Wildland Fire Emission Factors in North America: Synthesis of Existing Data, Measurement Needs and Management Applications
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Gas-Phase Boudouard Disproportionation Reaction Between Highly Vibrationally Excited CO Molecules
Chemical Physics 330 (2006) 506–514 www.elsevier.com/locate/chemphys Gas-phase Boudouard disproportionation reaction between highly vibrationally excited CO molecules Katherine A. Essenhigh, Yurii G. Utkin, Chad Bernard, Igor V. Adamovich *, J. William Rich Nonequilibrium Thermodynamics Laboratories, Department of Mechanical Engineering, The Ohio State University, Columbus, OH 43202, USA Received 3 September 2006; accepted 21 September 2006 Available online 30 September 2006 Abstract The gas-phase Boudouard disproportionation reaction between two highly vibrationally excited CO molecules in the ground elec- tronic state has been studied in optically pumped CO. The gas temperature and the CO vibrational level populations in the reaction region, as well as the CO2 concentration in the reaction products have been measured using FTIR emission and absorption spectroscopy. The results demonstrate that CO2 formation in the optically pumped reactor is controlled by the high CO vibrational level populations, rather than by CO partial pressure or by flow temperature. The disproportionation reaction rate constant has been determined from the measured CO2 and CO concentrations using the perfectly stirred reactor (PSR) approximation. The reaction activation energy, 11.6 ± 0.3 eV (close to the CO dissociation energy of 11.09 eV), was evaluated using the statistical transition state theory, by comparing the dependence of the measured CO2 concentration and of the calculated reaction rate constant on helium partial pressure. The dispro- À18 3 portionation reaction rate constant measured at the present conditions is kf =(9±4)· 10 cm /s. The reaction rate constants obtained from the experimental measurements and from the transition state theory are in good agreement. -
Alder Reactions of [60]Fullerene with 1,2,4,5-Tetrazines and Additions to [60]Fullerene-Tetrazine Monoadducts
University of New Hampshire University of New Hampshire Scholars' Repository Doctoral Dissertations Student Scholarship Spring 2002 Diels -Alder reactions of [60]fullerene with 1,2,4,5-tetrazines and additions to [60]fullerene-tetrazine monoadducts Mark Christopher Tetreau University of New Hampshire, Durham Follow this and additional works at: https://scholars.unh.edu/dissertation Recommended Citation Tetreau, Mark Christopher, "Diels -Alder reactions of [60]fullerene with 1,2,4,5-tetrazines and additions to [60]fullerene-tetrazine monoadducts" (2002). Doctoral Dissertations. 81. https://scholars.unh.edu/dissertation/81 This Dissertation is brought to you for free and open access by the Student Scholarship at University of New Hampshire Scholars' Repository. It has been accepted for inclusion in Doctoral Dissertations by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact [email protected]. INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand comer and continuing from left to right in equal sections with small overlaps. -
Emission Factors ⇑ Shawn Urbanski
Forest Ecology and Management 317 (2014) 51–60 Contents lists available at SciVerse ScienceDirect Forest Ecology and Management journal homepage: www.elsevier.com/locate/foreco Wildland fire emissions, carbon, and climate: Emission factors ⇑ Shawn Urbanski Missoula Fire Sciences Laboratory, Rocky Mountain Research Station, US Forest Service, 5775 US Highway 10 W, Missoula, MT 59808, USA article info abstract Article history: While the vast majority of carbon emitted by wildland fires is released as CO2, CO, and CH4, wildland fire Available online 21 June 2013 smoke is nonetheless a rich and complex mixture of gases and aerosols. Primary emissions include sig- nificant amounts of CH4 and aerosol (organic aerosol and black carbon), which are short-lived climate Keywords: forcers. In addition to CO2 and short-lived climate forcers, wildland fires release CO, non-methane organic Biomass burning compounds (NMOC), nitrogen oxides (NOx =NO+NO2), NH3, and SO2. These species play a role in radia- Greenhouse gases tive forcing through their photochemical processing, which impacts atmospheric