President Signs NASA 2010 Authorization Act

President Obama signs NASA Authorization Act of 2010. Image: NASA, Pete Souza

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President Barack Obama signed the NASA 2010 Authorization Act into law Monday, giving the go-ahead for $58.4 billion be spent on NASA programs over the course of the next three years. However, where and how that money will be spent – has yet to be decided. For that the space agency has to wait for appropriations to wrangle out the specifics in the upcoming legislative sessions. But this much is known for certain: there will be an additional shuttle flight added, the life of the International Space Station will be extended to 2020 – and perhaps beyond, and the development of heavy-lift rocket will start as early as 2011.

“We will foster a growing commercial space transportation industry that will allow NASA to focus our efforts on executing direction in the act to start work on a heavy-lift architecture to take astronauts beyond low-Earth orbit and to develop a multipurpose crew vehicle for use with our new space launch systems,” said NASA Administrator Charles Bolden when he thanked the president for signing the bill. “Also, we will continue to invest in green aviation and other technologies that make air travel safer and more efficient.”

This particular bill was one of two that were vying for dominance in the House and Senate over the past weeks. After the NASA FY 2011 Budget was announced it was clear that many were unhappy with the direction this budget entailed and wanted a balanced compromise. Senator Bill Nelson (D-FL) led the charge to see that while commercial firms were included in the new space mix, decades of skill and experience of workers at Kennedy Space Center and other centers and contractors are not lost in this transition period.

“We now have a way forward for NASA,” Nelson said during a press briefing today. “Now with the signing of this legislation into law, NASA has a blueprint, NASA has a roadmap. The goal is not the moon. We were there 40 years ago. The goal is Mars by a flexible path. The president has stated that goal and this legislation which he is signing into law will now set us on that course.”

Nelson has been working closely with U.S. Rep Suzanne Kosmas, whose district includes NASA’s Kennedy Space Center (KSC). Both of the lawmakers took time to acknowledge that this bill was a bipartisan effort that included concerned members from both political parties.

Kosmas had been highly critical of the president’s plans for NASA, stating that the changes he had planned would turn the space flight ‘gap’ into an “abyss.” Since that time numerous lawmakers including Kosmas have worked to see that NASA’s way forward contained elements from both established space companies as well as new start ups – the so-called ‘NewSpace’ groups.

Under this bill, the development of a new heavy-lift rocket would start as early as next year. This is a far cry from the 2015 review date for heavy-lifts that Obama had called for. This means that the space flight gap that NASA is facing potentially stands to be far less expansive than under the president’s original plans. Nelson stated that he views this and other elements of the bill as ensuring that NASA will have a very bright future.

The New Blue Marble

Permian Extinction
A new NASA image of Earth, by Robert Simmon and Marit Jentoft-Nilsen, based on MODIS data.

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Despite recent news of potential habitable exoplanets and amazing images of Mars and the Saturn system returned from visiting spacecraft, the ol’ home planet is still about the most gorgeous-looking planetary body out there. We first saw it as a whole “blue marble” when the Apollo astronauts sent back pictures while circling the Moon, and it has been said that the original “Blue Marble” image taken by the Apollo 17 crew has been one of the most viewed and most influential images ever. But truth be told, that “Blue Marble” really wasn’t all that blue (see the original below). However, this new look at the home world shows how prevalent water really is. This composite image is based largely on observations from the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Terra satellite.

It sure is pretty.

According to the NASA Earth Observatory website, Earth’s water content is about 1.39 billion cubic kilometers (331 million cubic miles), with the bulk of it, about 96.5%, being in the global oceans. As for the rest, approximately 1.7% is stored in the polar icecaps, glaciers, and permanent snow, and another 1.7% is stored in groundwater, lakes, rivers, streams, and soil. Only a thousandth of 1% of the water on Earth exists as water vapor in the atmosphere.

Here’s the original “Blue Marble,” the view of the Earth as seen by the Apollo 17 crew traveling toward the moon. This translunar coast photograph extends from the Mediterranean Sea area to the Antarctica south polar ice cap. This is the first time the Apollo trajectory made it possible to photograph the south polar ice cap. Almost the entire coastline of Africa is clearly visible. The Arabian Peninsula can be seen at the northeastern edge of Africa. The large island off the coast of Africa is Madagascar. The Asian mainland is on the horizon toward the northeast.

The original 'Blue Marble' taken by Apollo 17. Credit: NASA

For larger versions of the top image, see NASA Earth Observatory’s website, and this link for the Apollo 17 version, NASA also has versions of the Blue Marble compiled from various satellites in 2001 and 2002.

