Dc. Ferguson et al., Evidence for Martian electrostatic charging and abrasive wheel wear from the Wheel Abrasion Experiment on the Pathfinder Sojourner rover, J GEO R-PLA, 104(E4), 1999, pp. 8747-8759
The Wheel Abrasion Experiment (WAE) on the Mars Pathfinder rover was design
ed to find out how abrasive the Martian dust would be on strips of pure met
als attached to one of the wheels. A specially modified wheel, with 15 thin
film samples (five each of three different metals), specularly reflected s
unlight to a photovoltaic sensor. When the wheel was rotated to present the
different sample surfaces to the sensor, the resulting signal was interpre
ted in terms of dust adhesion and abrasive wear. Many data sequences were o
btained. Ground tests of similar wheels in a simulated Martian environment
showed that static charging levels of 100-300 V could be expected. To preve
nt the possibility of Paschen discharge in the low-pressure Martian atmosph
ere, charge dissipation points were added to the Sojourner rover and were s
hown in ground tests to keep charging levels at 80 V or less. Nevertheless,
significant dust accumulations on Sojourner's wheels may be interpreted as
evidence for electrostatic charging. Simple considerations of the expected
maximum level of charging and electrostatic dust adhesion lead to an estim
ate for the size of the adhering dust grains. From the WAE data, it is hypo
thesized that the photoelectric effect is the most important mechanism for
slow discharge in Martian daylight. Sensor signals obtained late in the Pat
hfinder mission show that significant wheel wear was seen on the metal whee
l strips, with the most wear on the thinnest aluminum samples and the least
on the thickest nickel and platinum samples. An estimate is made of the re
flectance of the adhering Martian dust. The depth of dig of the WAE wheel s
hows that the dust is in some places very loose and in others tightly packe
d. Finally, comparison of the WAE results with ground test results makes po
ssible a comparison of the Martian soil with mineral grain types and sizes
found on Earth and show that the Martian dust is fine-grained and of limite
d hardness.