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Geophysik III

  • Book
  • © 1982

Overview

Part of the book series: Handbuch der Physik Encyclopedia of Physics (HDBPHYS, volume 10 / 49 / 6)

Part of the book sub series: Geophysik / Geophysics (PHYSIK 10)

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Keywords

  • Geophysik

About this book

83 input to the ions is balanced by a cooling to atomic oxygen, the major neutral constituent, and measurements of the difference between ion and neutral tem­ perature permit the determination of atomic oxygen concentrations. Using this approach, ALCA YDE et al. 6 have shown from data taken above Saint Santin, France, that the atomic oxygen concentration at 200 km is slightly larger in winter than summer. () The molecular concentrations at heights near 200 km can also be derived from a determination of the ratio of the molecular-ion concentration to elec­ tron concentration, p (Cox and EVANS 7). It can be shown from the steady­ state form of the continuity equation for 0+ ions that (20.2) where Q(O+) represents the photoionization coefficient of oxygen atoms, and k and k19 represent the rate coefficients of reactions between 0+ ions and 1S molecular nitrogen Illld oxygen (reactions (12.18) and (12.19)). Then the ratio of atomic oxygen to weighted molecular sum is given by: (l-p)Ne [OJ (20.3) Q(O+) , [kMJ where Ne represents the electron concentration.

Authors and Affiliations

  • March-Hugstetten, Germany

    K. Rawer

Bibliographic Information

  • Book Title: Geophysik III

  • Authors: G.M. Nikol'skij, K. Rawer, P. Stubbe, L. Thomas, T. Yonezawa

  • Editors: Karl Rawer

  • Series Title: Handbuch der Physik Encyclopedia of Physics

  • Publisher: Springer Berlin, Heidelberg

  • eBook Packages: Springer Book Archive

  • Copyright Information: Springer-Verlag Berlin Heidelberg 1982

  • Softcover ISBN: 978-3-642-80909-5Published: 11 January 2012

  • Series ISSN: 0085-140X

  • Series E-ISSN: 2197-4195

  • Edition Number: 1

  • Number of Pages: VI, 386

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