New Research Sheds Light On Black Hole Growth

The black hole that has grown the most can be found in the Sombrero galaxy . The researchers estimate that this black hole has been swallowing the equivalent of one Sun every twenty years and is now over 500 million times as heavy as the Sun. ESO Public Image Release

In a new study led by University of Central Lancashire astronomer Dr. Victor Debattista, researchers are looking into the mystery of how black holes grow and evolve. For many years, astronomers surmised black holes took on mass when their host galaxies merged, but now new modeling techniques show that black holes in spiral galaxies are forced to take on mass.

“Recent Hubble Space Telescope (HST) observations have revealed that a majority of active galactic nuclei (AGN) are resident in isolated disk galaxies, contrary to the usual expectation that AGN are triggered by mergers.” says Debattista. “Here we develop a new test of the cosmic evolution of supermassive black holes (SMBHs) in disk galaxies by considering the local population of SMBHs. We show that substantial SMBH growth in spiral galaxies is required as disks assemble.”

Weighing in a range of one million to one billion times that of the Sun, the black holes located at the core of most galaxies would appear to be gaining at much quicker rates than expected. These are not just exceptions – more like rules. Even the Milky Way’s quiescent black hole might be gaining as much mass as the Sun every 3,000 years. Past observations have shown growth during collision events, when huge amounts of gas around the black hole become intensely hot and shine as an active galactic nucleus. This is a process which can be spotted as far back as the first formations in our Universe. However, these new simulations are giving insight into large scale growth without the need for violence.

“The X-ray-selected sample of moderate luminosity AGN consists of more than 50% disk galaxies, with ongoing mergers evident no more frequently than in nonactive galaxies.” explains the research team. “Some show that even heavily obscured quasars are hosted largely by disks, not by mergers. Studies of star-formation using Herschel find that the specific star formation rates of X-ray selected AGN hosts are no different from those of inactive galaxies, also indicating that AGN hosts are not undergoing fundamentally different behaviors”

These modeling techniques, combined with current observations done with the Hubble Space Telescope, give credence to the theory that black holes can gain significant mass even in “quiet” spiral galaxies. As a matter of fact, there is a strong possibility that AGNs present in some spiral galaxies may even outnumber galaxy mergers. To make this concept even more exciting, astronomers are anticipating an event later this year in our own galaxy – an event where a gas cloud near the Milky Way’s nucleus will encounter our own central black hole. According to predictions, our black hole may take on as much as 15 Earth masses in a period of 10 years from this cloud.

This concept of black hole growth isn’t entirely new, though. According to other research done with the Hubble Space Telescope and led by Dr. Stelios Kazantzidis of Ohio State University and Professor Frank C. van den Bosch of Yale University, they had previously pinpointed mass properties of black holes – making size predictions which utilized the speed of stars residing in the galaxies. In this instance, the team disproved previous assumptions that black holes were unable to grow while the host galaxy grew. Their comparison of spiral and elliptical galaxies “found there is no mismatch between how big their black holes are.” This means black holes would be gaining in mass – growing along at the same rate as the galaxy itself.

“These simulations show that it is no longer possible to argue that black holes in spiral galaxies do not grow efficiently. ” comments Debattista on this new research. ” Our simulations will allow us to refine our understanding of how black holes grew in different types of galaxies.”

See an Asteroid’s-Eye-View of Friday’s Close Approach Between 2012 DA14 and Earth

Painting of Asteroid 2012 DA14. © David A. Hardy/www.astroart.org

If you haven’t heard yet, this Friday, February 15, 2013 will be a close flyby of an asteroid named 2012 DA14. It’s turning out to be a highly anticipated event, as it will pass just 27,630 kilometers (17,168 miles) from the surface of the Earth, well within the range of many Earth-orbiting satellites. If you could watch the action from the vantage point of space, what would this flyby look like? Analytical Graphics, Inc., a company that creates modeling and analysis software for space, defense and other areas, has put together an animation which includes the asteroid’s trajectory as it approaches Earth, a closeup of the asteroid during its closest approach, a highlighted portion of Earth orbit that it is expected to pass through, and other interesting data.

