James Burkholder

Dr. James Burkholder


Research Focus & Metrics

Academic Career Length

32Years (1995-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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23 November 2007 in Physical Chemistry Chemical Physics
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Journal Article
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VPVassileios C. Papadimitriou
Vassileios C. Papadimitriou
RTRanajit K. Talukdar
Ranajit K. Talukdar
RPR. W. Portmann
R. W. Portmann
ARA. R. Ravishankara
A. R. Ravishankara
JBJames Burkholder
James Burkholder
Rate coefficients over the temperature range 206–380 K are reported for the gas-phase reaction of OH radicals with 2,3,3,3-tetrafluoropropene (CF3CFCH2), k1(T), and 1,2,3,3,3-pentafluoropropene ((Z)-CF3CFCHF), k2(T), which are major components in proposed substitutes for HFC-134a (CF3CFH2) in mobile air-conditioning units. Rate coefficients were measured under pseudo-first-order conditions in OH using pulsed-laser photolysis to produce OH and laser-induced fluorescence to detect it. Rate coefficients were found to be independent of pressure between 25 and 600 Torr (He, N2). For CF3CFCH2, the rate coefficients, within the measurement uncertainty, are given by the Arrhenius expression k1(T) = (1.26 ± 0.11) × 10−12 exp[(−35 ± 10)/T] cm3 molecule−1 s−1 where k1(296 K) = (1.12 ± 0.09) × 10−12 cm3 molecule−1 s−1. For (Z)-CF3CFCHF, the rate coefficients are given by the non-Arrhenius expression k2(T) = (1.6 ± 0.2) × 10−18T2 exp[(655 ± 50)/T] cm3 molecule−1 s−1 where k2(296 K) = (1.29 ± 0.06) × 10−12 cm3 molecule−1 s−1. Over the temperature range most relevant to the atmosphere, 200–300 K, the Arrhenius expression k2(T) = (7.30 ± 0.7) × 10−13 exp[(165 ± 20)/T] cm3 molecule−1 s−1 reproduces the measured rate coefficients very well and can be used in atmospheric model calculations. The quoted uncertainties in the rate coefficients are 2σ (95% confidence interval) and include estimated systematic errors. The global warming potentials for CF3CFCH2 and (Z)-CF3CFCHF were calculated to be <4.4 and <3.6, respectively, for the 100 year time horizon using infrared absorption cross sections measured in this work, and atmospheric lifetimes of 12 and 10 days that are based solely on OH reactive loss.

17 February 2017
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JBJames Burkholder
James Burkholder
JAJonathan P. D. Abbatt
Jonathan P. D. Abbatt
IBIan Barnes
Ian Barnes
JRJames M. Roberts
James M. Roberts
MMMegan L. Melamed
Megan L. Melamed
PZPaul J. Ziemann
Paul J. Ziemann

20 August 1995 in Journal of Geophysical Research: Atmospheres
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Journal Article
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JBJames Burkholder
James Burkholder
ARA. R. Ravishankara
A. R. Ravishankara
SSSusan Solomon
Susan Solomon

22 May 2013 in The Journal of Physical Chemistry A
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Journal Article
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MMMax R. McGillen
Max R. McGillen
MBMunkhbayar Baasandorj
Munkhbayar Baasandorj
JBJames Burkholder
James Burkholder

4 May 2018 in Atmospheric Chemistry and Physics
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Journal Article
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DPDimitrios K. Papanastasiou
Dimitrios K. Papanastasiou
ABAllison Beltrone
Allison Beltrone
Paul MarshallPaul Marshall
Paul Marshall
JBJames Burkholder
James Burkholder
Hydrochlorofluorocarbons (HCFCs) are ozone depleting substances and potent greenhouse gases that are controlled under the Montreal Protocol. However, the majority of the 274 HCFCs included in Annex C of the protocol do not have reported global warming potentials (GWPs) which are used to guide the phaseout of HCFCs and the future phase down of hydrofluorocarbons (HFCs). In this study, GWPs for all C1–C3 HCFCs included in Annex C are reported based on estimated atmospheric lifetimes and theoretical methods used to calculate infrared absorption spectra. Atmospheric lifetimes were estimated from a structure activity relationship (SAR) for OH radical reactivity and estimated O(1D) reactivity and UV photolysis loss processes. The C1–C3 HCFCs display a wide range of lifetimes (0.3 to 62 years) and GWPs (5 to 5330, 100-year time horizon) dependent on their molecular structure and the H-atom content of the individual HCFC. The results from this study provide estimated policy-relevant GWP metrics for the HCFCs included in the Montreal Protocol in the absence of experimentally derived metrics.

1 August 1999 in Geophysical Research Letters
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Journal Article
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RPRobert W. Portmann
Robert W. Portmann
SBSteven S. Brown
Steven S. Brown
TGTomasz Gierczak
Tomasz Gierczak
RTRanajit K. Talukdar
Ranajit K. Talukdar
JBJames Burkholder
James Burkholder
ARA. R. Ravishankara
A. R. Ravishankara