO2 emissions from two local power plants agree well with their CEMS (Continuous Emissions Monitoring Systems) records. For the 16 power plant plumes captured by the aircraft, the mean percentage difference of CO2 emissions was -0.3 %. For the Balt-Wash area as a whole, the 1σ CO2 emission rate uncertainty for any individual aircraft-based mass balance approach experiment was ±38 %. Treating the mass balance experiments, which were repeated seven times within nine days, as individual quantifications of the Balt-Wash CO2 emissions, the estimation uncertainty was ±16 % (standard error of the mean at 95% CL). Our aircraft-based estimate was compared to various bottom-up fossil fuel CO2 (FFCO2) emission inventories. Based on the FLAGG-MD aircraft observations, we estimate 1.9±0.3 MtC of FFCO2 from the Balt-Wash area during the month of February 2015. The mean estimate of FFCO2 from the four bottom-up models was 2.2±0.3 MtC.

Organic nitrate chemistry and its implications for nitrogen budgets in an isoprene- and monoterpene-rich atmosphere: constraints from aircraft (SEAC4RS) and ground-based (SOAS) observations in the Southeast US.

Formation of organic nitrates (RONO2) during oxidation of biogenic volatile organic compounds (BVOCs: isoprene, monoterpenes) is a significant loss pathway for atmospheric nitrogen oxide radicals (NOx), but the chemistry of RONO2 formation and degradation remains uncertain. Here we implement a new BVOC oxidation mechanism (including updated isoprene chemistry, new monoterpene chemistry, and particle uptake of RONO2) in the GEOS-Chem global chemical transport model with ∼25 × 25 km2 resolution over North America. We evaluate the model using aircraft (SEAC4RS) and ground-based (SOAS) observations of NOx, BVOCs, and RONO2 from the Southeast US in summer 2013. The updated simulation successfully reproduces the concentrations of individual gas- and particle-phase RONO2 species measured during the campaigns. Gas-phase isoprene nitrates account for 25-50% of observed RONO2 in surface air, and we find that another 10% is contributed by gas-phase monoterpene nitrates. Observations in the free troposphere show an important contribution from long-lived nitrates derived from anthropogenic VOCs. During both campaigns, at least 10% of observed boundary layer RONO2 were in the particle phase. We find that aerosol uptake followed by hydrolysis to HNO3 accounts for 60% of simulated gas-phase RONO2 loss in the boundary layer. Other losses are 20% by photolysis to recycle NOx and 15% by dry deposition. RONO2 production accounts for 20% of the net regional NOx sink in the Southeast US in summer, limited by the spatial segregation between BVOC and NOx emissions. This segregation implies that RONO2 production will remain a minor sink for NOx in the Southeast US in the future even as NOx emissions continue to decline.

Development of an automated cylindrical ion trap mass spectrometer for the determination of atmospheric volatile organic compounds.

Volatile organic compounds released from the biosphere are known to have a large impact on atmospheric chemistry. Field instruments for the detection of these trace gases are often limited by the lack of instrument portability and the inability to distinguish compounds of interest from background or other interfering compounds. We have developed an automated sampling and preconcentration system, coupled to a lightweight, low-power cylindrical ion trap mass spectrometer. The instrument was evaluated by measuring isoprene concentrations during a field campaign at the University of Michigan Biological Station PROPHET lab. Isoprene was preconcentrated by sampling directly into a short capillary column precooled without the aid of cryogens. The capillary column was then rapidly heated by moving the column to a preheated region to obtain fast separation of isoprene from other components, followed by detection with a cylindrical ion trap. This combination yielded a detection limit of approximately 80 ppt (parts per trillion) for isoprene with a measurement frequency of one sample every 11 min. The data obtained by the automated sampling and preconcentration system during the PROPHET 2005 campaign were compared to those of other field instruments measuring isoprene at this site in an intercomparison exercise. The intercomparisons suggest the new inlet system, when coupled with this ion trap detector, provides a viable field instrument for the fast, precise, and quantitative determination of isoprene and other trace gases over a variety of atmospheric conditions.

