A direct test of the poorly understood physical properties of rubble-pile asteroids was provided by the forces measured during the interaction between NASA's OSIRIS-REx and asteroid Bennu. A Southwest Research Institute-led study has found that the layer just below the asteroid's surface is composed of weakly bound rock fragments.
A paper about this research was published in the journal Science Advances. The low density weakly bound subsurface layer should be a global property of Bennu.
Bennu is a spheroidal collection of rock fragments and debris 1,700 feet in diameter. It is believed that it was formed after a collision. It has had a rough and tumble existence since it was liberated from its larger parent asteroid millions of years ago.
The OSIRIS-REx mission is to collect and return at least 60 grams of surface material from Bennu in order to deliver it to Earth. Additional insights came from sample collection activities.
Bennu's thermal properties and craters have been measured by researchers involved in the OSIRIS-REx mission. The regolith at an asteroid's surface has not been probed before.
The Sample Acquisition Verification Camera (SamCam) of the OSIRIS-REx Camera Suite captured images during and after the sampling event.
Ron Ballouz is a co-author of the paper. Every visible particle is moved or reoriented at all points along the circle of TAG SAM.
The downward force of TAG SAM lifted a large rock. Small debris was lofted off the rock's surface after it was reoriented and strengthened. The mobility of the millimeter-scale particles suggests that they are not cohesive with the larger rock.
The average regolith particle size increases as asteroid size decreases, according to scientists. Bennu was compared to rubble-pile asteroids.
There are ponds of small particles across 20% of the surface of Bennu and Itokawa. The compressed surface of the latter could be one of the reasons, along with the recent reorganization of the body.
The 30-foot-long elliptical crater excavated by the TAG SAM arm was described in a companion paper. The event exposed material that was darker and more abundant in fine particulates than the original surface. The bulk density of the displaced material is less than that of the asteroid as a whole.
More information: Kevin J. Walsh et al, Near-zero cohesion and loose packing of Bennu's near subsurface revealed by spacecraft contact, Science Advances (2022). DOI: 10.1126/sciadv.abm6229The Spacecraft sample collection and subsurface excavation of asteroid 101955 Bennu was written by D.S. Lauretta. There is a science.abm1018
Journal information: Science Advances , Science