Plasma clouds associated with Comet P/Borrelly dust impacts

Details Plasma clouds associated with Comet P/Borrelly dust impacts Plasma clouds associated with Comet P/Borrelly dust impacts

Jan 2004

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2004icar..167...89t&link_type=abstract

Icarus, Volume 167, Issue 1, p. 89-99.

Computer Science

4

Comets, Impact Processes, Instrumentation, Interplanetary Dust

Scientific paper

The NASA DS1 spacecraft encountered Comet P/Borrelly on September 22, 2001 at a distance of ~2171 km on the sunward side of the comet. The flyby speed was ~16.5 kms-1. Using high temporal resolution (50 μs) absolute electric field amplitude measurements from a ~1 m dipole antenna, new features of plasma clouds created by cometary dust impacts have been detected. The pulses have 1/e exponential decays of ~650 μs duration, exponentially shaped overshoots with rise times of ~2 ms, and exponential-shaped overshoot decay times of ~10 ms. Assuming a plasma temperature of 104 K, these pulse features have been explained as plasma cloud space charge effects from the electron, proton and heavy ion portions of the clouds passing the antenna. Complex pulse shapes were also detected. These are believed to be due to either plasma cloud scattering off of the spacecraft, or to secondary impacts. Small electric pulses of duration 10-15 ms of cometary origin were detected but are presently unexplained. The electric component of the plasma wave spectra at closest approach had an f-2.4 power law shape from 10 Hz to 1 kHz. The electron cyclotron frequency was approximately 1 kHz. One possible explanation of the wave spectrum is that whistler mode waves associated with phase steepened cometary plasma waves are dispersed, leading to the broad spectrum. Finally, based on the present results, a new type of low-cost, large-area dust detector is proposed.

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