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Geophysik III
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Geophysik III

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.
Redaktør
Karl Rawer
Opplag
Softcover reprint of the original 1st ed. 1982
ISBN
9783642809095
Språk
Engelsk
Vekt
310 gram
Utgivelsesdato
11.1.2012
Antall sider
386