Factors Influencing the Formation of Nitrous Acid from Photolysis of Particulate Nitrate

Enhanced photolysis of particulate nitrate (pNO3) to form photolabile species, such as gas-phase nitrous acid (HONO), has been proposed as a potential mechanism to recycle nitrogen oxides (NOx) in the remote boundary layer ("renoxification"). This article presents a series of laboratory experiments aimed at investigating the parameters that control the photolysis of pNO3 and the efficiency of HONO production. Filters on which artificial or ambient particles had been sampled were exposed to the light of a solar simulator, and the formation of HONO was monitored under controlled laboratory conditions. The results indicate that the photolysis of pNO3 is enhanced, compared to the photolysis of gas-phase HNO3, at low pNO3 levels, with the enhancement factor reducing at higher pNO3 levels. The presence of cations (Na+) and halides (Cl-) and photosensitive organic compounds (imidazole) also enhance pNO3 photolysis, but other organic compounds such as oxalate and succinic acid have the opposite effect. The precise role of humidity in pNO3 photolysis remains unclear. While the efficiency of photolysis is enhanced in deliquescent particles compared to dry particles, some of the experimental results suggest that this may not be the case for supersaturated particles. These experiments suggest that both the composition and the humidity of particles control the enhancement of particulate nitrate photolysis, potentially explaining the variability in results among previous laboratory and field studies. HONO observations in the remote marine boundary layer can be explained by a simple box-model that includes the photolysis of pNO3, in line with the results presented here, although more experimental work is needed in order to derive a comprehensive parametrization of this process.

Effects of halogens on European air-quality

Halogens (Cl, Br) have a profound influence on stratospheric ozone (O₃). They (Cl, Br and I) have recently also been shown to impact the troposphere, notably by reducing the mixing ratios of O₃ and OH. Their potential for impacting regional air-quality is less well understood. We explore the impact of halogens on regional pollutants (focussing on O₃) with the European grid of the GEOS-Chem model (0.25° × 0.3125°). It has recently been updated to include a representation of halogen chemistry. We focus on the summer of 2015 during the ICOZA campaign at the Weybourne Atmospheric Observatory on the North Sea coast of the UK. Comparisons between these observations together with those from the UK air-quality network show that the model has some skill in representing the mixing ratios/concentration of pollutants during this period. Although the model has some success in simulating the Weybourne ClNO₂ observations, it significantly underestimates ClNO₂ observations reported at inland locations. It also underestimates mixing ratios of IO, OIO, I₂ and BrO, but this may reflect the coastal nature of these observations. Model simulations, with and without halogens, highlight the processes by which halogens can impact O₃. Throughout the domain O₃ mixing ratios are reduced by halogens. In northern Europe this is due to a change in the background O₃ advected into the region, whereas in southern Europe this is due to local chemistry driven by Mediterranean emissions. The proportion of hourly O₃ above 50 nmol mol^-1 in Europe is reduced from 46% to 18% by halogens. ClNO₂ from N₂O₅ uptake onto sea-salt leads to increases in O₃ mixing ratio, but these are smaller than the decreases caused by the bromine and iodine. 12% of ethane and 16% of acetone within the boundary layer is oxidised by Cl. Aerosol response to halogens is complex with small (∼10%) reductions in PM_2.5 in most locations. A lack of observational constraints coupled to large uncertainties in emissions and chemical processing of halogens make these conclusions tentative at best. However, the results here point to the potential for halogen chemistry to influence air quality policy in Europe and other parts of the world.