The video above also provides a view of the asteroid’s pass by Earth below the geosynchronous orbit belt, how it will crossing the equatorial plane from South to North, a size comparison, and how the Earth/Moon will perturbs the asteroid’s orbit.

This asteroid is about 50 meters (164 feet) in size. Asteroid experts, including NASA’s Don Yeomans has , said there is no possibility of this asteroid hitting Earth, and they have also effectively ruled out the chance of any satellites getting hit.

The asteroid will not be bright enough to be visible with the unaided eye, but will be visible to backyard astronomers with good telescopes. The timing of the pass will allow viewers in eastern Europe, Africa, Australia and New Zealand to have the best chance of seeing this asteroid.

See our complete guide on how to see Asteroid 2012 DA14.

This asteroid must be stirring the imaginations of many; already renowned and award-winning space artist David A. Hardy has created a painting of his impression of 2012 DA14’s approach to Earth:

Thanks to Hardy for allowing us to post his lovely artwork. You can see more at his website, and he did an interview with us last year, which you can read here.

Animation courtesy of (AGI).

Cosmic Ink-blot Test: Can You See the Gecko in Space?

This image from the Wide Field Imager on the MPG/ESO 2.2-metre telescope at ESO’s La Silla Observatory in Chile, shows the bright star cluster NGC 6520 and its neighbour, the strangely shaped dark cloud Barnard 86. This cosmic pair is set against millions of glowing stars from the brightest part of the Milky Way — a region so dense with stars that barely any dark sky is seen across the picture.
Millions of glowing stars from the brightest part of the Milky Way — a region so dense with stars that barely any dark sky is seen across the picture. Credit: ESO

A small, isolated dark nebula known as a Bok globule was described as “a drop of ink on the luminous sky” by its discoverer, astronomer Edward Emerson Barnard. Through a small telescope, the object seen here, Barnard 86, does appear as though someone may have dropped a blob of dark ink on the telescope lens. Or perhaps it appears as a spot where there are no stars, or a window into a patch of distant, clearer sky. However, this object is actually in the foreground of the star field — a cold, dark, dense cloud made up of small dust grains that block starlight and make the region appear opaque. It is thought to have formed from the remnants of a molecular cloud that collapsed to form the nearby star cluster NGC 6520, seen just to the left of Barnard 86 in this image.

Some say Barnard 86 looks like a gecko … can you see the resemblance?

This image was taken with the Wide Field Imager on the MPG/ESO 2.2-meter telescope at ESO’s La Silla Observatory in Chile. This cosmic pair is set against millions of glowing stars from the brightest part of the Milky Way — a region so dense with stars that barely any dark sky is seen across the picture.

It is located in the constellation of Sagittarius in one of the richest star fields in the whole sky, the Large Sagittarius Star Cloud. The huge number of stars that light up this region dramatically emphasize the blackness of dark clouds like Barnard 86.

For more info on this image, see this ESO page.

A Cosmic Rose for Your Spacey Valentine

A beautiful planetary nebula, Sh2-174. Credit: T.A. Rector (University of Alaska Anchorage) and H. Schweiker (WIYN and NOAO/AURA/NSF)

We space-nerds like to express our amorous feelings, just like the rest of the population (although admittedly some of need more help/prodding in this area than others). And so just in time for Valentine’s Day comes this new image of a planetary nebula, which looks like a rose — or even a tulip – to share with your very spacey valentine.

The name of this planetary nebula, however, is not so romantic: Sh2-174. We need some suggestions for a better name!

And the way this object was created is not so romantic, either, as planetary nebulae come about in violent events. Sh2-174 was created when a low-mass star blew off its outer layers at the end of its life. The core of the star remains and is called a white dwarf. Usually the white dwarf can be found very near the center of the planetary nebula. But in the case of Sh2-174 it is off to the right. (It is the very blue star near the center of the blue gas). This asymmetry is due to the planetary nebula’s interaction with the interstellar medium that surrounds it.

