Ionic Reactions in the Earth's Upper Atmosphere.

Abstract

Measurements made on the selected-ion flow-tube at the Air Force Geophysics Laboratory on the temperature dependence of several ion-molecule reaction rate coefficients. The N(+) + CO and C(+)+ NO systems were studied over a range of 9 - 450 K. Measurements were also made on C(+) + O2, CO+ + O2, and CO2(+) + O2 over the range 90 - 450 K. Comparison with available earlier results showed agreement within experimental uncertainty. A flowing afterglow apparatus was developed at Oklahoma for the study of ion interactions. Positive-ion/negative ion recombination was studied in this apparatus. Preliminary work was carried out for the Cl2(+) + Cl system and photographic documentation is used to determine the strength of the recombination process. (Author)

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Document Details

Document Type
Technical Report
Publication Date
Mar 01, 1984
Accession Number
ADA141185

Entities

People

  • T. M. Miller

Organizations

  • University of Oklahoma

Tags

Communities of Interest

  • Materials and Manufacturing Processes

DTIC Thesaurus Topics

  • Afterglows
  • Air Force
  • Atmospheric Sciences
  • Charge Transfer
  • Classification
  • Cyclotron Resonance
  • Electron Energy
  • Energy
  • Energy Production
  • Excitation
  • Geophysics
  • Ion Density
  • Measurement
  • Oklahoma
  • Physics
  • Uncertainty
  • Universities

Fields of Study

  • Environmental science

Readers

  • Molecular Photonics/Laser Physics
  • Technical Research and Report Writing.