Watch Out! Galactic Collisions Could Snuff Out Star Formation

Galactic Collisions. Credit: Tomer Tal and Jeffrey Kenney/Yale University and NOAO/AURA/NSF

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It’s a violent universe out there! Yesterday we ran an article about galaxies colliding and forming fireballs. Today, there’s more evidence for galactic collisions, and it’s not good news for potential stars. While this image is stunning, such collisions could spell doom for future star formation. A deep new image of the Virgo cluster has revealed huge tendrils of ionized hydrogen gas 400,000 light-years long connecting the elliptical galaxy M86 and the disturbed spiral galaxy NGC 4438. This image, taken by the 4-meter telescope at Kitt Peak National Observatory, provides striking evidence of a previously unsuspected high-speed collision between the two galaxies. “Our data show that this system represents the nearest recent collision between a large elliptical galaxy and a large spiral,” said Jeffrey Kenney of Yale University, “This discovery provides some of the clearest evidence yet for high-speed collisions between large galaxies, and it suggests that the consequences of such collisions are a plausible alternative to black holes in trying to explain the mystery of what process turns off star formation in the biggest galaxies.”

Astronomers have been trying to understand the mystery of what causes the biggest galaxies in the Universe—which are primarily ellipticals, like M86—to stop forming stars. “Something needs to heat up the gas so it doesn’t cool and form stars,” Kenney says. “A number of recent studies suggest that energy from active galactic nuclei associated with supermassive black holes may do this, (see Universe Today articles here and here) but our new study shows that gravitational interactions may also do the trick.”

The Virgo cluster is located approximately 50 million light-years from Earth. Previous studies had noticed disturbed H-alpha gas around each of the two galaxies, but scientists didn’t think the two had a connection. Indeed, some results have suggested that NGC 4438 collided with the small lenticular galaxy NGC 4435, but NGC 4435 has a much higher line-of-sight velocity as seen from Earth and appears undisturbed.

Spectroscopy of selected regions along the filament between M86 and NGC 4438 shows a fairly smooth velocity gradient between the galaxies, supporting the collision scenario. And here’s the kicker: there are no obvious stars in the filaments.

As in most elliptical galaxies, most of the gas within M86 is extremely hot, and therefore radiates X-rays. The X-ray distribution in M86 is irregular and sports a long plume, which had previously been interpreted as a tail of gas which is being stripped by ram pressure as M86 falls into the intracluster medium of the Virgo cluster. The new H-alpha image from Kitt Peak suggests that most of the disturbances to the interstellar medium in M86 are instead due to the collision with NGC 4438.

Low-velocity collisions, especially between small- to medium-sized galaxies, often cause an increase in the local star formation rate, as the collisions tend to cause gas to concentrate in the galaxy centers. But in high velocity collisions (which happen naturally between large galaxies, since their large gravity pulls mass inward much faster), the kinetic energy of the collision can cause the gas to heat up so much that it cannot easily cool and form stars.

While not many galaxies suffer such extreme collisions as M86, most galaxies experience minor mergers and gas accretion events, and these may play a significant role in heating the galaxy’s gas. These more common but modest events are very hard to study, since their observational signatures are weak.

“The same physical processes occur in both strong and weak encounters, and by studying the observable effects in extreme cases like M86 we can learn about the role of gravity in the heating of galaxy gas, which appears to be quite significant,” Kenney adds.

Kenney is the lead author of a paper to be published in a November 2009 issue of Astrophysical Journal Letters.

Source: NOAO

Ozone Hole Bigger Again

Ozone hole during 7 October 2008 as measured by the Scanning Imaging Absorption Spectrometer for Atmospheric Cartography (SCIAMACHY) atmospheric sensor onboard ESA’s Envisat. Credits: KNMI/ESA

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Is the ozone hole was recovering? Maybe not. The protective atmospheric layer of ozone around our planet has been thinning over Antarctica for many years. New satellite data indicates the 2008 ozone hole is larger both in size and ozone loss than 2007 but is not as large as the record year of 2006. This year the area of the thinned ozone layer over the South Pole reached about 27 million square kilometers, compared to 25 million square kilometers in 2007 and a record ozone hole extension of 29 million square kilometers in 2006, which is about the size of the North American continent. Ozone is a protective atmospheric layer found about 25 kilometers in altitude that acts as a sunlight filter, shielding life on Earth from harmful ultraviolet rays. A thinner ozone layer can increase the risk of skin cancer and cataracts and harm marine life. What causes the ozone layer to change from year to year, and if CFC’s have been banned, why isn’t the ozone recovering?