The Convective Transport of Active Species in the Tropics (CONTRAST) Experiment

The Convective Transport of Active Species in the Tropics (CONTRAST) experiment was conducted from Guam (13.5° N, 144.8° E) during January-February 2014. Using the NSF/NCAR Gulfstream V research aircraft, the experiment investigated the photochemical environment over the tropical western Pacific (TWP) warm pool, a region of massive deep convection and the major pathway for air to enter the stratosphere during Northern Hemisphere (NH) winter. The new observations provide a wealth of information for quantifying the influence of convection on the vertical distributions of active species. The airborne in situ measurements up to 15 km altitude fill a significant gap by characterizing the abundance and altitude variation of a wide suite of trace gases. These measurements, together with observations of dynamical and microphysical parameters, provide significant new data for constraining and evaluating global chemistry climate models. Measurements include precursor and product gas species of reactive halogen compounds that impact ozone in the upper troposphere/lower stratosphere. High accuracy, in-situ measurements of ozone obtained during CONTRAST quantify ozone concentration profiles in the UT, where previous observations from balloon-borne ozonesondes were often near or below the limit of detection. CONTRAST was one of the three coordinated experiments to observe the TWP during January-February 2014. Together, CONTRAST, ATTREX and CAST, using complementary capabilities of the three aircraft platforms as well as ground-based instrumentation, provide a comprehensive quantification of the regional distribution and vertical structure of natural and pollutant trace gases in the TWP during NH winter, from the oceanic boundary to the lower stratosphere.

Multiannual observations of acetone, methanol, and acetaldehyde in remote tropical atlantic air: implications for atmospheric OVOC budgets and oxidative capacity

Oxygenated volatile organic compounds (OVOCs) in the atmosphere are precursors to peroxy acetyl nitrate (PAN), affect the tropospheric ozone budget, and in the remote marine environment represent a significant sink of the hydroxyl radical (OH). The sparse observational database for these compounds, particularly in the tropics, contributes to a high uncertainty in their emissions and atmospheric significance. Here, we show measurements of acetone, methanol, and acetaldehyde in the tropical remote marine boundary layer made between October 2006 and September 2011 at the Cape Verde Atmospheric Observatory (CVAO) (16.85° N, 24.87° W). Mean mixing ratios of acetone, methanol, and acetaldehyde were 546 ± 295 pptv, 742 ± 419 pptv, and 428 ± 190 pptv, respectively, averaged from approximately hourly values over this five-year period. The CAM-Chem global chemical transport model reproduced annual average acetone concentrations well (21% overestimation) but underestimated levels by a factor of 2 in autumn and overestimated concentrations in winter. Annual average concentrations of acetaldehyde were underestimated by a factor of 10, rising to a factor of 40 in summer, and methanol was underestimated on average by a factor of 2, peaking to over a factor of 4 in spring. The model predicted summer minima in acetaldehyde and acetone, which were not apparent in the observations. CAM-Chem was adapted to include a two-way sea-air flux parametrization based on seawater measurements made in the Atlantic Ocean, and the resultant fluxes suggest that the tropical Atlantic region is a net sink for acetone but a net source for methanol and acetaldehyde. Inclusion of the ocean fluxes resulted in good model simulations of monthly averaged methanol levels although still with a 3-fold underestimation in acetaldehyde. Wintertime acetone levels were better simulated, but the observed autumn levels were more severely underestimated than in the standard model. We suggest that the latter may be caused by underestimated terrestrial biogenic African primary and/or secondary OVOC sources by the model. The model underestimation of acetaldehyde concentrations all year round implies a consistent significant missing source, potentially from secondary chemistry of higher alkanes produced biogenically from plants or from the ocean. We estimate that low model bias in OVOC abundances in the remote tropical marine atmosphere may result in up to 8% underestimation of the global methane lifetime due to missing model OH reactivity. Underestimation of acetaldehyde concentrations is responsible for the bulk (∼70%) of this missing reactivity.

Structural analysis of oligomeric molecules formed from the reaction products of oleic acid ozonolysis

The products arising from the ozonolysis of oleic acid (cis-9-octadecenoic acid) in solution have been studied using negative ion mode electrospray ionization ion trap mass spectrometry. Oleic acid is an important component of atmospheric organic aerosol and is a key model species in predicting aerosol physical and chemical characteristics. The four predicted reaction products, 1-nonanal, nonanoic acid, 9-oxononanoic acid, and azelaic acid, were all observed in roughly equal yields. In addition to these products a large number of higher molecular weight compounds were detected with m/z ratios of up to 1000 Daltons. Tandem mass spectrometry of these larger ions revealed thatthey represented a complex mixture of linear alpha-acyloxyalkyl hydroperoxides, secondary ozonides, and cyclic diperoxides, formed by reactions between ozonolysis products and Criegee intermediates. These comprise the first directly elucidated structures of large oligomeric species from oleic acid ozonolysis. The degree of oligomerization and hence molecular weight distribution was observed to increase with reaction time in solution.