Habitable Environments Could Exist Underground on Mars

Possible Phyllosilicate-Rich Area in Syrtis Major. Credit: NASA/JPL/University of Arizona

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Data from the Mars Reconnaissance Orbiter suggests that there could be habitable environments underground on Mars – in the past, and perhaps even today. Scientists discovered evidence of long-sought-after hydrothermally altered carbonate-bearing rocks which were once deep within the Red Planet, exposed within an impact crater. “Carbonate rocks have long been a Holy Grail of Mars exploration for several reasons,” said Joseph Michalski from the Planetary Science Institute. He explained that on Earth, carbonates form with the ocean and within lakes, so the same could be true for ancient Mars. “Such deposits could indicate past seas that were once present on Mars. Another reason is because we suspect that the ancient Martian atmosphere was probably denser and CO2-rich, but today the atmosphere is quite thin so we infer that the CO2 must have gone into carbonate rocks somewhere on Mars.”

This unique mineralogy was spotted within the central peak of a crater to the southwest of a giant Martian volcanic province named Syrtis Major. With infrared spectra from the Compact Reconnaissance Imaging Spectrometer for Mars (CRISM), planetary geologists detected the hydrothermal minerals from their spectroscopic fingerprints. Visible images from the HiRISE camera (High Resolution Imaging Science Experiment) on board MRO show that the carbonates and hydrated silicate minerals occur within deformed bedrock that was exhumed by an ancient meteor impact that poked through the volcanic upper crust of Mars.

The carbonate-bearing rocks were once likely about 6 km (about 4 miles) underground. The carbonate minerals exist along with hydrated silicate minerals of a likely hydrothermal origin.

Syrtis Major Planum Channel and Depression. Credit: NASA/JPL/University of Arizona

While this is not the first detection of carbonates on Mars, Michalski said, “This detection is significant because it shows other carbonates detected by previous workers, which were found in a fairly limited spatial extent, were not a localized phenomenon. Carbonates may have formed over a very large region of ancient Mars, but been covered up by volcanic flows later in the history of the planet. A very exciting history of water on Mars may be simply covered up by younger lava!”

The discovery also has implications for the habitability of the Martian crust. “The presence of carbonates along with hydrothermal silicate minerals indicates that a hydrothermal system existed in the presence of CO2 deep in the Martian crust,” Michalski says. “Such an environment is chemically similar to the type of hydrothermal systems that exist within the ocean floor of Earth, which are capable of sustaining vast communities of organisms that have never seen the light of day.

“The cold, dry surface of Mars is a tough place to survive, even for microbes. If we can identify places where habitable environments once existed at depth, protected from the harsh surface environment, it is a big step forward for astrobiological exploration of the red planet.”

Michalski and co-author Paul B. Niles of NASA Johnson Space Center recently published the results in a paper titled “Deep crustal carbonate rocks exposed by meteor impact on Mars” in Nature Geoscience.

Source: Planetary Science Institute, Nature Geoscience

Breaking News: Small NEO Could Pass Within 60,000 km of Earth on Tuesday

Artists impression of an asteroid flying by Earth. Credit: NASA

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A small asteroid will likely pass very close to Earth this week Tuesday. Astronomers are still tracking the object, now designated as 2010 TD54, and various estimates say it could possibly come within anywhere from 52,000 km (33,000 miles) to 64,000 km (40,000 miles) on October 12, with closest approach at approximately 11:25 UT. Information on the IAU Minor Planet Center website lists the object as coming with 0.0003 AU. The size of the object has not been determined, but estimates say it is likely smaller than 10 meters. We’ll provide an update as soon as more information is available.

UPDATE: Don Yeomans, Manager of NASA’s Near-Earth Object Program Office replied to an inquiry about the object and said the newly discovered NEO 2010 TD54 is approximately 5-10 meters in size, and is now predicted to pass about 46,000 km from Earth’s surface at about 07:25 EDT (11:25 UT) on Tuesday, Oct 12, 2010. It was discovered by Catalina Sky Survey on Saturday morning.

“Only 1 in a million chance of an impact,” Yeomans said, “and even if it does impact, it is not large enough to make it through the Earth’s atmosphere to cause ground damage.”

The object may be visible to amateur telescopes as a 14th magnitude “star” — it will be traveling through the constellations Pisces and Aquarius.

Sources: IAU Minor Planet Center, Unmanned Spaceflight,Yahoo News Groups

Virgin Galactic’s SpaceShipTwo Makes First Glide Flight

SpaceShipTwo's glide flight. Credit: Virgin Galactic

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Does this image look futuristic? Well, the future is here, as this is an actual image from October 10, 2010 (today!) Virgin Galactic’s future passenger ship made its first manned glide flight on Sunday. SpaceShipTwo’s unpowered flighted lasted about 11 minutes after the spacecraft was released from its White Knight Two mother ship, Eve, at 13,700 meters (45,000 feet) over the Mojave Desert. Scaled Composites test pilot Pete Siebold flew her down to the Mojave Spaceport, with with Mike Alsbury as co-pilot. “The VSS Enterprise was a real joy to fly,” said Siebold after landing, “especially when one considers the fact that the vehicle has been designed not only to be a Mach 3.5 spaceship capable of going into space but also one of the worlds highest altitude gliders.”