This image was obtained with the wide-field view of the National Optical Astronomy Observatory (NOAO) Mosaic 1 camera on the Mayall 4-meter telescope at Kitt Peak National Observatory. Travis Rector from the University of Alaska Anchorage made the observations for this image, taken through four different filters which are assigned colors that approximate what the human eye can see: B (blue), I (orange), Hydrogen-alpha (red) and Oxygen [OIII] (blue) filters. In this image, North is up, East is to the left.

Source: NOAO

10 Amazing 3-D Views from the Mars Reconnaissance Orbiter

The Dunes of 'Inca City.' Credit: NASA/JPL/University of Arizona.

These pictures require you to grab the 3-D glasses you have handy by your desk (if you don’t have a pair, here’s some great options for buying some) and get a “you-are-there” experience from the HiRISE camera on the Mars Reconnaissance Orbiter. Here, you can virtually tumble down crater walls, hover over steep cliffs, and see how layered bedrock appears from above.

Our lead image is of an area referred to as “Inca City,” the informal name given by Mariner 9 scientists in 1972 to a set of intersecting, rectilinear ridges, which some people thought looked like structures or streets. Even back then scientists thought they might be dunes, but that didn’t keep people from going off the deep end about this region. But the power of HiRISE has revealed these truly are dunes, and in this image you can see some of the seasonal processes as the region goes from winter to spring. As the carbon dioxide frost and ice on the dunes warms, small areas warm and sublimate (turn from solid to gas) faster, creating a speckled surface.

Enjoy more 3-D views below. All images link directly to the HiRISE site where you can see other versions and get more info about each image. See all the HiRISE anaglyphs that are available here.

Fresh 4-Kilometer Rayed Crater Northeast of Chimbote Crater. Credit: NASA/JPL/University of Arizona.
Fresh 4-Kilometer Rayed Crater Northeast of Chimbote Crater. Credit: NASA/JPL/University of Arizona.
Cliff with Columnar Jointing. Credit: NASA/JPL/University of Arizona.
Cliff with Columnar Jointing. Credit: NASA/JPL/University of Arizona.
Central Uplift of a Large Impact Crater. Credit: NASA/JPL/University of Arizona.
Central Uplift of a Large Impact Crater. Credit: NASA/JPL/University of Arizona.
Buttes and craters: Compositional Diversity in Northern Hellas Region. Credit: NASA/JPL/University of Arizona.
Buttes and craters: Compositional Diversity in Northern Hellas Region. Credit: NASA/JPL/University of Arizona.
Well-Preserved 4-Kilometer impact Crater. Credit: NASA/JPL/University of Arizona.
Well-Preserved 4-Kilometer impact Crater. Credit: NASA/JPL/University of Arizona.
Flow Boundary in Elysium Planitia. Credit: NASA/JPL/University of Arizona.
Flow Boundary in Elysium Planitia. Credit: NASA/JPL/University of Arizona.
A fissure on Mars named Cerberus Fossae. Credit: NASA/JPL/University of Arizona.
A fissure on Mars named Cerberus Fossae. Credit: NASA/JPL/University of Arizona.
Possible Gullies in Graben. Credit: NASA/JPL/University of Arizona.
Possible Gullies in Graben. Credit: NASA/JPL/University of Arizona.
Layered Bedrock on Crater Floor. Credit: NASA/JPL/University of Arizona.
Layered Bedrock on Crater Floor. Credit: NASA/JPL/University of Arizona.

Carnival of Space #288

This week’s Carnival of Space is hosted by our pal Ray Sanders at his Dear Astronomer website!

Click here to read Carnival of Space #288.

And if you’re interested in looking back, here’s an archive to all the past Carnivals of Space. If you’ve got a space-related blog, you should really join the carnival. Just email an entry to [email protected], and the next host will link to it. It will help get awareness out there about your writing, help you meet others in the space community – and community is what blogging is all about. And if you really want to help out, sign up to be a host. Send an email to the above address.

45 meter Asteroid to Skirt Very Near Earth on Feb 15

Asteroid 2012 DA14 Zooms just 17,200 miles above Earth on Feb. 13 in this artist’s concept. Credit; NASA

Our home planet is due for a record setting space encounter on Friday (Feb. 15) of this week, when a space rock roughly half a football field wide skirts very close by Earth at break neck speed and well inside the plethora of hugely expensive communications and weather satellites that ring around us in geosynchronous orbit.