Measurement and modelling of air pollution and atmospheric chemistry in the U.K. West Midlands conurbation: overview of the PUMA Consortium project

The PUMA (Pollution of the Urban Midlands Atmosphere) Consortium project involved intensive measurement campaigns in the Summer of 1999 and Winter of 1999/2000, respectively, in which a wide variety of air pollutants were measured in the UK West Midlands conurbation including detailed speciation of VOCs and major component analysis of aerosol. Measurements of the OH and HO2 free radicals by the FAGE technique demonstrated that winter concentrations of OH were approximately half of those measured during the summer despite a factor of 15 reduction in production through the photolysis of ozone. Detailed box modelling of the fast reaction chemistry revealed the decomposition of Criegee intermediates formed from ozone-alkene reactions to be responsible for the majority of the formation of hydroxyl in both the summer and winter campaigns, in contrast to earlier rural measurements in which ozone photolysis was predominant. The main sinks for hydroxyl are reactions with NO2, alkenes and oxygenates. Concentrations of the more stable hydrocarbons were found to be relatively invariant across the conurbation, but the impacts of photochemistry were evident through analyses of formaldehyde which showed the majority to be photochemical in origin as opposed to emitted from road traffic. Measurements on the upwind and downwind boundaries of the conurbation revealed substantial enhancements in NOx as a result of emissions within the conurbation, especially during westerly winds which carried relatively clean air. Using calcium as a tracer for crustal particles, it proved possible to reconstruct aerosol mass from the major chemical components with a fairly high degree of success. The organic to elemental carbon ratios showed a far greater influence of photochemistry in summer than winter, presumably resulting mainly from the greater availability of biogenic precursors during the summer campaign. Two urban airshed models were developed and applied to the conurbation, one Eulerian, the other Lagrangian. Both were able to give a good simulation of concentrations of both primary and secondary pollutants at urban background locations.

Surgeon work input and risk in primary versus revision total joint arthroplasty

One hundred twenty stratified nonselected cases of primary and revision total joint arthroplasties performed between 1990 and 1992 in which complete financial and clinical data were available were reviewed. All cases were performed at a single university hospital. Compared with primary total joint arthroplasty, revision surgery involved significantly more operative time, greater blood loss, increased length of stay, and a much higher complication rate. The actual physician reimbursement was not significantly more than for primary procedures. Physician reimbursement constituted 18% of the total fees collected compared with 24% for the actual prosthesis cost. Surgeons performing revision surgery devote significantly more time and are at a higher liability than when performing primary total joint arthroplasty.

Phorbol myristate acetate produces injury to isolated rat lungs in the presence and absence of perfused neutrophils

Because lung injury induced by phorbol myristate acetate (PMA) has been reported by some to be mediated by blood neutrophils (PMN) and by others to occur independently of PMN, we examined the PMN dependency of PMA-induced injury in isolated, perfused lungs of rats. Depending on dose, PMA added to medium perfusing isolated rat lungs produced injury in the presence or in the absence of added PMN. When a high concentration of PMA (57 ng/ml) was added to medium devoid of added PMN, perfusion pressure and lung weight increased. Superoxide dismutase (500 U/ml) and catalase (400 U/ml) added to the medium prior to PMA had no effect on the increases in lung weight or perfusion pressure. When a concentration of PMA (21 ng/ml or less) that did not by itself cause lungs to accumulate fluid was added to perfusion medium containing PMN (1 X 10(8)), superoxide was produced, perfusion pressure increased, and lungs accumulated fluid. Addition of superoxide dismutase and catalase to this preparation prevented the increase in lung weight, but not the increase in perfusion pressure. We conclude that high concentrations of PMA produce lung injury which is independent of neutrophils and oxygen radicals and that lower concentrations produce injury which is neutrophil-dependent and mediated by oxygen radicals. These results may explain why PMA-induced lung injury has variously been reported to be PMN-dependent in some systems and PMN-independent in others.

