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Dive into the research topics where Arthur J. Sedlacek is active.

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Featured researches published by Arthur J. Sedlacek.


Aerosol Science and Technology | 2010

Soot Particle Studies—Instrument Inter-Comparison—Project Overview

Eben S. Cross; Timothy B. Onasch; Adam Ahern; William Wrobel; Jay G. Slowik; Jason S. Olfert; D. A. Lack; Paola Massoli; Christopher D. Cappa; Joshua P. Schwarz; J. Ryan Spackman; D. W. Fahey; Arthur J. Sedlacek; A. Trimborn; John T. Jayne; Andrew Freedman; Leah R. Williams; Nga L. Ng; Claudio Mazzoleni; Manvendra K. Dubey; Benjamin T. Brem; Greg Kok; R. Subramanian; Steffen Freitag; Antony D. Clarke; D. A. Thornhill; Linsey C. Marr; Charles E. Kolb; Douglas R. Worsnop; P. Davidovits

An inter-comparison study of instruments designed to measure the microphysical and optical properties of soot particles was completed. The following mass-based instruments were tested: Couette Centrifugal Particle Mass Analyzer (CPMA), Time-of-Flight Aerosol Mass Spectrometer—Scanning Mobility Particle Sizer (AMS-SMPS), Single Particle Soot Photometer (SP2), Soot Particle-Aerosol Mass Spectrometer (SP-AMS) and Photoelectric Aerosol Sensor (PAS2000CE). Optical instruments measured absorption (photoacoustic, interferometric, and filter-based), scattering (in situ), and extinction (light attenuation within an optical cavity). The study covered an experimental matrix consisting of 318 runs that systematically tested the performance of instruments across a range of parameters including: fuel equivalence ratio (1.8 ≤ φ ≤ 5), particle shape (mass-mobility exponent ( D fm ), 2.0 ≤ D fm ≤ 3.0), particle mobility size (30 ≤ d m ≤ 300 nm), black carbon mass (0.07 ≤ m BC ≤ 4.2 fg) and particle chemical composition. In selected runs, particles were coated with sulfuric acid or dioctyl sebacate (DOS) (0.5 ≤ Δ r ve ≤ 201 nm) where Δ r ve is the change in the volume equivalent radius due to the coating material. The effect of non-absorbing coatings on instrument response was determined. Changes in the morphology of fractal soot particles were monitored during coating and denuding processes and the effect of particle shape on instrument response was determined. The combination of optical and mass based measurements was used to determine the mass specific absorption coefficient for denuded soot particles. The single scattering albedo of the particles was also measured. An overview of the experiments and sample results are presented.


Applied Spectroscopy | 2000

Stand-off Detection of Chemicals by UV Raman Spectroscopy

Ming Wu; Mark D. Ray; K. Hang Fung; M. W. Ruckman; David Harder; Arthur J. Sedlacek

Experimental results are reported on a mobile, stand-alone, solar-blind ultraviolet (UV) Raman lidar system for the stand-off detection and identification of liquid and solid targets at ranges of hundreds of meters. The lidar is a coaxial system capable of performing range-resolved measurements of gases and aerosols, as well as solids and liquids. The transmitter is a flash lamp pumped 30 Hz Nd:YAG laser with quadrupled output at 266 nm. The receiver subsystem is comprised of a 40 cm Cassegrain telescope, a holographic UV edge filter for suppressing the elastic channel, a 0.46 m Czerny–Turner spectrometer, and a time gated intensified charge-coupled device (CCD) detector. The rejection of elastic light scattering by the edge filter is better than one part in 105, while the transmittance 500 cm−1 to the red of the laser line is greater than 50%. Raman data are shown for selected solids, neat liquids, and mixtures down to the level of 1% volume ratio. On the basis of the strength of the Raman returns, a stand-off detection limit of ∼ 500 g/m2 for liquid spills of common solvents at the range of one half of a kilometer is possible.


Geophysical Research Letters | 2012

Determination of and evidence for non‐core‐shell structure of particles containing black carbon using the Single‐Particle Soot Photometer (SP2)

Arthur J. Sedlacek; Ernie R. Lewis; Lawrence I. Kleinman; Jianzhong Xu; Qi Zhang

[1] The large uncertainty associated with black carbon (BC) direct forcing is due, in part, to the dependence of light absorption of BC-containing particles on the position of the BC within the particle. It is predicted that this absorption will be greatest for an idealized core-shell configuration in which the BC is a sphere at the center of the particle whereas much less absorption should be observed for particles in which the BC is located near or on the surface. Such microphysical information on BC-containing particles has previously been provided only by labor-intensive microscopy techniques, thus often requiring that climate modelers make assumptions about the location of the BC within the particle that are based more on mathematical simplicity than physical reality. The present paper describes a novel analysis method that utilizes the temporal behavior of the scattering and incandescence signals from individual particles containing


Review of Scientific Instruments | 2000

Ultraviolet mini-Raman lidar for stand-off, in situ identification of chemical surface contaminants

Mark D. Ray; Arthur J. Sedlacek; Ming Wu

The Mini-Raman Lidar System (MRLS) is a portable chemical sensor that combines the spectral fingerprinting of Raman spectroscopy with the principles of solar-blind ultraviolet lidar for short-range, noncontact detection and identification of unknown substances on surfaces. The MRLS has the potential to detect contaminant films several microns thick at distances of meters and bulk quantities of substances at distances of tens of meters. The signal acquisition time is less than 1 min. The device has application to those involved in emergency response, environmental remediation, and military reconnaissance who respond initially at the site of a chemical spill or attack.


