Geophysik III (Paperback, Softcover reprint of the original 1st ed. 1982)

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.

General

Imprint:	Springer-Verlag
Country of origin:	Germany
Series:	Geophysik / Geophysics, 10 / 49 / 6
Release date:	2012
First published:	1982
Authors:	G M Nikol'skij
Editors:	Karl Rawer
Authors:	K. Rawer • P Stubbe • L. Thomas • T. Yonezawa
Dimensions:	244 x 170 x 20mm (L x W x T)
Format:	Paperback
Pages:	386
Edition:	Softcover reprint of the original 1st ed. 1982
ISBN-13:	978-3-642-80909-5
Categories:	Books > Science & Mathematics > Physics > Applied physics & special topics > Geophysics
LSN:	3-642-80909-X
Barcode:	9783642809095

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