Gå direkt till innehållet
Geophysik III
Spara

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.
Redaktör
Karl Rawer
Upplaga
Softcover reprint of the original 1st ed. 1982
ISBN
9783642809095
Språk
Engelska
Vikt
310 gram
Utgivningsdatum
11.1.2012
Sidor
386