UPDATE: Virgin has now released a video of the flight, see below.

SpaceShipTwo will carry six people in addition to two pilots, providing those on board with a view of space and several minutes of weightlessness once space flights begin. Eventual operational flights of SpaceShipTwo will occur from Spaceport America in New Mexico. Latest word is that the first passenger flights could begin in 2011.

All the flight and all systems appeared to operate trouble free. After a clean release, Siebold completed initial flight handling and stall characteristic evaluation of SpaceShipTwo. After completing a practice approach and landing, Siebold made a smooth landing.

VSS Enterprise glides through the Mojave skies. Credit: Virgin Galactic, Mark Greenberg

“This was one of the most exciting days in the whole history of Virgin,” said Richard Branson, founder of Virgin Galactic. “For the first time since we seriously began the project in 2004, I watched the world’s first manned commercial spaceship landing on the runway at Mojave Air and Space Port and it was a great moment. Now, the sky is no longer the limit and we will begin the process of pushing beyond to the final frontier of space itself over the next year.”

“This is a critical milestone in Virgin Galactic’s test program and a great day for the commercial spaceflight industry,” added John Gedmark, Executive Director of the Commercial Spaceflight Federation. “At the end of the day, getting hardware off the ground is what it’s really all about. Today’s SpaceShipTwo test flight marks another key milestone towards opening the space frontier for private individuals, researchers, and explorers. Congratulations to the entire SpaceShipTwo team.”

SpaceShipTwo and WhiteKnightTwo are being developed for Virgin Galactic by Scaled Composites, who built SpaceShipOne, the first privately-built vehicle to fly a person into space, which won the $10 million Ansari X PRIZE.

Future passengers will be flown about 100km (62 miles) above the Earth and experience several minutes of weightlessness before returning to Spaceport America. Tickets cost $200,000 and deposits start from $20,000. Find more info about passenger flights at Virgin Galactic’s website

Sources: Virgin Galactic, Commercial Spaceflight Federation

Interview with Nancy at PARS3C

Elizabeth Howell is a writer/blogger from Canada, and I met her when I was at Kennedy Space Center earlier this year for a space shuttle launch. She has a blog called “PARS3C” and each week she has a feature called “High 5” where she interviews a “spacey”-type person. This week, Elizabeth has interviewed me, so if you’d like to read it, head on over to her blog, where you can find out how I came to be a journalist, and what some of the articles are I’m working on for the future. And stay awhile and browse through the other articles that Elizabeth has written, too. She’s got a nice writing style, and covers a large range of topics — she was nominated for a Canadian Weblog award this year, too.

Thanks Elizabeth!

Astronomy Without A Telescope – Solar Or RTG?

The 'edge of the envelope' solar powered Juno mission - scheduled for launch in 2011.

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It used to be the case that if you wanted to send a spacecraft mission out past the asteroid belt, you’d need a chunk of plutonium-238 to generate electric power – like for Pioneers 10 and 11, Voyagers 1 and 2, Galileo, Cassini, even Ulysses which just did a big loop out and back to get a new angle on the Sun – and now New Horizons on its way to Pluto.

But in 2011, the Juno mission to Jupiter is scheduled for launch – the first outer planet exploration mission to be powered by solar panels. And also scheduled for 2011, in another break with tradition – Curiosity, the Mars Science Laboratory will be the first Mars rover to be powered by a plutonium-238 radioisotope thermoelectric generator – or RTG.

I mean OK, the Viking landers had RTGs, but they weren’t rovers. And the rovers (including Sojourner) had radioisotope heaters, but they weren’t RTGs.

So, solar or RTG – what’s best? Some commentators have suggested that NASA’s decision to power Juno with solar is a pragmatic one – seeking to conserve a dwindling supply of RTGs – which have a bit of a PR problem due to the plutonium.

However, if it works, why not push the limits of solar? Although some of our longest functioning probes (like the 33 year old Voyagers) are RTG powered, their long-term survival is largely a result of them operating far away from the harsh radiation of the inner solar system – where things are more likely to break down before they run out of power. That said, since Juno will lead a perilous life flying close to Jupiter’s own substantial radiation, longevity may not be a key feature of its mission.

Perhaps RTG power has more utility. It should enable Curiosity to go on roving throughout the Martian winter – and perhaps manage a range of analytical, processing and data transmission tasks at night, unlike the previous rovers.

