The Mystery of Asteroid Oljato's Magnetic Disturbance
Oljato orbits the Sun once every 3.2 years. During its lifetime, NASA’s Pioneer Venus Orbiter observed three passages of Oljato between Venus and the Sun. Each time, there was a marked increase in the region of unusual magnetic peaks known as Interplanetary Field Enhancements (IFEs), both ahead and behind the asteroid.
Russell said, “This is not typical asteroidal behavior! These magnetic increases are rare, occurring in Venus orbit about 10 times per year. Pioneer observed that when Oljato was just in front or just behind Venus, the rate of IFEs approximately trebled. And yet, in more recent observations with Venus Express, the occurrence of IFEs is now lower than the average we find outside this region.”
Russell explained, “At one point in time Oljato shed boulders -- mostly a few tens of meters in diameter -- into its orbit and they formed a debris trail in front and behind Oljato. These impactors then hit other targets as they passed between Venus and the Sun. The large amount of fine dust released by these collisions was picked up by the solar wind, producing the IFEs observed by Pioneer, and was accelerated out of the solar system.”
The reduced rate of IFEs observed during the Venus Express epoch suggests that the collisions with Oljato’s co-orbiting material have reduced the general debris in the region as well as the co-orbiting material shed by Oljato.
“The IFEs observed by Pioneer suggest that more than 3 tons of dust was being lost from the region each day. Effects associated with solar heating and gravitational perturbations have gradually nudged larger chunks of debris away from Oljato’s orbit. From once being unusually crowded, the region has become unusually clear and free of IFEs,” said Russell.