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Articles
Apollo 12 Seismic Signal: Indication of a Deep Layer of Powder
1 Center for Radiophysics and Space Research, Cornell University, Ithaca, New York 14850
The seismic signal caused by the Apollo 12 lunar module is interpreted in terms of propagation between source and receiver through a layer of powder in which sound velocity increases with depth. This increase, which is due to compaction, extends over several kilometers and leads to a concentration of seismic waves toward the surface. Computer simulations with the use of ray acoustics and on the assumption of a randomly undulating lunar surface approximate well the observed signal. Seismic amplitudes are greatly enhanced in such a medium compared to solid rock, so that the observed signal requires less power to be transmitted than previously estimated.
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Science. ISSN 0036-8075 (print), 1095-9203 (online)