Involvement of thromboxane in injury to isolated rat lungs perfused with phorbol myristate acetate in the presence and absence of neutrophils

In a previous study, we demonstrated that a non-toxic concentration of phorbol myristate acetate (PMA) produced edema in isolated rat lungs which were coperfused with neutrophils (PMN). In this study, we examined whether prostaglandins or thromboxane were responsible for increases in pressure and/or edema in this preparation. In lungs perfused with PMA (14 ng/ml) and PMN (1 X 10(8], significantly greater amounts of thromboxane B2 (TxB2) and 6-keto-prostaglandin F1 alpha (6-keto-PGF1 alpha) were produced than in controls. Relative lung weights and increases in perfusion pressure correlated with concentrations of TxB2 and 6-keto-PGF1 alpha that were produced. Indomethacin (10 microM) or Dazmegrel (10 microM) retarded the increase in perfusion pressure and prevented the increase in relative lung weight induced by PMA and PMN. When lungs were perfused with a high concentration of PMA (57 ng/ml) in the absence of added PMN, lungs also become edematous. Compared to controls, concentrations of TxB2 and 6-keto-PGF1 alpha were elevated in media collected from this preparation. As with lungs perfused with PMN and PMA, increases in pressure and relative weights of lungs perfused with PMA (57 ng/ml) correlated with the concentrations of TxB2 that were detected in perfusion media. Although indomethacin (10 microM) and Dazmegrel (50 microM) retarded the increase in perfusion pressure in this preparation, they only partially attenuated the increase in lung weight. These results suggest that, depending on the concentration, PMA can produce lung injury via different mechanisms. Thromboxane does not seem to be required for the genesis of edema induced by a high concentration of PMA in the absence of perfused neutrophils; however, it appears to play an obligatory role in the pathogenesis of edema induced by a low concentration of PMA in the presence of PMN.

Lack of effect of deferoxamine, dimethyl sulfoxide, and catalase on monocrotaline pyrrole pulmonary injury

Monocrotaline pyrrole (MCTP) is a reactive metabolite of the pyrrolizidine alkaloid monocrotaline. MCTP given intravenously to rats causes pulmonary hypertension and right ventricular hypertrophy. Lesions in lungs after MCTP treatment contain macrophages and neutrophils, which may contribute to the damage by generation of reactive oxygen metabolites. Rats were treated with MCTP and agents known to protect against oxygen radical-mediated damage in acute models of neutrophil-dependent lung injury. Rats received MCTP and deferoxamine mesylate (DF), dimethyl sulfoxide (DMSO), or polyethylene glycol-coupled catalase (PEG-CAT). MCTP/vehicle-treated controls developed lung injury manifested as increased lung weight, release of lactate dehydrogenase into the airway, and sequestration of 125I-labeled bovine serum albumin in the lungs. Cotreatment of rats with DF, DMSO, or PEG-CAT did not protect against the injury due to MCTP. These results suggest that toxic oxygen metabolites do not play an important role in the pathogenesis of MCTP-induced pulmonary injury.

Effect of a mixed function oxidase inducer and inhibitor on monocrotaline pyrrole pneumotoxicity

Monocrotaline (MCT) produces vascular injury to the lung, pulmonary hypertension, and right ventricular hypertrophy when injected into rats. It is well established that the pneumotoxicity of MCT depends on its hepatic bioactivation to monocrotaline pyrrole (MCTP) and perhaps other toxic metabolites. To test whether MCTP requires further bioactivation, we synthesized this metabolite chemically, confirmed its structure using fast-atom bombardment-mass spectrometry and nuclear magnetic resonance, and injected it into rats previously treated with an inducer or inhibitor of MFOs. Pretreatment with either phenobarbital or SKF-525A did not alter the pneumotoxic effects of an intravenous injection of MCTP. Rats given the same intravenous dose of either MCT, MCT N-oxide, or MCTP responded with toxicity only to MCTP. MCTP added to rat serum in vitro resulted in a color change (Amax = 477 nm) that developed over several seconds, an observation consistent with degradation of MCTP in serum. To explore the possibility that aqueous degradation products might contribute to its toxicity, the same intravenous dose of MCTP was administered to rats in N,N-dimethylformamide (DMF), serum, or saline. Only MCTP administered in in DMF resulted in toxicity. These results support the contention that MCT requires metabolism to MCTP to produce pneumotoxicity and that exposure to aqueous media renders MCTP incapable of causing lung injury.