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  • 1
    Publication Date: 2019
    Description: Abstract As part of the WINTER (Wintertime Investigation of Transport, Emissions, and Reactivity) campaign, a Particle‐into‐Liquid Sampler with a fraction collector was flown aboard the National Center for Atmospheric Research C‐130 aircraft. Two‐minute integrated liquid samples containing dissolved fine particulate matter (PM1) species were collected and analyzed off‐line for the smoke marker levoglucosan using high‐performance anion‐exchange chromatography‐pulsed amperometric detection to compare levoglucosan with aerosol mass spectrometer (AMS) biomass burning markers and investigate the contribution from residential burning during the study. Levoglucosan was correlated with AMS organic aerosol (R2 = 0.49) and with carbon monoxide (CO; R2 = 0.51) for all flights. Levoglucosan was not correlated with the inorganic smoke marker water‐soluble potassium but was correlated with the AMS markers ∆C2H4O2+ (high resolution, R2 = 0.60) and ∆m/z 60 (unit mass resolution, R2 = 0.61). However, at low levoglucosan, AMS markers deviated potentially due to interferences from other sources or differences with the species captured by the AMS markers. Analysis of levoglucosan changes relative to carbon monoxide as plumes advected from source regions showed no systematic levoglucosan loss for plumes up to 20 hr old. Based on literature residential burning source ratios and measured levoglucosan, contributions of organic carbon (OC) due to residential burning were estimated. The contribution ranged from ~30 to 100% of the OC, with significant variability depending on the source ratio used; however, the results show that biomass burning was a significant PM1 OC source across the entire sampling region. A GEOS‐Chem model simulation predicted significantly less smoke contribution.
    Print ISSN: 2169-897X
    Electronic ISSN: 2169-8996
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 2
    Publication Date: 2010-03-12
    Description: Halogen atoms and oxides are highly reactive and can profoundly affect atmospheric composition. Chlorine atoms can decrease the lifetimes of gaseous elemental mercury and hydrocarbons such as the greenhouse gas methane. Chlorine atoms also influence cycles that catalytically destroy or produce tropospheric ozone, a greenhouse gas potentially toxic to plant and animal life. Conversion of inorganic chloride into gaseous chlorine atom precursors within the troposphere is generally considered a coastal or marine air phenomenon. Here we report mid-continental observations of the chlorine atom precursor nitryl chloride at a distance of 1,400 km from the nearest coastline. We observe persistent and significant nitryl chloride production relative to the consumption of its nitrogen oxide precursors. Comparison of these findings to model predictions based on aerosol and precipitation composition data from long-term monitoring networks suggests nitryl chloride production in the contiguous USA alone is at a level similar to previous global estimates for coastal and marine regions. We also suggest that a significant fraction of tropospheric chlorine atoms may arise directly from anthropogenic pollutants.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Thornton, Joel A -- Kercher, James P -- Riedel, Theran P -- Wagner, Nicholas L -- Cozic, Julie -- Holloway, John S -- Dube, William P -- Wolfe, Glenn M -- Quinn, Patricia K -- Middlebrook, Ann M -- Alexander, Becky -- Brown, Steven S -- England -- Nature. 2010 Mar 11;464(7286):271-4. doi: 10.1038/nature08905.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Atmospheric Sciences, University of Washington, Seattle, Washington 98195, USA. thornton@atmos.washington.edu〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/20220847" target="_blank"〉PubMed〈/a〉
    Keywords: Aerosols/chemistry ; Air/analysis ; Atmosphere/*chemistry ; Chlorine/*chemistry ; Colorado ; Models, Chemical ; Nitrites/analysis/*chemistry ; Nitrogen/*chemistry ; Nitrogen Oxides/chemistry ; Time Factors
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 3
  • 4
    Publication Date: 2014-02-28
    Description: Forests emit large quantities of volatile organic compounds (VOCs) to the atmosphere. Their condensable oxidation products can form secondary organic aerosol, a significant and ubiquitous component of atmospheric aerosol, which is known to affect the Earth's radiation balance by scattering solar radiation and by acting as cloud condensation nuclei. The quantitative assessment of such climate effects remains hampered by a number of factors, including an incomplete understanding of how biogenic VOCs contribute to the formation of atmospheric secondary organic aerosol. The growth of newly formed particles from sizes of less than three nanometres up to the sizes of cloud condensation nuclei (about one hundred nanometres) in many continental ecosystems requires abundant, essentially non-volatile organic vapours, but the sources and compositions of such vapours remain unknown. Here we investigate the oxidation of VOCs, in particular the terpene alpha-pinene, under atmospherically relevant conditions in chamber experiments. We find that a direct pathway leads from several biogenic VOCs, such as monoterpenes, to the formation of large amounts of extremely low-volatility vapours. These vapours form at significant mass yield in the gas phase and condense irreversibly onto aerosol surfaces to produce secondary organic aerosol, helping to explain the discrepancy between the observed atmospheric burden of secondary organic aerosol and that reported by many model studies. We further demonstrate how these low-volatility vapours can enhance, or even dominate, the formation and growth of aerosol particles over forested regions, providing a missing link between biogenic VOCs and their conversion to aerosol particles. Our findings could help to improve assessments of biosphere-aerosol-climate feedback mechanisms, and the air quality and climate effects of biogenic emissions generally.