levels of CO2,CH4, tro- Emission factors pospheric O3, and aerosol. This paper reviews the current state of knowledge regarding the chemical composition of emissions and emission factors for fires in United States vegetation types as pertinent to radiative forcing and climate. Emission factors are critical input for the models used to estimate wild- land fire greenhouse gas and aerosol emission inventories. Published by Elsevier B.V. 1. Introduction Fuels are defined as biomass (dead and live) that is available for combustion (Sandberg et al., 2001). While most emission models Emissions from wildland fires are a significant source of carbo- are based on Eq. -
Some Unusual, Astronomically Significant Organic Molecules
'lL-o Thesis titled: Some Unusual, Astronomically Significant Organic Molecules submitted for the Degree of Doctor of Philosophy (Ph,D.) by Salvatore Peppe B.Sc. (Hons.) of the Department of Ghemistty THE UNIVERSITY OF ADELAIDE AUSTRALIA CRUC E June2002 Preface Gontents Contents Abstract IV Statement of Originality V Acknowledgments vi List of Figures..... ix 1 I. Introduction 1 A. Space: An Imperfect Vacuum 1 B. Stellff Evolution, Mass Outflow and Synthesis of Molecules 5 C. Astronomical Detection of Molecules......... l D. Gas Phase Chemistry.. 9 E. Generation and Detection of Heterocumulenes in the Laboratory 13 L.2 Gas Phase Generation and Characterisation of Ions.....................................16 I. Gas Phase Generation of Ions. I6 A. Positive Ions .. I6 B. Even Electron Negative Ions 17 C. Radical Anions 2t tr. Mass Spectrometry 24 A. The VG ZAB 2}lF Mass Spectrometer 24 B. Mass-Analysed Ion Kinetic Energy Spectrometry......... 25 III. Characterisation of Ions.......... 26 A. CollisionalActivation 26 B. Charge Reversal.... 28 C. Neutralisation - Reionisation . 29 D. Neutral Reactivity. JJ rv. Fragmentation Behaviour ....... 35 A. NegativeIons.......... 35 Preface il B. Charge Inverted Ions 3l 1.3 Theoretical Methods for the Determination of Molecular Geometries and Energetics..... ....o........................................ .....39 L Molecular Orbital Theory........ 39 A. The Schrödinger Equation.... 39 B. Hartree-Fock Theory ..44 C. Electron Correlation ..46 D. Basis sets............ .51 IL Transition State Theory of Unimolecular Reactions ......... ................... 54 2. Covalently Bound Complexes of CO and COz ....... .........................58 L Introduction 58 tr. Results and Discussion........... 59 Part A: Covalently bound COz dimers (OzC-COr)? ............ 59 A. Generation of CzO¿ Anions 6I B. NeutralCzO+........ -
Download Download
The Preparation of Aromatic Esters of Malonic Acid 1 John H. Billman, R. Vincent Cash 2 and Eleanor K. Wakefield The preparations of four aromatic esters of malonic acid have been described in the literature. These are the diphenyl-, di-/3-naphthyl-, di- p-tolyl-, and di-p-nitrophenyl malonates. The preparation of diphenyl malonate by Bischoff and von Heden- strom (5) in 1902 illustrates one of the synthetic methods employed. Phenol and malonyl chloride were warmed on a water bath for a short time; hydrogen chloride was envolved and the solid ester crystallized on cooling. -* C1-C-CH.-C-C1 + 2 CeHtfOH C 6 H 5 -0-C-CH a -C-0-C 6 H 6 + 2 HC1 These workers tried without success to prepare this ester from malonic acid, phenol, and thionyl chloride. However, Auger and Billy (1) were able to synthesize diphenyl malonate from malonic acid, phenol, and phosphorus oxychloride. Guia (6) obtained di-/3-naphthnyl malonate rather than the desired counmarin-type compound when he heated /3-naphthol, malonyl chloride, and aluminum chloride in carbon disulfide. Backer and Lolkema (2) synthesized di-p-tolyl malonate and di-p-nitrophenyl malonate from malonyl chloride according to the above equation. The latter ester was also prepared by these investigators by treatment of the diphenyl malonate with nitric acid at 0°. Since carbon suboxide has been reported (7) to react with alcohols to yield dialkyl malonates, it seemed of interest to attempt to extend the reaction to phenols. -* 0=C=C=C=0 + 2 HOAr Ar-0-C-CH 2 -C-0-Ar Five phenols were successfully esterified with carbon suboxide, with sulfuric acid or p-toluenesulfonic acid present at catalyst. -
The Infrared Absorption Spectrum of Carbon Sub Oxide