Aerosol Science and Technology | 2007

Photothermal Interferometric Aerosol Absorption Spectrometry

Arthur J. Sedlacek; Jeonghoon Lee

Aerosol light absorption still remains a difficult quantity to measure at the precision, accuracy and temporal resolution necessary to quantitatively bound the contribution of this direct effect on aerosol radiative forcing. These continuing difficulties are due, in part, because aerosol extinction is dominated by light scattering. In response to these and other issues, the aerosol community has been developing a new generation of instrumentation that can measure aerosol absorption without the need to deposit aerosols on a filter. Here we introduce work on the application of photothermal interferometry (PTI) towards this measurement problem. The advantages of this approach are: its complete insensitivity to aerosol scattering (true for any photothermal technique) and high sensitivity resulting from use of an interferometric technique. Using NO2 as a calibration standard, the accuracy of the PTI technique was measured to be 5% (95% confidence interval). Measurement at a 10-second time constant yields a precision of 0.2 Mm−1 (95% confidence interval) and a lower limit of detection of 0.4 Mm−1 for a sample pathlength of 5 cm. Using laboratory-generated nigrosin aerosols an intercomparison between the PTI and a 3-λ Particle Soot Absorption Photometer (PSAP) gives a slope of 0.96 ± 0.02. Acquisition of absorption coefficients for ambient aerosols reveals very good agreement between the two instruments except for periods of high relative humidity (>70%) whereupon the PSAP reports a larger absorption coefficient.


Journal of Chemical Physics | 1991

Interrogating the vibrational relaxation of highly excited polyatomics with time-resolved diode laser spectroscopy: C6H6, C6D6, and C6F6+CO2

Arthur J. Sedlacek; Ralph E. Weston; George W. Flynn

The vibrational relaxation of highly excited ground state benzene, benzene d6, and hexafluorobenzene by CO2 has been investigated with high resolution diode laser spectroscopy. The vibrationally hot polyatomics are formed by single photon 248 nm excitation to the S1 state followed by rapid radiationless transitions. It has been found that in all cases less than 1% of the energy initially present in the polyatomics is deposited into the high frequency mode of CO2 (ν3). An investigation of the CO2(0001) nascent rotational distribution under single collision conditions reveals that very little rotational excitation accompanies vibrational energy transfer to the ν3 mode. The CO2(ν3) rotational states can be described by temperatures, Trot, as follows: C6H6, Trot =360±30 K; C6D6, Trot =350±35 K and C6F6, Trot =340±23 K. An estimate of 〈ΔE〉ν3, the mean energy transferred to the CO2 ν3 mode per collision, suggests that as the availability of low frequency modes in the excited molecule increases, less energy is d...


Review of Scientific Instruments | 2006

Real-time detection of ambient aerosols using photothermal interferometry: Folded Jamin interferometer

Arthur J. Sedlacek

Work in our laboratory has been directed at the development of a new class of instrumentation that can directly measure ambient aerosol absorption through photothermal interferometry. The hallmark of this approach is its ability to directly measure aerosol absorption without interference from aerosol scattering since the signal originates from the thermal dissipation of the spectrally absorbed energy. While the principle of the photothermal technique for the detection of aerosols was demonstrated in the mid-1980s, this interferometric technique remains a laboratory technique largely due to sensitivity to mechanical vibrations and other environmental factors that result in unwanted signal interference and commensurate reduction in detection sensitivity. In order to realize its application outside the laboratory, a folded Jamin interferometer design has replaced both the traditional Mach-Zehnder and unfolded Jamin configurations. The folded Jamin affords many advantages, which include high degree of common ...


Environmental Science & Technology | 2016

Regional Influence of Aerosol Emissions from Wildfires Driven by Combustion Efficiency: Insights from the BBOP Campaign

Sonya Collier; Shan Zhou; Timothy B. Onasch; Daniel A. Jaffe; Lawrence I. Kleinman; Arthur J. Sedlacek; Nicole L. Briggs; Jonathan Hee; Edward Charles Fortner; John E. Shilling; Douglas R. Worsnop; Robert J. Yokelson; Caroline Parworth; Xinlei Ge; Jianzhong Xu; Zachary Butterfield; D. Chand; Manvendra K. Dubey; Mikhail S. Pekour; Stephen R. Springston; Qi Zhang

