D. Slusher
Georgia Institute of Technology
9 Papers
53 Citations
D. Slusher is an academic researcher from Georgia Institute of Technology. The author has contributed to research in topics: Chemical ionization & Firn. The author has an hindex of 8, co-authored 9 publications. Previous affiliations of D. Slusher include Coastal Carolina University.
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Papers
A thermal dissociation–chemical ionization mass spectrometry (TD‐CIMS) technique for the simultaneous measurement of peroxyacyl nitrates and dinitrogen pentoxide
TL;DR: In this article, a thermal dissociation-chemical ionization mass spectrometry (TD-CIMS) technique was developed for fast measurements of a series of peroxyacyl nitrates and dinitrogen pentoxide.
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An overview of ISCAT 2000
Douglas D. Davis,Fred L. Eisele,Fred L. Eisele,G. Chen,G. Chen,James H. Crawford,L. Gregory Huey,David B. Tanner,D. Slusher,Lee Mauldin,Steven P. Oncley,Donald H. Lenschow,S. R. Semmer,Richard E. Shetter,Barry Lefer,Richard Arimoto,A. Hogan,P. Grube,Matthew A. Lazzara,Alan R. Bandy,Donald C. Thornton,Harald Berresheim,Heinz Bingemer,Manuel A. Hutterli,Joseph R. McConnell,Roger C. Bales,Jack E. Dibb,M. P. Buhr,Ji Young Park,Peter H. McMurry,Aaron L. Swanson,Simone Meinardi,Donald R. Blake +32 more
TL;DR: The International Scientific and Technological Assessment of Sulfur Chemistry in the Antarctic Troposphere (ISCAT) was conducted at the Amundsen Scott Station in Antarctica from 15 November to 31 December 2000 as discussed by the authors.
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A chemical ionization technique for measurement of pernitric acid in the upper troposphere and the polar boundary layer
TL;DR: The potential of SF 6 for the detection of pemitric acid in air by chemical ionization mass spectrometry was studied in the laboratory via its reactions with HO 2 NO 2, O 3, H 2 O, and NO 2.
54
CIMS measurements of HNO3 and SO2 at the South Pole during ISCAT 2000
L. G. Huey,David J. Tanner,D. Slusher,Jack E. Dibb,Richard Arimoto,G. Chen,Douglas D. Davis,M. Buhr,John B. Nowak,Roy L. Mauldin,Fred L. Eisele,Fred L. Eisele,E. Kosciuch +12 more
TL;DR: A simple steady state photochemical analysis indicates that most of the time HNO 3 is deposited to the snow with a lifetime of the order of a few hours at the South Pole.