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Ehn, Mikael -- Thornton, Joel A -- Kleist, Einhard -- Sipila, Mikko -- Junninen, Heikki -- Pullinen, Iida -- Springer, Monika -- Rubach, Florian -- Tillmann, Ralf -- Lee, Ben -- Lopez-Hilfiker, Felipe -- Andres, Stefanie -- Acir, Ismail-Hakki -- Rissanen, Matti -- Jokinen, Tuija -- Schobesberger, Siegfried -- Kangasluoma, Juha -- Kontkanen, Jenni -- Nieminen, Tuomo -- Kurten, Theo -- Nielsen, Lasse B -- Jorgensen, Solvejg -- Kjaergaard, Henrik G -- Canagaratna, Manjula -- Maso, Miikka Dal -- Berndt, Torsten -- Petaja, Tuukka -- Wahner, Andreas -- Kerminen, Veli-Matti -- Kulmala, Markku -- Worsnop, Douglas R -- Wildt, Jurgen -- Mentel, Thomas F -- England -- Nature. 2014 Feb 27;506(7489):476-9. doi: 10.1038/nature13032.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉1] Institute for Energy and Climate Research (IEK-8), Forschungszentrum Julich, 52425 Julich, Germany [2] Department of Physics, PO Box 64, 00014 University of Helsinki, Finland. ; 1] Department of Physics, PO Box 64, 00014 University of Helsinki, Finland [2] Department of Atmospheric Sciences, University of Washington, Seattle, Washington 98195, USA. ; Institute of Bio- and Geosciences (IBG-2), Forschungszentrum Julich, 52425 Julich, Germany. ; Department of Physics, PO Box 64, 00014 University of Helsinki, Finland. ; Institute for Energy and Climate Research (IEK-8), Forschungszentrum Julich, 52425 Julich, Germany. ; Department of Atmospheric Sciences, University of Washington, Seattle, Washington 98195, USA. ; 1] Department of Physics, PO Box 64, 00014 University of Helsinki, Finland [2] Institute for Tropospheric Research (TROPOS), 04318 Leipzig, Germany. ; 1] Department of Physics, PO Box 64, 00014 University of Helsinki, Finland [2] Helsinki Institute of Physics, PO Box 64, 00014 University of Helsinki, Finland. ; Department of Chemistry, PO Box 55, 00014 University of Helsinki, Finland. ; Department of Chemistry, University of Copenhagen, Universitetsparken 5, 2100 Copenhagen O, Denmark. ; Aerodyne Research, Inc., 45 Manning Road, Billerica, Massachusetts 01821, USA. ; Department of Physics, Tampere University of Technology, PO Box 692, 33101 Tampere, Finland. ; Institute for Tropospheric Research (TROPOS), 04318 Leipzig, Germany. ; 1] Department of Physics, PO Box 64, 00014 University of Helsinki, Finland [2] Aerodyne Research, Inc., 45 Manning Road, Billerica, Massachusetts 01821, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/24572423" target="_blank"〉PubMed〈/a〉
    Keywords: Aerosols/analysis/*chemistry/metabolism ; Atmosphere/chemistry ; Climate ; Ecosystem ; Finland ; Gases/analysis/chemistry ; *Models, Chemical ; Monoterpenes/chemistry ; Oxidation-Reduction ; Ozone/chemistry ; Particle Size ; Trees/metabolism ; Volatile Organic Compounds/analysis/*chemistry/metabolism ; Volatilization
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 5
    Publication Date: 2013-07-21
    Description: [1]  Heterogeneous N 2 O 5 uptake onto aerosol is the primary nocturnal path for removal of NO x (= NO + NO 2 ) from the atmosphere and can also result in halogen activation through production of ClNO 2 . The N 2 O 5 uptake coefficient has been the subject of numerous laboratory studies; however, only a few studies have determined the uptake coefficient from ambient measurements, and none have been focused on winter conditions, when the portion of NO x removed by N 2 O 5 uptake is the largest. In this work, N 2 O 5 uptake coefficients are determined from ambient wintertime measurements of N 2 O 5 and related species at the Boulder Atmospheric Observatory in Weld County, CO, a location that is highly impacted by urban pollution from Denver, as well as emissions from agricultural activities and oil and gas extraction. A box model is used to analyze the nocturnal nitrate radical chemistry and predict the N 2 O 5 concentration. The uptake coefficient in the model is iterated until the predicted N 2 O 5 concentration matches the measured concentration. The results suggest that during winter, the most important influence that might suppress N 2 O 5 uptake is aerosol nitrate, but that this effect does not suppress uptake coefficients enough to limit the rate of NO x loss through N 2 O 5 hydrolysis. N 2 O 5 hydrolysis was found to dominate the nocturnal chemistry during this study consuming ~80% of nocturnal gas-phase nitrate radical production. Typically, less than 15% of the total nitrate radical production remained in the form of nocturnal species at sunrise when they are photolyzed and reform NO 2 .