AUGUST, 1937 JOURNAL OF CHEMICAL PHVSICS VOLUME 5 The Infrared Absorption Spectrum of Carbon Suboxide R. C. LORD, JR.* AND NORMAN WRIGHT Departments of Chemistry and Physics, University of Michigan, A nn Arbor, Michigan (Received "May 24, 1937) The infrared absorption spectrum of carbon suboxide vapor has been studied under low dispersion in the region from 2).1 to 25).1. The vibrational bands observed may be satisfactorily accounted for on the basis of a linear symmetric structure for the carbon suboxide molecule, in agreement with evidence obtained from Raman spectra and from electron diffraction investigations. ECENT studies of the structure of the material was prepared by the pyrolysis of R carbon suboxide molecule by electron dif diacetyl tartaric anhydride8 and was purified by fractiont ,2 and by ultraviolet absorption and two distillations in an all-glass system. Measure 3 Raman spectra - 5 have made desirable an in ments of the vapor pressure of the suboxide over vestigation of the molecule's absorption spectrum a range of temperatures up to O°C agreed in the infrared region. The information to be satisfactorily with those in the literature. 9 The gained from such an investigation should be absorption cell was filled by distilling the middle particularly helpful since the spectroscopic and fraction of the particular sampJe at hand into electron diffraction evidence indicates that the the evacuated ce1l, the desired pressure being most probable form of the carbon suboxide obtained by surrounding the distilling vessel molecule is one possessing a symmetry center. with a bath of acetone of the proper temperature. -
Carbon Dioxide Hydrogenation to Aromatic Hydrocarbons by Using an Iron/Iron Oxide Nanocatalyst
Carbon dioxide hydrogenation to aromatic hydrocarbons by using an iron/iron oxide nanocatalyst Hongwang Wang*1, Jim Hodgson1, Tej B. Shrestha2, Prem S. Thapa3, David Moore3, Xiaorong Wu4, Myles Ikenberry5, Deryl L. Troyer2, Donghai Wang4, Keith L. Hohn5 and Stefan H. Bossmann*1 Full Research Paper Open Access Address: Beilstein J. Nanotechnol. 2014, 5, 760–769. 1Kansas State University, Department of Chemistry, 201CBC doi:10.3762/bjnano.5.88 Building, Manhattan, KS 66506, USA, 001-785-532-6817, 2Kansas State University, Department of Anatomy & Physiology, 130 Coles Received: 11 March 2014 Hall, Manhattan, KS 66506, USA, 3University of Kansas, Microscopy Accepted: 30 April 2014 and Analytical Imaging Laboratory, 1043 Haworth, Lawrence, KS Published: 02 June 2014 66045, USA, 4Kansas State University, Department of Biological and Agricultural Engineering, 150 Seaton Hall, Manhattan, KS 66506, Associate Editor: J. J. Schneider USA and 5Kansas State University, Department of Chemical Engineering, 1016 Durland Hall, Manhattan, KS 66506, USA © 2014 Wang et al; licensee Beilstein-Institut. License and terms: see end of document. Email: Hongwang Wang* - [email protected]; Stefan H. Bossmann* - [email protected] * Corresponding author Keywords: aromatic hydrocarbons; carbon dioxide reduction; heterogenous catalysis; iron/iron oxide nanocatalyst Abstract The quest for renewable and cleaner energy sources to meet the rapid population and economic growth is more urgent than ever before. Being the most abundant carbon source in the atmosphere of Earth, CO2 can be used as an inexpensive C1 building block in the synthesis of aromatic fuels for internal combustion engines. We designed a process capable of synthesizing benzene, toluene, xylenes and mesitylene from CO2 and H2 at modest temperatures (T = 380 to 540 °C) employing Fe/Fe3O4 nanoparticles as cata- lyst. -
Wildland Fire Emission Sampling at Fishlake National Forest, Utah Using an Unmanned Aircraft System
