[1] The morphology of particles emitted by wildland fires contributes to their physical and chemical properties but is rarely determined. As part of a study at the USFS Fire Sciences Laboratory (FSL) investigating properties of particulate matter emitted by fires, we studied the size, morphology, and microstructure of particles emitted from the combustion of eight different wildland fuels (i.e., sagebrush, poplar wood, ponderosa pine wood, ponderosa pine needles, white pine needles, tundra cores, and two grasses) by scanning electron microscopy. Six of these fuels were dry, while two fuels, namely the tundra cores and one of the grasses, had high fuel moisture content. The particle images were analyzed for their density and textural fractal dimensions, their monomer and agglomerate number size distributions, and three different shape descriptors, namely aspect ratio, root form factor, and roundness. The particles were also probed with energy dispersive X-ray spectroscopy confirming their carbonaceous nature. The density fractal dimension of the agglomerates was determined using two different techniques, one taking into account the three-dimensional nature of the particles, yielding values between 1.67 and 1.83, the other taking into account only the two-dimensional orientation, yielding values between 1.68 and 1.74. The textural fractal dimension that describes the roughness of the boundary of the two-dimensional projection of the particle was between 1.10 and 1.19. The maximum length of agglomerates was proportional to a power a of their diameter and the proportionality constant and the three shape descriptors were parameterized as function of the exponent a.
Combustion of wildland fuels represents a major source of particulate matter (PM) and light-absorbing elemental carbon (EC) on a national and global scale, but the emission factors and source profiles have not been well characterized with respect to different fuels and combustion phases. These uncertainties limit the accuracy of current emission inventories, smoke forecasts, and source apportionments. This study investigates the evolution of gaseous and particulate emission and combustion efficiency by burning wildland fuels in a laboratory combustion facility. Emission factors for carbon dioxide (CO2), carbon monoxide (CO), total hydrocarbon (THC), nitrogen oxides (NO(x)), PM, light extinction and absorption cross sections, and spectral scattering cross sections specific to flaming and smoldering phases are reported. Emission factors are generally reproducible within +/- 20% during the flaming phase, which, despite its short duration, dominates the carbon emission (mostly in the form of CO2) and the production of light absorption and EC. Higher and more variable emission factors for CO, THC, and PM are found during the smoldering phase, especially for fuels containing substantial moisture. Organic carbon (OC) and EC mass account for a majority (i.e., > 60%) of PM mass; other important elements include potassium, chlorine, and sulfur. Thermal analysis separates the EC into subfractions based on analysis temperature demonstrating that high-temperature EC (EC2; at 700 degrees C) varies from 1% to 70% of PM among biomass burns, compared to 75% in kerosene soot. Despite this, the conversion factor between EC and light absorption emissions is rather consistent across fuels and burns, ranging from 7.8 to 9.6 m2/g EC. Findings from this study should be considered in the development of PM and EC emission inventories for visibility and radiative forcing assessments.
[1] Time-resolved optical properties of smoke particles from the controlled laboratory combustion of mid-latitude wildland fuels were determined for the first time using advanced techniques, including cavity ring-down/cavity enhanced detection (CRD/CED) for light extinction and two-wavelength photoacoustic detection for light absorption. This experiment clearly resolves the dependence of smoke properties on fuel and combustion phase. Intensive flaming combustion during ponderosa pine wood (PPW) burning produces particles with a low single scattering albedo of 0.32 and a specific mass extinction efficiency of 8.9 m 2 g
À1. Burning white pine needles (WPN) features a prolonged smoldering phase emitting particles that are not light-absorbing and appear much larger in size with an extinction efficiency %5 m 2 g À1 . A Mie scattering model was formulated, which estimates the black carbon fraction in the PPW and WPN smoke particles at 66% and 12%, respectively. These observations may refine the current radiative forcing estimates for biomass burning emissions. Citation:
Abstract. In this study we identify pyrolysis gases from prescribed burns conducted in
pine forests with a shrub understory captured using a manual extraction
device. The device selectively sampled emissions ahead of the flame front,
minimizing the collection of oxidized gases, with the captured gases analyzed in
the laboratory using infrared (IR) absorption spectroscopy. Results show
that emission ratios (ERs) relative to CO for ethene and acetylene were
significantly greater than in previous fire studies, suggesting that the sample
device was able to collect gases predominantly generated prior to ignition.
Further evidence that ignition had not begun was corroborated by novel IR
detections of several species, in particular naphthalene. With regards to
oxygenated species, several aldehydes (acrolein, furaldehyde, acetaldehyde,
formaldehyde) and carboxylic acids (formic, acetic) were all observed;
results show that ERs for acetaldehyde were noticeably greater, while ERs for
formaldehyde and acetic acid were lower compared to other studies. The
acetylene-to-furan ratio also suggests that high-temperature pyrolysis was
the dominant process generating the collected gases.
Abstract. Volatile organic compounds (VOCs) are emitted from many sources, including
wildland fire. VOCs have received heightened emphasis due to such gases'
influential role in the atmosphere, as well as possible health effects. We
have used extractive infrared (IR) spectroscopy on recent prescribed burns
in longleaf pine stands and herein report the first detection of five
compounds using this technique. The newly reported IR detections include
naphthalene, methyl nitrite, allene, acrolein and acetaldehyde. We discuss
the approaches used for detection, particularly the software methods needed
to fit the analyte and multiple (interfering) spectral components within the
selected spectral micro-window(s). We also discuss the method's detection
limits and related parameters such as spectral resolution.
As an alternative to open pile burning, use of forest wastes from fuel hazard reduction projects at Blodgett Forest Research Station for electricity production was shown to produce energy and emission benefits: energy (diesel fuel) expended for processing and transport was 2.5% of the biomass fuel (energy equivalent); based on measurements from a large pile burn, air emissions reductions were 98%-99% for PM 2.5 , CO (carbon monoxide), NMOC (nonmethane organic compounds), CH 4 (methane) and BC (black carbon), and 20% for NOx and CO 2 -equivalent greenhouse gases. Due to transport challenges and delays, delivered cost was $70 per bone dry ton (BDT) -comprised of collection and processing ($34/BDT) and transport ($36/BDT) for 79 miles one waywhich exceeded the biomass plant gate price of $45/BDT. Under typical conditions, the break-even haul distance would be approximately 30 miles one way, with a collection and processing cost of $30/BDT and a transport cost of $16/BDT. Revenue generated from monetization of the reductions in air emissions has the potential to make forest fuel reduction projects more economically viable.
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