The depletion of ozone is caused by extreme cold temperatures at high altitude and the presence of ozone-destructing gases in the atmosphere such as chlorine and bromine. Most of these gases originate from man-made products like chlorofluorocarbons (CFCs), which were phased out under the 1987 Montreal Protocol. But they continue to linger in the atmosphere.

Depending on the weather conditions, the size the Antarctic ozone hole varies every year. As the polar spring arrives in September or October, the combination of returning sunlight and the presence of so-called stratospheric clouds (PSCs) over the Antarctic leads to a release of highly ozone-reactive chlorine radicals present in the atmosphere that break ozone down into individual oxygen molecules. A single molecule of chlorine has the potential to break down thousands of molecules of ozone.

Chlorine activation and ozone hole extension early September 2007 and 2008.   Credits: DLR
Chlorine activation and ozone hole extension early September 2007 and 2008. Credits: DLR

Colder temperatures in the stratosphere over Antarctica, combined with a high formation rate of PSCs caused more lingering chlorine radicals to be released, making the current hole one of the largest. 2006 saw the largest hole. A unit of measurement called a Dobson Unit describes the thickness of the ozone layer, and this year (2008) about 120 Dobson Units were observed compared to around 100 Dobson Units in 2006.

The analysis is based upon the Scanning Imaging Absorption Spectrometer for Atmospheric Cartography (SCIAMACHY) atmospheric sensor onboard ESA’s Envisat, the Global Ozone Monitoring Experiment (GOME) aboard ESA’s ERS-2 and its follow-on instrument GOME-2 aboard EUMETSAT’s MetOp.

Source: ESA

A Different Side of Mercury

A different side of Mercury. Credit: NASA/Johns Hopkins University Applied Physics Laboratory/Carnegie Institution of Washington

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Here’s the first image from MESSENGER’s flyby of Mercury on Monday. The bright crater just south of the center of the image is Kuiper, which has been seen before on images from the Mariner 10 mission in the 1970s. But most of this image, to the east, or right of Kuiper, toward the limb of Mercury is new territory for human eyes – at least in optical views. The image was taken by the Wide Angle Camera as MESSENGER was departing from the planet, and are among the first spacecraft views of that portion of Mercury’s surface. Most striking are the large pattern of rays that extend from north to south, almost along the entire face of Mercury. Amazing! This extensive ray system appears to emanate from a relatively young crater newly imaged by MESSENGER, providing a view of the planet distinctly unique from that obtained during MESSENGER’s first flyby.

2nd Update: (9:40 am CDT) More images!

Update: (8:50 am CDT) See 2nd image released below:


Mercury's limb.  Credit: NASA/Johns Hopkins University Applied Physics Laboratory/Carnegie Institution of Washington
Mercury's limb. Credit: NASA/Johns Hopkins University Applied Physics Laboratory/Carnegie Institution of Washington

Above is the 3rd image released from the second flyby, a spectacular close-up of Mercury, as seen by the MESSENGER as it approached the planet, at about 17,100 kilometers (10,600 miles) altitude. The features in the foreground, near the right side of the image, are close to the terminator, the line between the sunlit dayside and dark night side of the planet, so shadows are long and prominent. The MESSENGER team has only had a few hours to examine these intriguing features, and, currently, more images from the flyby are still streaming back to Earth.

Mercury close up. Credit: NASA/Johns Hopkins University Applied Physics Laboratory/Carnegie Institution of Washington
Mercury close up. Credit: NASA/Johns Hopkins University Applied Physics Laboratory/Carnegie Institution of Washington

Here’s the second image released from the flyby. This is a close-up image taken 9 minutes and 14 seconds after MESSENGER’s closest approach to Mercury, when the spacecraft was moving at 6.1 kilometers/second (3.8 miles/second). The largest impact feature at the top of the image is about 133 kilometers (83 miles) in diameter and is named Polygnotus. This area was imaged previously by Mariner 10.