“There is no possibility of an Earth impact” by the Near Earth Asteroid (NEO) known as 2012 DA 14, said Don Yeomans, NASA’s foremost asteroid expert at a media briefing. Well that’s good news for us – but a little late for the dinosaurs.

At its closest approach in less than 4 days, the 45 meter (150 feet) wide Asteroid 2012 DA14 will zoom by within an altitude of 27,700 kilometers (17,200 miles). That is some 8000 km (5000 miles) inside the ring of geosynchronous satellites, but far above most Earth orbiting satellites, including the 6 person crew currently working aboard the International Space Station.

Although the likelihood of a satellite collision is extremely remote, NASA is actively working with satellite providers to inform them of the space rocks path.

The razor thin close shave takes place at about 2:24 p.m. EST (11:24 a.m. PST and 1924 UTC) as the asteroid passes swiftly by at a speed of about 7.8 kilometers per second (17,400 MPH)- or about 8 times the speed of a rifle bullet. For some perspective, it will be only about 1/13th of the distance to the moon at its closest.

“Asteroid 2012 DA14 will make a very close Earth approach, traveling rapidly from South to North and be moving at about two full moons per minute,” said Yeomans, who manages NASA’s Near-Earth Object Program Office at the Jet Propulsion Laboratory in Pasadena, Calif. “That’s very fast for a celestial object.”

Diagram depicting the passage of asteroid 2012 DA14 through the Earth-moon system on Feb. 15, 2013. Credit: NASA/JPL-Caltech
Diagram depicting the passage of asteroid 2012 DA14 through the Earth-moon system on Feb. 15, 2013. Credit: NASA/JPL-Caltech

No known asteroid has ever passed so near to Earth.

“This is a record predicted close approach for a known object this size,” stated Yeomans. “Such close flybys happen every 40 years on average. An actual Earth collision would happen about every 1200 years.”

Read also: Asteroid 2012 DA14: Observing Prospects and How to See It

Yeomans said that if an asteroid the size of 2012 DA14 fell to Earth, the impact effect would be similar to the 1908 Tunguska event in Siberia. That was an air blast event that leveled trees over an area greater than about 800 square miles.

So the local effect on human cities for example of a 50 meter wide asteroid impact would be deadly and utterly devastating. But it would not be catastrophic to all life on Earth. Nevertheless, at this moment, Earth has no defenses against asteroids other than talk.

By comparison, the K-T event that caused the mass extinction of the dinosaurs some 65 million years ago was caused by an asteroid about 10 km (6 mi) in diameter. About 2/3 of all species went extinct. If 2012 DA14 impacted Earth the force would be equivalent to about 2.4 megatons of energy (2.4 million tons of TNT), said Yeomans.

Artists concept of meteoroide impact event
Artists concept of meteoroide impact event

There is no danger to the ISS crew and apparently they won’t have any chance to observe it.

“The ISS is not positioned right for observations,” Lindley Johnson, program executive, Near Earth Object Observations Program, NASA Headquarters, Washington, told Universe Today.

“No NASA space-based assets will be making measurements,” Lindley told me. “The asteroid is moving to fast.”

However, radar astronomers do plan to take images around eight hours after the flyby using the Goldstone antenna in California’s Mojave Desert, which is part of NASA’s Deep Space Network.

Some skilful and knowledgeable Earthlings might have a chance to see the asteroid hurtling by with binoculars or a small telescope.

“The asteroid will be observable in the dark sky in Eastern Europe, Asia and Australia, achieving about 7.5 magnitude, somewhat fainter than naked eye visibility,” explained Yeomans. “Closest approach will be over Indonesia.”

Astronomers at the La Sagra Sky Survey program in southern Spain discovered the asteroid in February 2012 just after its last Earth flyby, at a fairly distant 7 Earth-Moon distances. They reported the finding to the Minor Planet Center.

NASA’s NEO group and collaborators in Pisa, Italy then use such data to predict future flight paths and look into past trajectories as well.

