Lunar Ejecta and Meteorites Experiment
The Lunar Ejecta and Meteorites Experiment was a lunar science experiment that flew to the Moon on board Apollo 17 in 1972. It collected information on dust particles produced as a result of meteoroid impacts on the surface of the Moon.
Background
Instruments on Pioneer 8 and Pioneer 9 were believed to have detected at least two instances of interstellar dust particles. It was therefore believed that the LEAM experiment would be able to distinguish dust particles of interstellar origins from other sources of cosmic dust.Instrument
The LEAM instrument was designed to ascertain a dust particle's speed, direction, kinetic energy and momentum. LEAM had three detectors: east, west, and up. The east and top sensors consist of a series of pairs of parallel film-grid arrays placed apart. The rear film-grid array was mounted to an acoustic impact plate.As high-velocity particles enter the detector, they interact with the front film sensor. Some of the particle's kinetic energy results in the creation of an ionised plasmas. Electrons are collected by a positively charged grid. Positive ions are collected on a negatively charged grid. Lower energy high-velocity particles will have all of their kinetic energy used in the creation of plasma and not interact further with the sensor.
High energy high-velocity particles may not generate any plasma at the first grid array and go on to interact with the second film grid and make contact with the rear impact plate generating a second plasma pulse. If the particle's momentum is sufficient it will generate an acoustic signal on the plate. Time of flight through the sensors is recorded to establish the particle's speed. The west sensor omitted the front film array and as a result, could not measure the speed of dust particles. Control sensors were coated with an epoxy resin to isolate them from the ionization products. A control microphone was provisioned in the experiment by having a place one-third the size.