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 6
    Publication Date: 2012-11-27
    Description: The sea breeze/land breeze diurnal circulation within the Los Angeles Basin and adjacent waters transports marine air into the basin during the day and urban air to Santa Monica Bay during the night. Nitryl chloride, ClNO2 is a nocturnal trace gas formed from the heterogeneous reaction of dinitrogen pentaoxide (N2O5) with chloride containing aerosol. Its photolysis after sunrise produces atomic chlorine radicals and regenerates NO2, both of which may increase ozone production. Mixing of the chloride source from marine sea salt with the urban NOx source in Los Angeles provides conditions ideal for the production of ClNO2. This paper presents an analysis using a wind profiler on the coast and measurements of ClNO2 and its precursors made from both ship and aircraft to assess the prevailing meteorological conditions important for ClNO2 production in this region, with a particular focus on the production over water within the land breeze phase of the circulation. A box model is used to calculate an upper limit to the amount of ClNO2 capable of being produced strictly over Santa Monica Bay during the land breeze. On three out of the four nights of ClNO2 measurements in Santa Monica Bay, the ClNO2 exceeds the upper limit calculated using the box model and shows that the majority of the ClNO2 is produced over the city and transported to Santa Monica Bay by the land breeze. This ClNO2 transport suggests the sea breeze more efficiently transports aerosol chloride inland than land breeze transports NOx offshore.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 7
    Electronic Resource
    Electronic Resource
    Palo Alto, Calif. : Annual Reviews
    Annual Review of Materials Research 7 (1977), S. 239-260 
    ISSN: 0084-6600
    Source: Annual Reviews Electronic Back Volume Collection 1932-2001ff
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    [S.l.] : American Institute of Physics (AIP)
    Journal of Applied Physics 67 (1990), S. 2637-2642 
    ISSN: 1089-7550
    Source: AIP Digital Archive
    Topics: Physics
    Notes: This paper reports the results of a comparative study of chalcopyrite-structure CuInSe2 deposited by three techniques, three-source evaporation, reactive sputtering and a hybrid sputtering, and evaporation method. All films exhibit comparable microstructures and microchemistries. Evaporated and hybrid-process films include significant porosity. All layers show dislocations, twins, and stacking faults. No second phases were observed in layers deposited by any of the techniques, independent of film composition. Data supporting this conclusion include average and single-grain energy-dispersive x-ray fluorescence spectroscopy measurements, diffraction studies of the film structure, and transmission electron microscopy images of the films. Finally, grain sizes can be increased by annealing films at temperatures above 400 °C.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 200 (1963), S. 1185-1187 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] AN examination of human serum cholinesterase by starch-gel electrophoresis, using sera from many different individuals, revealed that several components with the characteristics of that enzyme were regularly present, though one of these components, referred to as C4, was very much more prominent ...
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Czechoslovak journal of physics 23 (1973), S. 431-435 
    ISSN: 1572-9486
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract Experiments are described in which structured discharges, including stationary and moving striations, were observed in 4 MHz rf plasmas generated using two solenoidal coil configurations. The structured plasmas which formed in the vicinity of the solenoidal coils were not quenched when elaborate precautions were taken to shield the capacitive electric fields. Measurements of the rf power input to the plasma and the resistance reflected by the plasma into the drive circuit showed no discontinuous change during the formation or disappearance of the structured discharges surrounding the solenoidal coils. Observations of striated rf discharges reported by other investigators are reviewed. Arguments are given to support the conclusion that the striation-like structures observed in rf plasmas and the moving striations observed in dc plasmas are part of the same general family.
    Type of Medium: Electronic Resource
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