Yeomans said that the Feb 15 flyby will be the closest for the next 100 years and its orbit will be perturbed so that it comes back less frequently – changing its orbital class from Apollo to Aten.

Due to its small size and recent discovery, not much is known about the composition of 2012 DA14. It might be silicate rock.

Small space rocks hit Earth on a daily basis amounting to about 100 tons. Car sized rocks hit weekly.

Stay Alert !

Ken Kremer

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Scientist Explains the Weird Shiny Thing on Mars

A zoomed-in view of the shiny protuberance. Credit: NASA/JPL-Caltech/Malin Space Science Systems. Image via 2di7 & titanio44 on Flickr.

As we reported last week, images from the Curiosity rover showed what looked like a piece of shiny metal sticking out from a rock. Some of our readers suggested that it might be a handle or knob of some kind. It’s a knob, yes, says Ronald Sletten from the Mars Science Laboratory team, but a completely natural formation. Sletten, from the University of Washington, explained that, not surprisingly, it is actually a part of the rock that is different — harder and more resistant to erosion — than the rest of the rock it’s embedded in.

On Earth, as on Mars, “often you can see knobs or projections on surfaces eroded by the wind, particularly when a harder, less erodible rock is on top,” Sletten said, via an email to Universe Today from the Jet Propulsion Laboratory media relations office. “The rock on top of the projection is likely more resistant to wind erosion and protects the underlying rock from being eroded.”

As far as why it appears shiny, Sletten said, “The shiny surface suggests that this rock has a fine grain and is relatively hard. Hard, fine grained rocks can be polished by the wind to form very smooth surfaces.”

It also may be shiny because it is wind-blasted and therefore dust-free, Sletten said, “while the surfaces not directly being eroded by wind may have a fine layer of reddish dust or rock-weathering rind. The sandblasted surfaces may reveal the inherent rock color and texture.”

He added that the object is an interesting study in how wind and the natural elements cause erosion and other effects on various types of rocks.

A closeup of the shiny protuberance. Credit: NASA/JPL/Malin Space Science Systems.
A closeup of the shiny protuberance. Credit: NASA/JPL/Malin Space Science Systems.

In looking at a zoomed-in close-up of the “knob” or protuberance from the rock, Sletten said, “This knob has a different type of rock on the end of the projection. This rock may vary in composition or the rock grain size may be smaller.”

A shiny-looking Martian rock is visible in this image taken by NASA's Mars rover Curiosity's Mast Camera (Mastcam) during the mission's 173rd Martian day, or sol (Jan. 30, 2013). Image Credit: NASA/JPL-Caltech/Malin Space Science Systems.
A shiny-looking Martian rock is visible in this image taken by NASA’s Mars rover Curiosity’s Mast Camera (Mastcam) during the mission’s 173rd Martian day, or sol (Jan. 30, 2013). Image Credit: NASA/JPL-Caltech/Malin Space Science Systems.

Because of the winds on Mars, there is quite a bit of erosion of rock, visible in the image above, as well as in many images from all the Mars rovers and landers. These type of surfaces are called “ventifacted” — wind-eroded surfaces caused by many fine particles of dust or sand impacting the surface over time. Areas of rocks may appear sculpted, as softer parts erode more easily or they may reflect small scale wind patterns, Sletten said.

In some ways, he added, it’s a lot like what happens to rocks in Antarctica. See the annotated images he provided below:

Annotated image supplied by Ronald Sletten, MSL science team.
Annotated image supplied by Ronald Sletten, MSL science team.
Annotated image supplied by Ronald Sletten, MSL science team.
Annotated image supplied by Ronald Sletten, MSL science team.

So, this weird shiny thing on Mars is nothing too out of the ordinary — not a door handle, hood ornament or not even Richard Hoagland’s bicycle, as was suggested by readers on our previous article.

But for one more look, here’s the 3-D version(make sure you use the red-green 3-D glasses):

3-D anaglyph from the right and left Mastcam from Curiosity showing the metal-looking protuberance. Credit: NASA/JPL/Caltech/Malin Space Science Systems. Anaglyph by by 2di7 & titanio44 on Flickr.
3-D anaglyph from the right and left Mastcam from Curiosity showing the metal-looking protuberance. Credit: NASA/JPL/Caltech/Malin Space Science Systems. Anaglyph by by 2di7 & titanio44 on Flickr.

