Space Telescope Witnesses Asteroid Smashup

Using NASA's Spitzer Space Telescope, astronomers including Wiphu Rujopakarn of the Kavli IPMU have spotted an eruption of dust around a young star, possibly the result of a smashup between large asteroids. This type of collision can eventually lead to the formation of planets. The results of this study are published in the journal Science.

Figure 1: This artist’s concept shows a large asteroid impact around NGC 2547-ID8, a 35-million-year-old sun-like star thought to be forming rocky planets. NASA's Spitzer Space Telescope witnessed a giant surge in dust around the star, likely the result of two asteroids colliding. Credit: Kavli IPMUFigure 1: This artist’s concept shows a large asteroid impact around NGC 2547-ID8, a 35-million-year-old sun-like star thought to be forming rocky planets. NASA's Spitzer Space Telescope witnessed a giant surge in dust around the star, likely the result of two asteroids colliding. Credit: Kavli IPMU

Figure 2: NGC2547, open cluster located about 1,200 light-years from Earth in the constellation Vela. Credit: ESO/Digitized Sky Survey 2/Kavli  IPMUFigure 2: NGC2547, open cluster located about 1,200 light-years from Earth in the constellation Vela. Credit: ESO/Digitized Sky Survey 2/Kavli IPMU
 Figure 3: Zoom up of the central part of Figure 2. NGC 2547-ID8 locates at the center of the circle in the middle of the picture. Credit:  ESO/Digitized Sky Survey 2/Kavli  IPMUFigure 3: Zoom up of the central part of Figure 2. NGC 2547-ID8 locates at the center of the circle in the middle of the picture. Credit: ESO/Digitized Sky Survey 2/Kavli IPMU

Scientists had been regularly tracking the star, called NGC 2547-ID8, when it surged with a huge amount of fresh dust between August 2012 and January 2013.

"We think two big asteroids crashed into each other, creating a huge cloud of grains the size of very fine sand, which are now smashing themselves into smithereens and slowly leaking away from the star," said lead author and graduate student Huan Meng of the University of Arizona, Tucson.

While dusty aftermaths of suspected asteroid collisions have been observed by Spitzer before, this is the first time scientists have collected data before and after a planetary system smashup. The viewing offers a glimpse into the violent process of making rocky planets like ours.

Rocky planets begin life as dusty material circling around young stars. The material clumps together to form asteroids that ram into each other. Although the asteroids often are destroyed, some grow over time and transform into proto-planets. After about 100 million years, the objects mature into full-grown, terrestrial planets. Our moon is thought to have formed from a giant impact between proto-Earth and a Mars-size object.

In the new study, Spitzer set its heat-seeking infrared eyes on the dusty star NGC 2547-ID8, which is about 35 million years old and lies in the Vela constellation. Previous observations had already recorded variations in the amount of dust around the star, hinting at possible ongoing asteroid collisions. In hope of witnessing an even larger impact, which is a key step in the birth of a terrestrial planet, the astronomers turned to Spitzer to observe the star regularly. Beginning in May 2012, the telescope began watching the star, sometimes daily.

A dramatic change in the star came during a time when Spitzer had to point away from NGC 2547-ID8 because our sun was in the way. When Spitzer started observing the star again five months later, the team was shocked by the data they received.

"We not only witnessed what appears to be the wreckage of a huge smashup, but have been able to track how it is changing -- the signal is fading as the cloud destroys itself by grinding its grains down so they escape from the star," said Kate Su of the University of Arizona and co-author on the study. "Spitzer is the best telescope for monitoring stars regularly and precisely for small changes in infrared light over months and even years."

A very thick cloud of dusty debris now orbits the star in the zone where rocky planets form. As the scientists observe the star system, the infrared signal from this cloud varies based on what is visible from Earth. For example, when the elongated cloud is facing us, more of its surface area is exposed and the signal is greater. When the head or the tail of the cloud is in view, less infrared light is observed. By studying the infrared oscillations, the team is gathering first-of-its-kind data on the detailed process and outcome of collisions that create rocky planets like Earth.

"This is what we have been teaching our schoolchildren about how planets like our Earth was formed. To witness it in our lifetime in a truly extraordinary opportunity" said Wiphu Rujopakarn of the Kavli IPMU and co-author on the study.

The team is continuing to keep an eye on the star with Spitzer. They will see how long the elevated dust levels persist, which will help them calculate how often such events happen around this and other stars, and they might see another smashup while Spitzer looks on.

The results of this study are published in the journal Science.

