Why Do Some Asteroids Spin Themselves to Dust?

Astronomers Spy Out Active Asteroids

Active asteroid P/2012 F5 captured by Keck II/DEIMOS in mid-2014. Top panel shows a wide-angle view of the main nucleus and smaller fragments embedded in a long dust trail. Bottom panel shows a close-up view with the trail numerically removed to enhance the visibility of the fragments.  CREDIT: M. DRAHUS, W. WANIAK (OAUJ) / W. M. KECK OBSERVATORY

In the “Department of Unusual Solar System Activities” today we have a close look at a type of asteroid that may spin so fast that it literally explodes itself as it ejects dust out to space. This comes to us courtesy of the W.M. Keck Observatory in Hawai’i, and a team of astronomers at the Jagellonian University of Krakow, Poland. To date, astronomers know of a handful of these busy objects and are seeking to understand why they do what they do.

The main asteroid belt of our solar system is likely a pretty orderly place, with asteroids moving along in their orbits without too many collisions, sort of like a well-run superhighway. But, sometimes things happen, even on a smoothly moving roadway. One car runs into another and that sets one or both of them spinning. Or, a truck has a blowout on its tire, and that sends it weaving all over the road.

In the case of the asteroid belt, which is home to the very fascinating Ceres dwarf planet (currently being studied by the Dawn spacecraft), we’re talking about “active asteroids” that are posing some interesting challenges to astronomers studying them. These are asteroids that eject steams of ice particles out as they orbit, most of the time in a steady jet. But, in 2010, astronomers found a more “explody” version of these objects. They eject material in shots, sort of like that tire blowout. The reasons they do this aren’t clear yet, but there are two ideas to explain them. One is that two objects—one moving very fast (say, at hypervelocity (which means really high velocity)) running into another. That causes one or both to catastrophically spew ice particles and dust to space in giant spurts.

The other idea is that an active asteroid experiences “rotational disruption”. That literally means it rotates so fast and wildly that it alters the shape of the asteroid, introducing cracks and crevices and fragmenting the body. As the active asteroid spins, it launches dust and ice chunks, which further unbalancing itself. Eventually, it can break apart.

The astronomers on the team using Keck focused in on a specific one that had caught their interest to see if they could capture a view of one of these tiny objects and figure out what makes it so unusual. The object they chose is called P/2012 F5, which had a big dust outburst in 2011. They wanted to measure its rotation rate (how fast it spins on its axes), and whether or not it was fragmented and broken apart. They found four large fragments in the object, which is rotating once every 3.2 hours. That’s fast enough to cause these impulsive explosions that result in dust and ice outbursts. For now, this object is still one big fragmented body. As it rotates, it is heated by the Sun on different sides and it’s possible that one day it will rotate itself apart, sending more ice and dust and fragments into space.

Interestingly, P/2012 F5 was first thought to be a comet due to its outbursts. Astronomers now know that it’s a fragmented asteroid, acting like a comet. Why it’s rotating and how it got fragmented—those are questions still to be answered.

Back in graduate school, we often talked about “asteroids acting like comets”, although they were quite rare. Now, what was once rare is an observable object, giving us another look at how amazing varied the places in our solar system can be.

Messenger Readies For its Last Weeks at Mercury

Low Flyovers Will Give the Best Close-up Views

Does this image prove water ice near the poles of Mercury? Here’s how a Mercury MESSENGER scientist sees it. The top left view shows the crater rim outlined in pink and the edge of the 24-meter/pixel, low-altitude broadband MDIS instrument image in green. The large bottom image (with processing) reveals details of the shadowed surface inside the crater. The yellow arrows in the top right image indicate a region inside the crater that has a lower reflectance. The edge of the low-reflectance region has a sharp and well-defined boundary. The sharp boundary suggests that the low-reflectance material is sufficiently young to have preserved a sharp boundary against lateral mixing by impact craters. The sharp boundary matches the location predicted by temperature models for the stability of a surface layer of volatile, organic-rich material tens of centimeters thick on top of a thicker layer of water ice. Courtesy: NASA/Johns Hopkins University Applied Physics Laboratory/Carnegie Institution of Washington

Sometime in the next few months, the long-running MESSENGER mission at Mercury is going to take its last swoop over the planet, and then angle into Mercury’s surface. The long-planned Hover Campaign, uses orbit-correction maneuvers to delay the spacecraft’s final plunge for a few weeks so that they can send it on some low-pass runs and get some last good birds-eye views of the cratered terrain. They’ll also be using the spacecraft’s magnetometer (which senses the magnetic fields and magnetic anomalies in the surface), and the neutron spectrometer, which will let them get more data on the crustal composition.

In particular, the mission scientists want to zero in on those mysterious shadowed craters at Mercury’s poles, to study the water ice that exists within their chilly dark areas. If it does, then they’ll have some proof that water can exist in this region, and try to figure out just how the water got there. One idea is that comet bombardments could have deposited ice in these regions. Since the walls of the craters do not get sunlight, the ice could have been safely locked away there for a while.

How long? It’s a good question. The images and data returned about Mercury ice so far indicate that it is relatively young, meaning it was delivered (or uncovered) in recent geological time.  Mercury ice is a mystery, and although it sounds crazy that ice could exist so close to the Sun, the MESSENGER images and data have shown that it’s there and sitting there quite happily NOT getting melted by sunlight. It’s yet another dazzling result delivered from a very successful mission.

Why the rush to get MESSENGER in low swooping and controlled orbits? Well, the spacecraft is running out of propellant, and its subject to the gravitational pull of the Sun, both of which will combine to send it to its final resting place on Mercury. Mission controllers are taking advantage now of the spacecraft’s continuing good health to plan the final views and studies, and giving it the best altitude to do so. Once the propellant is gone, that’s the end of the road for a mission that has lasted since its 2004 launch, and has been orbiting Mercury since March 18, 2011. I remember the evening it went into orbit; we went down to the University of Colorado’s Laboratory for Atmospheric and Space Physics (my old employer) to sit with friends who are on the spacecraft team and watch as the mission slipped into orbit around the planet after a nearly five-year trip to get there.

The MESSENGER spacecraft is the first ever to orbit the planet Mercury, and the spacecraft’s seven scientific instruments and radio science investigation have done a spectacular job of studying this world, and helping us to understand its history and evolution. MESSENGER has acquired over 250,000 images and extensive other data sets. I suspect that there will be many incredible papers written about this treasure trove of information about the solar system’s smallest rocky planet. Stay tuned as MESSENGER spends her final weeks cranking out some spectacular science!

Exploring Science and the Cosmos

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