Atmospheric Environment 247 (2021) 118193 Contents lists available at ScienceDirect Atmospheric Environment journal homepage: http://www.elsevier.com/locate/atmosenv Wildland fire emission sampling at Fishlake National Forest, Utah using an unmanned aircraft system J. Aurell a, B. Gullett b,*, A. Holder b, F. Kiros a, W. Mitchell b, A. Watts c, R. Ottmar d a University of Dayton Research Institute, 300 College Park, Dayton, OH, 45469, USA b U.S. Environmental Protection Agency, Office of Research and Development, 109 T.W. Alexander Drive Research Triangle Park, NC, 27711, USA c Desert Research Institute, 2215 Raggio Parkway, Reno, NV, 89512, USA d U.S. Forest Service, Pacific Wildland Forest Sciences Laboratory, 400 North 34th Street, Seattle, WA, 98103, USA HIGHLIGHTS GRAPHICAL ABSTRACT • An unmanned aircraft system was used to measure air pollutants from a wild land fire. • The prescribed fire included slash pile burns and crown fires. • Emission factors were determined for a comprehensive list of gases and particles. • Emissions typically decreased with increasing combustion efficiency. • The system enabled unprecedented ac cess to the fire while minimizing risk. ARTICLE INFO ABSTRACT Keywords: Emissions from a stand replacement prescribed burn were sampled using an unmanned aircraft system (UAS, or Prescribed fire “drone”) in Fishlake National Forest, Utah, U.S.A. Sixteen flightsover three days in June 2019 provided emission Wildfire factors for a broad range of compounds including carbon monoxide (CO), carbon dioxide (CO2), nitric oxide Emissions (NO), nitrogen dioxide (NO2), particulate matter < 2.5 μm in diameter (PM2.5), volatile organic compounds Measurements (VOCs) including carbonyls, black carbon, and elemental/organic carbon. -
Critical Assessment of Wildland Fire Emissions Inventories: Methodology, Uncertainty, Effectiveness Final Report Joint Fire Sciences Program Project # 12-1-07-1
Critical Assessment of Wildland Fire Emissions Inventories: Methodology, Uncertainty, Effectiveness Final Report Joint Fire Sciences Program Project # 12-1-07-1 Principal Investigator: Wei Min Hao US Forest Service, Rocky Mountain Research Station Missoula Fire Sciences Laboratory 5775 W US Highway 10 Missoula, MT 59808 Co-Principal Investigators Shawn Urbanski, US Forest Service, Rocky Mountain Research Station, Missoula Fire Sciences Laboratory, Missoula, MT Helen Naughton, University of Montana Department of Economics University of Montana Missoula, MT 59812-4572 Background and Purpose Fires emit a substantial amount of atmospheric pollutants (CO, CH4, non-methane organic compounds (NMOC), NOx, PM2.5), greenhouse gases (CO2, CH4, N2O), and black carbon that can have major impacts on regional air quality and global climate. In addition to being primary pollutants, the photochemical processing of NOX and NMOC leads to the formation of ozone and secondary PM2.5. The most important criteria for assessing the impacts of fires on the regional and global environment are accurate, reliable information on the spatial and temporal distribution of fire emissions (Riebau and Fox, 2010). Fire Emission Inventories (FEI) provide a spatially and temporally resolved accounting of air pollutants released to the atmosphere by wildland fires. On a national level FEI typically indicate fires as a major source of PM2.5 on an annual basis (Figure 1). However, since most fires occur during the wildfire season, the annual, CONUS wide figures greatly understate the potential impact of fire emissions on air quality. During active periods of the wildfire season, fire emissions are believed to dwarf anthropogenic sources of PM2.5 and NMOC (Figure 2), the latter of which includes hazardous air pollutants (HAP) and reactive gases that can lead to the formation of ozone and secondary PM2.5. -
Wildland Fire Emissions, Carbon, and Climate: Emission Factors
Forest Ecology and Management 317 (2014) 51–60 Contents lists available at SciVerse ScienceDirect Forest Ecology and Management journal homepage: www.elsevier.com/locate/foreco Wildland fire emissions, carbon, and climate: Emission factors ⇑ Shawn Urbanski Missoula Fire Sciences Laboratory, Rocky Mountain Research Station, US Forest Service, 5775 US Highway 10 W, Missoula, MT 59808, USA article info abstract Article history: While the vast majority of carbon emitted by wildland fires is released as CO2, CO, and CH4, wildland fire Available online 21 June 2013 smoke is nonetheless a rich and complex mixture of gases and aerosols. Primary emissions include sig- nificant amounts of CH4 and aerosol (organic aerosol and black carbon), which are short-lived climate Keywords: forcers. In addition to CO2 and short-lived climate forcers, wildland fires release CO, non-methane organic Biomass burning compounds (NMOC), nitrogen oxides (NOx =NO+NO2), NH3, and SO2. These species play a role in radia- Greenhouse gases tive forcing through their photochemical processing, which impacts atmospheric levels