The role of Br2 and BrCl in surface ozone destruction at polar sunrise.

Bromine atoms are believed to play a central role in the depletion of surface-level ozone in the Arctic at polar sunrise. Br2, BrCl, and HOBr have been hypothesized as bromine atom precursors, and there is evidence for chlorine atom precursors as well, but these species have not been measured directly. We report here measurements of Br2, BrCl, and Cl2 made using atmospheric pressure chemical ionization-mass spectrometry at Alert, Nunavut, Canada. In addition to Br2 at mixing ratios up to approximately 25 parts per trillion, BrCl was found at levels as high as approximately 35 parts per trillion. Molecular chlorine was not observed, implying that BrCl is the dominant source of chlorine atoms during polar sunrise, consistent with recent modeling studies. Similar formation of bromine compounds and tropospheric ozone destruction may also occur at mid-latitudes but may not be as apparent owing to more efficient mixing in the boundary layer.

Mutagenicity of peroxyacetyl nitrate (PAN) in vivo: tests for somatic mutations and chromosomal aberrations.

A series of experiments was conducted in which Chinese hamsters inhaled PAN, an ubiquitous pollutant that is present in the atmosphere at concentrations that are as high as, or higher than, other known genotoxic agents. The animals were exposed to PAN in air at concentrations of approximately 3 ppm for up to 1 month and then examined for somatic mutations and chromosomal aberrations. Mutations were assayed by measuring the frequency of thioguanine-resistant lung fibroblasts (isolated de novo and cultured). Chromosomal aberrations were assayed by measuring the frequency of micronuclei in either the bone marrow (polychromatic erythrocytes) or the lungs (binucleate lung fibroblasts cultured in the presence of cytochalasin B). The results for the test animals were compared to those from animals exposed similarly, but without PAN. Although in each experiment the mutation frequencies for the test animals were higher than the corresponding controls, the mutation frequencies were not significantly different from the concurrent negative controls (P > .05) or the historical controls, except for experiment C. In experiment C, there was a significant regression of mutation frequency versus dose (P < 0.001) if all of the historical controls for pooled animals are included at zero dose. No reproducible evidence of chromosomal breakage was found in either lung or bone marrow. Thus, although PAN has been found to be a bacterial mutagen, we did not find statistically significant evidence of mutagenicity in vivo. The toxicity of PAN limited the exposure concentration that could be used. When all of the PAN data were used, the best estimate of the mutagenic potency proved to be comparable to that of ethylene dibromide, a carcinogenic atmospheric pollutant.

Comparison of mutagenic activities of several peroxyacyl nitrates.

Salmonella typhimurium, strain TA100 was exposed to a series of peroxyacyl nitrates including peroxyacetyl nitrate (PAN), peroxypropionyl nitrate (PPN), peroxybutyryl nitrate (PBN), peroxybenzoyl nitrate (PBzN), and chloroperoxyacetyl nitrate (CPAN). Gas-phase concentrations for the individual exposures were in the high part per billion by volume ppbv range. The dose was determined from the deposition rate and measured from the net decrease of the test compound in the exposure chamber and the exposure time. The mutagenic activity for each compound determined from the dose-response relationship gave values ranging from 250 (PBN) to 6,500 (PBzN) revertants/mumols. The mutagenic activity for CPAN could not be determined, due to an interference from chloroacetaldehyde. The difficulties of quantifying the actual gas-phase chemical dose the bacteria are exposed to in this variant of the Ames test are delineated.

Peroxyacetyl nitrate: measurement of its mutagenic activity using the Salmonella/mammalian microsome reversion assay.

Exposures of Salmonella typhimurium strain TA100 with and without S9 metabolic activation to low ppm levels of pure peroxyacetyl nitrate (PAN) in the gas phase were conducted. Measurements of the gas-phase PAN exposure concentration and the concentration of its decomposition products in surrogate test media led to a measured mutagenic activity of 34 +/- 5 revertants/mumole. The data indicate that PAN is a relatively weak direct-acting mutagen with TA100.