NASA Logo

NTRS

NTRS - NASA Technical Reports Server

Back to Results
Lunar portable magnetometer experimentThe purpose of the Apollo 16 lunar portable magnetometer (LPM) experiment is to measure the permanent magnetic field at different geological sites on the lunar surface. The LPM field measurements are a vector sum of the steady remanent field from the lunar crust and of the time-varying ambient fields. The remanent magnetic fields measured in the Descartes region are the largest extraterrestrial fields yet measured in situ. These measurements show for the first time that the Descartes highlands have a stronger remanent magnetization than do the mare regions of the previous Apollo landing sites. The experimental technique used in the LPM experiment is described and the preliminary results obtained are discussed.
Document ID
19730013017
Acquisition Source
Legacy CDMS
Document Type
Other
Authors
Dyal, P.
(NASA Ames Research Center Moffett Field, CA, United States)
Parkin, C. W.
(NASA Ames Research Center Moffett Field, CA, United States)
Sonett, C. P.
(NASA Ames Research Center Moffett Field, CA, United States)
Dubois, R. L.
(Okla. Univ.)
Simmons, G.
(MIT)
Date Acquired
August 7, 2013
Publication Date
January 1, 1972
Publication Information
Publication: Apollo 16 Prelim. Sci. Rept.
Subject Category
Space Sciences
Accession Number
73N21744
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
Document Inquiry

Available Downloads

There are no available downloads for this record.
No Preview Available