Figure 4:Witnessing a Planetary Wreckage: Astronomers were surprised to see these data from NASA's Spitzer Space Telescope in January 2013, showing a huge eruption of dust around a star called NGC 2547-ID8. In this plot, infrared brightness is represented on the vertical axis, and time on the horizontal axis. The data at left show infrared light from the dust around the star back in 2012. Between 2012 and 2013, Spitzer had to stop observing the star because it was located behind the sun, as seen from Spitzer's Earth-trailing orbit.
When Spitzer began watching the star again in January 2013, the astronomers noticed a huge jump in the data. Why the dramatic change? The team says that dust in the star system surged intensely, likely after two large asteroids collided, kicking up fresh dust.
The periodic variability of the signal is caused by the remaining dust cloud in orbit around the star. This dust cloud is elongated, so the amount of infrared signal it produces changes as it circles the star from our point of view. The infrared signal is decreasing over time as dust from the collision is ground down to finer sizes and blown of the system. 
Image credit: NASA/JPL-Caltech/University of Arizona Figure 4:Witnessing a Planetary Wreckage: Astronomers were surprised to see these data from NASA's Spitzer Space Telescope in January 2013, showing a huge eruption of dust around a star called NGC 2547-ID8. In this plot, infrared brightness is represented on the vertical axis, and time on the horizontal axis. The data at left show infrared light from the dust around the star back in 2012. Between 2012 and 2013, Spitzer had to stop observing the star because it was located behind the sun, as seen from Spitzer's Earth-trailing orbit.
When Spitzer began watching the star again in January 2013, the astronomers noticed a huge jump in the data. Why the dramatic change? The team says that dust in the star system surged intensely, likely after two large asteroids collided, kicking up fresh dust.
The periodic variability of the signal is caused by the remaining dust cloud in orbit around the star. This dust cloud is elongated, so the amount of infrared signal it produces changes as it circles the star from our point of view. The infrared signal is decreasing over time as dust from the collision is ground down to finer sizes and blown of the system.
Image credit: NASA/JPL-Caltech/University of Arizona

Publication

Journal:

Science
Vol. 345 no. 6200 pp. 1032-1035
DOI: 10.1126/science.1255153
http://www.sciencemag.org/content/345/6200/1032
 

Title:

Large impacts around a solar-analog star in the era of terrestrial planet formation

Authors:

Huan Y. A. Meng,1 Kate Y. L. Su,2 George H. Rieke,1,2 David J. Stevenson,3 Peter Plavchan,4,5 Wiphu Rujopakarn,2,6,7 CareyM. Lisse,8 Saran Poshyachinda,9 Daniel E. Reichart10

Affiliations:

1Lunar and Planetary Laboratory and Department of Planetary Sciences, University of Arizona, 2Steward Observatory and Department of Astronomy, University of
Arizona, 3Division of Geological and Planetary Sciences, California Institute of Technology, 4NASA Exoplanet Science Institute, California Institute of Technology, 5Missouri State University, 6Department of Physics, Faculty of Science, Chulalongkorn University, 7Kavli Institute for the Physics and Mathematics of the Universe (WPI), Todai Institute for Advanced Study, University of Tokyo, 8Space Department, Applied Physics Laboratory, Johns Hopkins University, 9National Astronomical Research Institute of Thailand (Public Organization), Ministry of Science and Technology, 10Department of Physics and Astronomy, Campus Box 3255, University of North Carolina at Chapel Hill.

Contacts

Science Contact:

Wiphu Rujopakarn
Kavli Institute for the Physics and Mathematics of the Universe, The University of Tokyo

wiphu.rujopakarn_at_ipmu.jp
+81-4-7136-6555

PIO Contact:

Yoshihisa Obayashi
Kavli Institute for the Physics and Mathematics of the Universe, The University of Tokyo
press_at_ipmu.jp
+81-4-7136-5974

(replace _at_ by @ when you send e-mail.)

About Kavli IPMU

Kavli IPMU (Kavli Institute for the Physics and Mathematics of the Universe) is an international research institute with English as its official language. The goal of the institute is to discover the fundamental laws of nature and to understand the Universe from the synergistic perspectives of mathematics, astronomy, and theoretical and experimental physics. The Institute for the Physics and Mathematics of the Universe (IPMU) was established in October 2007 under the World Premier International Research Center Initiative (WPI) of the Ministry of Education, Sports, Science and Technology in Japan with the University of Tokyo as the host institution. IPMU was designated as the first research institute within Todai Institutes for Advanced Study (TODIAS) in January 2011. It received an endowment from The Kavli Foundation and was renamed the “Kavli Institute for the Physics and Mathematics of the Universe” in April 2012. Kavli IPMU is located on the Kashiwa campus of the University of Tokyo, and more than half of its full-time scientific members come from outside Japan. http://www.ipmu.jp/