More on the first image: Data from the flyby started coming back to Earth early this morning, at about 1:50 am EDT. This spectacular image is one of the first to be returned and was taken about 90 minutes after the spacecraft’s closest approach to Mercury. This young, extensively rayed crater, along with the prominent rayed crater to the southeast of Kuiper, near the limb of the planet, were both seen in Earth-based radar images of Mercury but not previously imaged by spacecraft. As the MESSENGER team is busy examining this newly obtained view that is only a few hours old, data from the flyby continue to stream down to Earth, including higher resolution close-up images of this previously unseen terrain.

MESSENGER completed the flyby on Oct. 6 at 4:40 am EDT.

We’ll add more images as they become available.

Source: MESSENGER Gallery

Extracting Water From the Moon With Basic Home Appliances

Two scientists have cooked up a way to get water and oxygen from the moon. And to test their idea, they used a basic kitchen microwave oven. “This is exploration,” said Dr. Bill Kaukler of the University of Alabama in Huntsville’s Center for Materials Research. Kaukler and Dr. Ed Etheridge of Marshall Space Flight Center have proposed using microwaves to draw water from below the lunar surface. To do this, microwaves would be “shot” at the moon, likely from an orbiting spacecraft. But to test their theory, Kaukler and Etheridge didn’t build an elaborate test site. They just put a plate of simulated lunar regolith in a microwave oven and “nuked” it for a few minutes.

Kaukler said they were inspired by the results of 1994’s Clementine mission which uncovered the possible existence of ice within some of the craters at the moon’s poles. This discovery was confirmed in early 1998 by NASA’s lunar prospector. Scientists believe the ice was brought to the moon the same way water was brought to Earth – by comets crashing into the surface.

“If you estimate, there would be billions of tons of water,” Ethridge said.

The surface is covered by regolith, or silicate rock that is the lunar version of top soil. It’s about two meters deep “and where you have silicates, you have oxygen,” said Kaukler. “That makes it worthwhile to extract, and, one of the beauties of this is we don’t have to dig.”

Digging could stir up the fine, gritty dust. The microscopic particles then could adversely affect the astronauts’ spacesuits and their equipment, he said.

To get to the water, microwaves would be shot into the regolith, “thawing” the ice to about minus-50 degrees Celsius. Water vapor would be drawn to the surface by the moon’s vacuum environment. The water vapor is then collected on a plate as ice and scraped off to be used as water for the astronauts. The hydrogen and oxygen can also be separated through electrolysis to use as fuel for a trip to Mars.

In their Marshall lab, the scientists used a microwave oven, a vacuum, water and a simulant to regolith to verify their findings.

“We put some water in the simulant and placed it inside the microwave,” Kaukler said. “Then, we used the vacuum to replicate the lunar atmosphere.

“We were able to get about 95 percent of the water back in about two minutes.”

Other uses of microwaves would be to “melt” the lunar surface. The process would help create dust-free landing and launch sites as well as smoother floors for structures and roads for traveling without kicking up dust.

“For surface site preparation, the microwaves would melt the top layer, glazing it, so it’s not all dust,” Ethridge said. “It would create a cobblestone effect.”

So if the moon had water, oxygen and useable real estate, it might be a financially viable place to colonize.

“Since we’re planning to go to the moon and Mars, the idea is to save weight (on the flight) and to extract the materials the astronauts would need – oxygen and water,” said Kaukler. “There have been studies that showed (getting the water) to be economically viable,” he said. “It could be the first commercial venture.”

Source: Huntsville Alabama Times

Galaxy Ramming Through Space Creates Fireballs

Fireball Galaxy. Credit: Subaru Telescope, National Astronomical Observatory of Japan (NAOJ)

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During routine observations of the Coma Cluster of galaxies using the Subaru Telescope in Hawaii, astronomers discovered a thread-like structure stretching from one of the galaxies. The astronomers determined this filament was about 260 thousand light years long, and spectral analysis of the filament suggested a younger age toward the outer edge of the filament. The filament also has many young stars surrounded by ionized gas that look like projectiles flying out from the galaxy. So what happened in this chaotic area of space? Astronomers determined a speeding galaxy rammed into the Coma Cluster, stripping gas from the galaxy and creating fireball-like projectiles.