of CO2,CH4, tro- Emission factors pospheric O3, and aerosol. This paper reviews the current state of knowledge regarding the chemical composition of emissions and emission factors for fires in United States vegetation types as pertinent to radiative forcing and climate. Emission factors are critical input for the models used to estimate wild- land fire greenhouse gas and aerosol emission inventories. Published by Elsevier B.V. 1. Introduction Fuels are defined as biomass (dead and live) that is available for combustion (Sandberg et al., 2001). While most emission models Emissions from wildland fires are a significant source of carbo- are based on Eq. -
Abstracts and Presenter Biographical Information Oral Presentations
ABSTRACTS AND PRESENTER BIOGRAPHICAL INFORMATION ORAL PRESENTATIONS Abstracts for oral presentations and biographical information for presenters are listed alphabetically below by presenting author’s last name. Abstracts and biographical information appear unmodified, as submitted by the corresponding authors. Day, time, and room number of presentation are also provided. Abatzoglou, John John Abatzoglou, Assistant Professor of Geography, University of Idaho. Research interests span the weather-climate continuum and both basic and applied scientific questions on past, present and future climate dynamics as well as their influence on wildfire, ecology and agriculture and is a key player in the development of integrated climate scenarios for the Pacific Northwest, US. Oral presentation, Wednesday, 2:30 PM, B114 Will climate change increase the occurrence of megafires in the western United States? The largest wildfires in the western United States account for a substantial portion of annual area burned and are associated with numerous direct and indirect geophysical impacts in addition to commandeering suppression resources and national attention. While substantial prior work has been devoted to understand the influence of climate, and weather on annual area burned, there has been limited effort to identify factors that enable and drive the very largest wildfires, or megafires. We hypothesize that antecedent climate and shorter-term biophysically relevant meteorological variables play an essen- tial role in favoring or deterring historical megafire occurrence identified using the Monitoring Trends in Burn Severity Atlas from 1984-2010. Antecedent climatic factors such as drought and winter and spring temperature were found to vary markedly across geographic areas, whereas regional commonality of prolonged extremely low fuel moisture and high fire danger prior to and immediately following megafire discovery. -
Effects of Pressure and Particle Size on the Carbonization of a Packed Bed of Biomass
Effects of Pressure and Particle Size on the Carbonization of a Packed Bed of Biomass A THESIS SUBMITTED TO THE GRADUATE DIVISION OF THE UNIVERSITY OF HAWAIʻI AT MĀNOA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE IN MECHANICAL ENGINEERING May 2014 By Gregory Patrick Specht Thesis Committee: Michael J. Antal Jr., Chairperson Weilin Qu Beei-Huan Chao i We certify that we have read this thesis and that, in our opinion it is satisfactory in scope and quality as a dissertation for a degree of Master of Science in Mechanical Engeineering. THESIS COMMITTEE Chairperson ii © Copyright 2014 By Gregory Patrick Specht All Rights Reserved iii Abstract A relatively new technique for charcoal production has been developed called Flash CarbonizationTM and has proven to be efficient and most importantly fast. The technique begins with a packed bed of biomass pressurized at 1-2 MPa. A fire is ignited at the bottom of the bed while air is introduced through the top. The flame travels up the bed converting the biomass to bio carbon otherwise known as charcoal. One of the most important metrics a charcoal has is its Fixed Carbon Yield (yfc) or the percentage of carbon left in it after it is carbonized. Many factors affect the yfc of charcoal three in particular were investigated in this thesis; feedstock, pressure, and particle size. Each feedstock that was used in the FC process and analyzed in this thesis was sent out to a lab to discover its elemental composition. Using this data calculations were performed to discover the highest theoretical yfc each feedstock could produce.