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Hagermann, A.; Tanaka, S.; Yoshida, S.; Hayakawa, M.; Fujimura, A. and Mizutani, H.
(2001).
URL: http://www.lpi.usra.edu/meetings/lpsc2001/pdf/1497...
Abstract
For determining the lunar heat flow two parameters need to be measured: The thermal gradient and the thermal conductivity of the regolith. Methods for inferring these quantities from in situ measurements using the LUNAR-A penetrators will be presented.