Galaxies evolve over time, and astronomers do not yet understanding how they change in shape, size, and color. Galaxy Clusters, which are dense populations of galaxies, rich with hot intergalactic gas, accompanied by strong gravitational forces are some of the best locations to observe galactic evolution.

A team of researchers from the National Astronomical Observatory of Japan and the University of Tokyo used Suprime-cam on the Subaru Telescope to observe the Coma Cluster of galaxies. The Coma Cluster contains over 1,000 galaxies and is fairly close to Earth at about 300 million light years away.
During observations in 2006 and 2007, the astronomers saw the filament extending from Galaxy RB199 and several of the “fireballs.” Detailed study identified several bright knots connected by blue filamentary structures, and the knots are actually the clusters of young stars weighing 10 million times our Sun, contained in an area about 3000 to 6000 light years across. Because the knots are accompanied by ionized gas, active star formation is going on in the fireballs where usually far less star formation would be expected. The team noted that the size and the mass of the fireballs indicate they could develop into dwarf galaxies.

Closeups of four fireballs.  Subaru Telescope, National Astronomical Observatory of Japan (NAOJ)
Closeups of four fireballs. Subaru Telescope, National Astronomical Observatory of Japan (NAOJ)

Because the inside of the cluster is crowded with galaxies, they pass by each other and crash into each other. The team thought that the tidal forces during such encounters could strip gas or stars from the galaxies. They also postulated that as a galaxy falls into the center of the cluster the gravitational forces of the cluster could remove the gas and stars from that galaxy. Both scenarios are possible, however, the research team found that these mechanisms could hardly explain the characteristics of the fireballs. The team then realized that ram pressure stripping occurs when superheated gas (several tens of million Kelvin) in the cluster and the galaxies collide at high speeds. Previous X-ray observation shows the presence of large amounts of hot ionized gas in the middle of the Coma Cluster while RB199 crashes into the center at a speed of 1200 miles per second, causing strong friction with this hot gas. As such, the team concluded that the ram pressure has enough power to strip the gas from the galaxy AND create the fireballs.

While there are several reports indicating ram pressure stripping in nearby galaxy clusters, the identification of fireballs in this study is the first to demonstrate the stripped gas turns into stars while traveling through remote space far away from its source. Similar phenomena have been observed in galaxy clusters much further away at several billions light years, however, those distant cases were interpreted through witnessing the transitional phase of galaxies changing their morphology or colors as they fall into a cluster. The fireballs discovered by this team of Japanese astronomers provide the first sample of such structures in a nearby cluster. Principal investigator, Dr. Michitoshi Yoshida, said “the team is confident that our study of these phenomena leads to a better understanding of the gas stripping processes in galaxy clusters, and the effect of clusters on the evolution of individual galaxies”.

Source: Subaru Press release

Asteroid To Enter Earth’s Atmosphere Tonight (Oct. 6)

Looking for a little excitement tonight? An asteroid between 1-5 meters (3-15 feet) was discovered just hours ago at an Arizona observatory, and might provide a spectacular light show as it comes through Earth’s atmosphere. But don’t be alarmed – scientists predict it will be harmless and burn up before it reaches the ground. It is expected to be visible over eastern Africa, at approximately 2:46 a.m. Greenwich Mean Time (10:46 p.m. Eastern time ). There is no danger to people or property since the asteroid will not reach the ground. It will burn up in the upper atmosphere, well above aircraft heights. A brilliant fireball will be visible as a result. “We want to stress that this object is not a threat,” said Dr. Timothy Spahr, director of the International Astronomical Union’s Minor Planet Center. “We’re excited since this is the first time we have issued a prediction that an object will enter Earth’s atmosphere,” Spahr added. Odds are between 99.8 and 100 percent that the object will encounter Earth, according to calculations provided by Andrea Milani of the University of Pisa.