The original raw image from the Curiosity rover can be seen here, and our thanks to Elisabetta Bonora, an image editing enthusiast from Italy, who originally pointed this image out to us.

Stunning Compilation of the Solar Dynamic Observatory’s Observations

Magnificent eruption from the Sun, shown in 304 and 171 Angstrom wavelength light, on August 31, 2012. Credit: NASA

Three years ago today, (February 11, 2010) I was standing at Kennedy Space Center watching the launch of the Solar Dynamics Observatory. The launch was spectacular, and included a unique effect as the Atlas rocket flew close to a sundog just as the spacecraft reached Max-Q, creating a ripple effect around the spacecraft. And so, SDO started off with a bang and she’s been producing incredible data ever since. The folks at Goddard Spaceflight Center’s Scientific Visualiation Studio have put together a highlight reel for the third year of SDO operations. You’ll see morphing sunspots, fountains of solar plasma, sun-grazing comets and more. Throughout its mission, SDO has not only studied the Sun, but also opened up several new, unexpected doors to scientific inquiry. Enjoy this “greatest hits” video of SDO’s third year.

Freaky Fast Delivery: Progress Blasts Off, Docks at ISS Hours Later

Progress 50 approaching the International Space Station on Feb. 11, 2013. Via NASA TV.

The Progress 50 resupply ship has now arrived at the International Space Station, just hours after it launched from the Baikonur Cosmodrome in Kazakhstan. Launch took place at 9:41 a.m. EST, (14:40 UTC) today (February 11, 2013) and it took only a four-orbit journey to rendezvous with the ISS, docking at 3:34 pm EST (20:35 UTC).

“Progress 50 just docked to our Space Station!” Tweeted astronaut Chris Hadfield (@Cmdr_Hadfield) “I was right at the hatch, it made a quick sliding scraping noise & then a solid thud. Success!”

This is third successful execution of the new, modified launch and docking profile for the Russion Progress ships, and its success is paving the way for its first use on a manned mission – possibly as early as March 2013 for Soyuz TMA-08, Roscosmos said via Facebook. Russian cosmonaut Gennady Padalka has been quoted as saying it is every cosmonaut’s dream to only have a 6-hour flight in the cramped Soyuz.

Watch the launch and docking video below:


Normally, Progress supply ships –and manned Soyuz capsules — are launched on trajectories that require about two days, or 34 orbits, to reach the ISS. The new fast-track trajectory has the rocket launching shortly after the ISS passes overhead — today, the space station was just 1,400 kilometers (870 miles) downrange from the launch site at the time of liftoff. Then additional firings of the Progress engines early in its mission expedites the time required for a Russian vehicle to reach the complex.

That also give the ISS crew the chance to actually see the launch from orbit. Today, NASA-TV commentator Kyle Herring said that ISS commander Kevin Ford reported he was able to see the first stage separation, which occurred about two minutes after launch. Herring said the cameras on the International Space Station were pointed to try and observe the launch. We’ll add any images here, if the cameras were able to capture anything.

Progress 50 is carrying 2.9 tons of supplies and equipment, including 800 kg (1,764 pounds) of space station propellant, 50 kg (110 lbs)of oxygen and air, 420 kg (926lbs) of water and 1,360 kg (3,000 lbs) of spare parts, science gear and other dry cargo. Right now, this Progress is scheduled to remain docked at the ISS until late April. The previous Progress cargo ship undocked from the Pirs module of the International Space Station at 13:15 GMT on Saturday February 9 and re-entered Earth’s atmosphere over the Pacific Ocean, burning up during re-entry.

Earlier this month, NASA’s Space Station Program Manager Mike Suffradini said the space station partners have tentatively agreed to try a the fast-track trajectory with a manned mission “at least once or twice to show we have the capability in case we need to get to ISS quick for any reason.”

He added that the decision to fly like this long-term is still to be determined.

This article has been updated.