Wildfires are important contributors to atmospheric aerosols and a large source of emissions that impact regional air quality and global climate. In this study, the regional and nearfield influences of wildfire emissions on ambient aerosol concentration and chemical properties in the Pacific Northwest region of the United States were studied using real-time measurements from a fixed ground site located in Central Oregon at the Mt. Bachelor Observatory (∼2700 m a.s.l.) as well as near their sources using an aircraft. The regional characteristics of biomass burning aerosols were found to depend strongly on the modified combustion efficiency (MCE), an index of the combustion processes of a fire. Organic aerosol emissions had negative correlations with MCE, whereas the oxidation state of organic aerosol increased with MCE and plume aging. The relationships between the aerosol properties and MCE were consistent between fresh emissions (∼1 h old) and emissions sampled after atmospheric transport (6-45 h), suggesting that biomass burning organic aerosol concentration and chemical properties were strongly influenced by combustion processes at the source and conserved to a significant extent during regional transport. These results suggest that MCE can be a useful metric for describing aerosol properties of wildfire emissions and their impacts on regional air quality and global climate.


Journal of Geophysical Research | 2017

Airborne Measurements of Western U.S. Wildfire Emissions: Comparison with Prescribed Burning and Air Quality Implications

Xiaoxi Liu; L. Gregory Huey; Robert J. Yokelson; Vanessa Selimovic; Isobel J. Simpson; Markus Müller; Jose L. Jimenez; Pedro Campuzano-Jost; Andreas J. Beyersdorf; D. R. Blake; Zachary Butterfield; Yonghoon Choi; John D. Crounse; Douglas A. Day; Glenn S. Diskin; Manvendra K. Dubey; Edward Charles Fortner; T. F. Hanisco; Weiwei Hu; Laura E. King; Lawrence I. Kleinman; Simone Meinardi; Tomas Mikoviny; Timothy B. Onasch; Brett B. Palm; J. Peischl; Ilana B. Pollack; Thomas B. Ryerson; Glen W. Sachse; Arthur J. Sedlacek

Wildfires emit significant amounts of pollutants that degrade air quality. Plumes from three wildfires in the western U.S. were measured from aircraft during the Studies of Emissions and Atmospheric Composition, Clouds and Climate Coupling by Regional Surveys (SEAC^4RS) and the Biomass Burning Observation Project (BBOP), both in summer 2013. This study reports an extensive set of emission factors (EFs) for over 80 gases and 5 components of submicron particulate matter (PM_1) from these temperate wildfires. These include rarely, or never before, measured oxygenated volatile organic compounds and multifunctional organic nitrates. The observed EFs are compared with previous measurements of temperate wildfires, boreal forest fires, and temperate prescribed fires. The wildfires emitted high amounts of PM_1 (with organic aerosol (OA) dominating the mass) with an average EF that is more than 2 times the EFs for prescribed fires. The measured EFs were used to estimate the annual wildfire emissions of carbon monoxide, nitrogen oxides, total nonmethane organic compounds, and PM_1 from 11 western U.S. states. The estimated gas emissions are generally comparable with the 2011 National Emissions Inventory (NEI). However, our PM_1 emission estimate (1530 ± 570 Gg yr^(−1)) is over 3 times that of the NEI PM_(2.5) estimate and is also higher than the PM_(2.5) emitted from all other sources in these states in the NEI. This study indicates that the source of OA from biomass burning in the western states is significantly underestimated. In addition, our results indicate that prescribed burning may be an effective method to reduce fine particle emissions.


Optical Technologies for Industrial, Environmental, and Biological Sensing | 2004

Application of UV-Raman spectroscopy to the detection of chemical and biological threats

Arthur J. Sedlacek; Steven D. Christesen; Tom Chyba; Pat Ponsardin

Brookhaven National Laboratory (BNL), Edgewood Chemical and Biological Center (ECBC) and ITT Industries Advanced Engineering and Sciences Division (AES) have been collaborating on the transitioning and subsequent development of a short-range, non-contact Raman lidar system specifically designed to detect and identify chemical agents on the battlefield. [The instrument, referred to as LISA (Laser Interrogation of Surface Agents), will the subject of an accompanying paper.] As part of this collaboration, BNL has the responsibility for developing a spectral database (library) of surrogates and precursors for use with LISA’s pattern recognition algorithms. In this paper, the authors discuss the phenomenon of UV Raman and resonance-enhanced Raman spectroscopy, the development of an instrument-independent Raman spectral library, and highlight the exploitable characteristics present in the acquired spectral signatures that suggest potential utility in our country’s efforts on Homeland Security.

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Stephen R. Springston

Brookhaven National Laboratory

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Manvendra K. Dubey

Los Alamos National Laboratory

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Anne Jefferson

Cooperative Institute for Research in Environmental Sciences

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Chongai Kuang

Brookhaven National Laboratory

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Thomas Watson

Brookhaven National Laboratory

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Annette Koontz

Pacific Northwest National Laboratory

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John E. Shilling

Pacific Northwest National Laboratory

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Gunnar Senum

Brookhaven National Laboratory

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Jerome D. Fast

Pacific Northwest National Laboratory

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