When a meteoroid (small asteroid) enters the atmosphere, it compresses the air in front of it. That compression heats the air, which in turn heats the object, causing it to glow and vaporize. Once it starts to glow, the object is called a meteor.

“A typical meteor comes from an object the size of a grain of sand,” explained Gareth Williams of the Minor Planet Center. “This meteor will be a real humdinger in comparison!”

The meteor is expected to be visible from eastern Africa as an extremely bright fireball traveling rapidly across the sky from northeast to southwest. The object is expected to enter the atmosphere over northern Sudan at a shallow angle.

“We’re eager for observations from astronomers near the asteroid’s approach path. We really hope that someone will manage to photograph it,” said Williams

Source: Center for Astrophysics Minor Planet Center

Image source

MESSENGER’s Second Flyby of Mercury: Awaiting Data

Mercury, prior to MESSENGER's closest approach. Credit: NASA/Johns Hopkins University Applied Physics Laboratory/Carnegie Institution of Washington

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This morning at 4:40 am EDT, the MESSENGER spacecraft passed only 200 kilometers (124 miles) above Mercury’s surface as it made its second flyby of the mission. Now, the spacecraft is speeding away from Mercury, continuing its science observations for about 20 hours following closest approach. This flyby should provide the first global perspective of Mercury, as, if all went well, we should have images in total covering about 95 percent of the planet. “This second flyby will show us a completely new area of Mercury’s surface, opposite from the side of the planet we saw during the first,” said Louise M. Prockter, scientist for the mission.

If you’re looking for images and data from the flyby here, sorry to disappoint, but data will be transmitted to Earth only after the completion of all science observations. So, for now, even the MESSENGER science team has to wait. But scientists are already eagerly exploring the optical navigation images acquired just prior to the flyby. Shown here is a Narrow Angle Camera (NAC) image from the eighth and final optical navigation image set, taken about 14.5 hours before the flyby’s closest approach.

As in the earlier seven sets, Mercury appears as a thin sunlit crescent. Though much of Mercury is in darkness in this image, the visible portion had never been seen by spacecraft before. This portion of Mercury’s surface was not viewed during any of Mariner 10’s three flybys or during MESSENGER’s first flyby earlier this year. The newly imaged terrain shows a wide range of geologic features, and scientists have marked them on the image. Near the northern limb of the planet, extensive smooth plains, possibly volcanic in origin, are identified. A nearby crater is the brightest feature visible in the image, suggesting a relatively young age. In the southern region, a large basin is seen with a smooth floor, likely also a product of volcanism. A large scarp that appears to cut through this basin may have formed as Mercury cooled and contracted.

For this flyby, MESSENGER was a “green” spacecraft – meaning it didn’t require the firing of its thrusters to fly precisely where the scientists wanted to make observations. Instead, engineers used a type of “solar sailing,” to guide the spacecraft. “There are no refueling station in interplanetary space, so we’re stuck with the amount of fuel we had at launch,” said principal investigator Sean Solomon during a press conference last week. “Some of that fuel is required to get us into orbit (of Mercury in 2011). By not using fuel on some smaller maneuvers makes the mission more reliable and saves propellant, and allows us to have it in our back pocket when we need it for contingencies.” This is the first spacecraft to use this technique with such precision. Planetary flyby has been described as a complex ‘threading of a needle,’ and the MESSENGER team is getting better and better. The spacecraft’s first flyby was in January 2008, and a third will take place on Sept. 29, 2009. Orbit insertion will be on March 18, 2011.

We’ll post the MESSENGER images from this second flyby as soon as they’re available.

Source: MESSENGER website

Astronaut Diary Survives Columbia Accident

Page from Ilan Ramon's diary. Credit: Israel Museum

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Pages from an astronaut’s diary survived the explosion of the space shuttle Columbia in 2003, and on Sunday, selected pages went on display at a museum in Jerusalem. Israeli astronaut Ilan Ramon kept a personal diary during his time in orbit, and portions of it were found about two months after Columbia broke apart on February 1, 2003 while returning to Earth following the STS-107 mission. “Today was the first day that I felt that I am truly living in space. I have become a man who lives and works in space,” Ramon wrote in an entry on his sixth day in orbit.

