Publikationsdatum:
2019-07-13
Beschreibung:
Data from the Charged Particle Lunar Environment Experiment (CPLEE), at the Apollo 14 site, are used to investigate the interactive properties of the plasma sheet and the lunar photoelectron layer. It is shown that the predictions of the Guernsey-Fu model are compatible with SIDE but not CPLEE observations. The apparent contradiction is resolved by fitting the remanent magnetic field to that of a dipole buried about 1.1 km beneath the surface. In this case a charge separation layer must form above the instrument due to the different rigidities of plasma sheet electrons and protons. The qualitative properties of the charge separation layer needed to reconcile CPLEE and SIDE observations are presented.
Schlagwort(e):
LUNAR AND PLANETARY EXPLORATION
Materialart:
Lunar Science Conference; Mar 17, 1975 - Mar 21, 1975; Houston, TX
Format:
text
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