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Geophysik III
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Geophysik III

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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.
Redaktör
Karl Rawer
Upplaga
Softcover reprint of the original 1st ed. 1982
ISBN
9783642809095
Språk
Engelska
Vikt
310 gram
Utgivningsdatum
2012-01-11
Sidor
386