Astronaut Ilan Ramon departs for his flight aboard Columbia. Credit: Chris O’Meara/Associated Press
Astronaut Ilan Ramon departs for his flight aboard Columbia. Credit: Chris O’Meara/Associated Press

37 pages survived the extreme heat of the explosion, as well as the 60 km (37-mile) fall to earth and several days of wet weather before they were found. “It’s almost a miracle that it survived — it’s incredible,” Israel Museum curator Yigal Zalmona said. “There is no rational explanation for how it was recovered when most of the shuttle was not.”

 Diary pages as they were found.  Credit:  Israel Ministry of Public Security
Diary pages as they were found. Credit: Israel Ministry of Public Security

The pages were found in a field just outside of Palestine, Texas. On some pages, the writing was washed out, other pages were tattered and torn, pocked with irregular holes as if debris had ripped through them. Pieces were twisted into tightly crumpled wads smaller than a fingernail. Some pages were stuck tightly together and had to be delicately pried apart.

Once it had been verified that the pages were relevant to the Columbia debris, the papers were collected and given to Colonel Ramon’s family. Ramon’s wife, Rona, decided to bring the papers to Israel for deciphering the damaged writing and, ultimately, conservation of the torn and tattered pages.

Most of the pages contain personal information which Mrs. Ramon did not wish to make public. “We agreed to do the restoration completely respecting the family’s privacy and the sensitivity about how intimate the document is,” museum director James Snyder said.

The diary took about a year to restore, Zalmona said, and it took police scientists about four more years to decipher the pages. About 80 percent of the text has been deciphered, and the rest remains unreadable, he said.

Page of Ramon's diary that was restored using Photoshop™ and Image-Pro Plus™
Page of Ramon's diary that was restored using Photoshop™ and Image-Pro Plus™

Two pages will be displayed at the museum. One contains notes written by Ramon, and the other is a copy of the Kiddush prayer, a blessing over wine that Jews recite on the Sabbath. Zalmona said Ramon copied the prayer into his diary so he could recite it on the space shuttle and have the blessing broadcast to Earth.

There is no information available as to where the pages of the diary were situated during reentry, for example if they were in a pocket of Ramon’s spacesuit or in a padded, heat resistant container or simply held under his leg, as one astronaut suggested.

The diary provides no indication Ramon knew anything about potential problems on the shuttle. Columbia’s wing was gashed by a chunk of fuel tank foam insulation at liftoff and broke up just 16 minutes before it was scheduled to land at the Kennedy Space Center in Florida. All seven astronauts on board were killed.

The diary is being displayed as part of a larger exhibit of famous documents from Israel’s history, held to mark the country’s 60th anniversary this year.

Sources: Israel Ministry of Public Security, AP article

Where Are All the Kuiper Belt Objects?

Occultations of KBOs. Credit: TAOS

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A group of astronomers spent two years photographing portions of the sky to look for small chunks of rock and ice orbiting beyond Neptune, in the Kuiper Belt region of our Solar System. The survey targeted Kuiper Belt objects (KBOs) with sizes between 2 miles (3 km) and 17 miles (28 km). The researchers are surprised, as well as a little disappointed with the results. They came up empty. Nada. Not a single KBO within those parameters was spotted. But these researchers from the Taiwanese-American Occultation Survey (TAOS) are ‘glass-half-full’ types, and say that defeat can provide as much information as a successful search, so they are making the most of their data. What this means is that there are less KBOs out there than previously thought.

Since the KBO’s this group searched for are too small to see directly, the survey watched for stars to dim as KBOs passed in front of and occulted them. After accumulating more than 200 hours of data watching for stellar flickers lasting a second or less, TAOS did not spot any occultations.

Here’s a movie that illustrates their search.

The Kuiper Belt contains objects in a range of sizes: a few very large ones (like the dwarf planets Pluto, Eris, Makemake and Haumea) and many more smaller ones. The commonness of a given size tells us information about the history of planet formation and dynamics. In particular, the size distribution of KBOs reflects a history of agglomeration, in which colliding objects tended to stick together, followed by destructive collisions, where collisional velocities were high enough to shatter the rocks involved.

Astronomers questioned whether they would find more and more objects as sizes decreased further, or whether the distribution leveled out. The fact that no occultations were seen sets a stringent upper limit on the number density of KBOs between 2 and 17 miles in diameter. The outer solar system, therefore, appears not as crowded as some theories suggest, perhaps because small KBOs have already stuck together to form larger bodies or frequent collisions have ground down small KBOs into even smaller bits below the threshold of the survey.

The paper announcing this result, co-authored by CfA director Charles Alcock, was published in the October 1 issue of the Astrophysical Journal Letters.

Sources: TAOS, CfA

Did Our Solar System Start With a “Little Bang?”

Artist illustration of supernova. Credit: NASA

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What prompted the formation of our little corner of the universe – our sun and planetary system? For several decades, scientists have thought that the Solar System formed as a result of a shock wave from an exploding star—a supernova—that triggered the collapse of a dense, dusty gas cloud, which then contracted to form the Sun and the planets. But detailed models of this formation process have only worked under the simplifying assumption that the temperatures during the violent events remained constant. That, of course, is very unlikely. But now, astrophysicists at the Carnegie Institution’s Department of Terrestrial Magnetism (DTM) have shown for the first time that a supernova could indeed have triggered the Solar System’s formation under the more likely conditions of rapid heating and cooling. So have these new findings resolved this long-standing debate?

“We’ve had chemical evidence from meteorites that points to a supernova triggering our Solar System’s formation since the 1970s,” remarked lead author, Carnegie’s Alan Boss. “But the devil has been in the details. Until this study, scientists have not been able to work out a self-consistent scenario, where collapse is triggered at the same time that newly created isotopes from the supernova are injected into the collapsing cloud.”

Short-lived radioactive isotopes—versions of elements with the same number of protons, but a different number of neutrons—found in very old meteorites decay on time scales of millions of years and turn into different (so-called daughter) elements. Finding the daughter elements in primitive meteorites implies that the parent short-lived radioisotopes must have been created only a million or so years before the meteorites themselves were formed. “One of these parent isotopes, iron-60, can be made in significant amounts only in the potent nuclear furnaces of massive or evolved stars,” explained Boss. “Iron-60 decays into nickel-60, and nickel-60 has been found in primitive meteorites. So we’ve known where and when the parent isotope was made, but not how it got here.”

Cross-sectional view of one-half of a solar-mass target cloud being struck by a supernova shock front that is traveling downward. Credit:  Carnigie Institution for Science
Cross-sectional view of one-half of a solar-mass target cloud being struck by a supernova shock front that is traveling downward. Credit: Carnigie Institution for Science

Previous models by Boss and former DTM Fellow Prudence Foster showed that the isotopes could be deposited into a pre-solar cloud if a shock wave from a supernova explosion slowed to 6 to 25 miles per second and the wave and cloud had a constant temperature of -440 °F (10 K). “Those models didn’t work if the material was heated by compression and cooled by radiation, and this conundrum has left serious doubts in the community about whether a supernova shock started these events over four billion years ago or not,” remarked Harri Vanhala, who found the negative result in his Ph.D. thesis work at the Harvard-Smithsonian Center for Astrophysics in 1997.

Using an adaptive mesh refinement hydrodynamics code, FLASH2.5, designed to handle shock fronts, as well as an improved cooling law, the Carnegie researchers considered several different situations. In all of the models, the shock front struck a pre-solar cloud with the mass of our Sun, consisting of dust, water, carbon monoxide, and molecular hydrogen, reaching temperatures as high as 1,340°F (1000 K). In the absence of cooling, the cloud could not collapse. However, with the new cooling law, they found that after 100,000 years the pre-solar cloud was 1,000 times denser than before, and that heat from the shock front was rapidly lost, resulting in only a thin layer with temperatures close to 1,340°F (1000 K). After 160,000 years, the cloud center had collapsed to become a million times denser, forming the protosun. The researchers found that isotopes from the shock front were mixed into the protosun in a manner consistent with their origin in a supernova.

“This is the first time a detailed model for a supernova triggering the formation of our solar system has been shown to work,” said Boss. “We started with a Little Bang 9 billion years after the Big Bang.”

Source: Carnegie Institution for Science