With respect to power output, Juno’s solar panels would allegedly produce a whopping 18 kilowatts in Earth orbit, but will only manage 400 watts in Jupiter orbit. If correct, this is still on par with the output of a standard RTG unit – although a large spacecraft like Cassini can stack several RTG units together to generate up to 1 kilowatt.

So, some pros and cons there. Nonetheless, there is a point – which we might position beyond Jupiter’s orbit now – where solar power just isn’t going to cut it and RTGs still look like the only option.

Left image: a plutonium-238 ceramic pellet glowing red hot, like most concentrated ceramicised radioisotopes will do. Credit: Los Alamos National Laboratory. Right image: the Apollo 14 ALSEP RTG, almost identical to Apollo 13's RTG which re-entered Earth's atmosphere with the demise of the Aquarius lunar module. Credit: NASA

RTGs take advantage of the heat generated by a chunk of radioactive material (generally plutonium 238 in a ceramic form), surrounding it with thermocouples which use the thermal gradient between the heat source and the cooler outer surface of the RTG unit to generate current.

In response to any OMG it’s radioactive concerns, remember that RTGs travelled with the Apollo 12-17 crews to power their lunar surface experiment packages – including the one on Apollo 13 – which was returned unused to Earth with the lunar module Aquarius – the crew’s life boat until just before re-entry. Allegedly, NASA tested the waters where the remains of Aquarius ended up and found no trace of plutonium contamination – much as expected. It’s unlikely that its heat tested container was damaged on re-entry and its integrity was guaranteed for ten plutonium-238 half-lives, that is 900 years.

In any case, the most dangerous thing you can do with plutonium is to concentrate it. In the unlikely event that an RTG disintegrates on Earth re-entry and its plutonium is somehow dispersed across the planet – well, good. The bigger worry would be that it somehow stays together as a pellet and plonks into your beer without you noticing. Cheers.

Melas Chasma: The Deepest Abyss on Mars

Melas Chasma sinks 9 km below the surrounding surface, making it one of the lowest depressions on the planet. Credits: ESA/DLR/FU Berlin (G. Neukum)

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Melas Chasma is part of the huge Valles Marineris that cuts into the middle of Mars surface, making it a pretty interesting place: there is abundant evidence for water having flowed here, with ancient water-cut channels visible even from orbit. Also visible are landslides that have created huge fans of rubble at the base of the cliffs. These newest images from ESA’s Mars Express show Melas Chasma, which sinks 9 km below the surrounding surface, making it one of the lowest depressions on the planet. This is just a small part of the bigger Valles Marineris, which stretches for more than 4,000 km across the surface of Mars. Around Melas Chasma, there are lighter-coloured deposits of sulphate components that were probably deposited in a former lake.

Melas Chasma stretches for more than 4000 km across the face of Mars. Credits: ESA/DLR/FU Berlin (G. Neukum)

These images were captured in 2006 and just released by the Mars Express team. See more details and images at the ESA website.

Poor in one, Rich in another

Tycho's Supernova Remnant. Credit: Spitzer, Chandra and Calar Alto Telescopes.

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Just over three years ago, I wrote a blog post commemorating the 50th anniversary of one of the most notable papers in the history of astronomy. In this paper, Burbidge, Burbidge, Fowler, and Hoyle laid out the groundwork for our understanding of how the universe builds up heavy elements.

The short version of the story is that there are two main processes identified: The slow (s) process and the rapid (r) process. The s-process is the one we often think about in which atoms are slowly bombarded with protons and neutrons, building up their atomic mass. But as the paper pointed out, this often happens too slowly to pass roadblocks to this process posed by unstable isotopes which don’t last long enough to catch another one before falling back down to lower atomic number. In this case, the r-process is needed in which the flux of nucleons is much higher in order to overcome the barrier.

The combination of these two processes has done remarkably well in matching observations of what we see in the universe at large. But astronomers can never rest easily. The universe always has its oddities. One example is stars with very odd relative amounts of the elements built up by these processes. Since the s-process is far more common, they’re what we should see primarily, but in some stars, such as SDSS J2357-0052, there exists an exceptionally high concentration of the rare r-process elements. A recent paper explores this elemental enigma.

As the designation implies, SDSS J2357-0052’s uniqueness was discovered by the Sloan Digital Sky Survey (SDSS). The survey uses several filters to image fields of stars at different wavelengths. Some of the filters are chosen to lie in wavelength ranges in which there are well known absorption lines for elements known to be tracers of overall metallicity. This photometric system allowed an international team of astronomers, led by Wako Aoki of the National Astronomical Observatory in Tokyo, to get a quick and dirty view of the metal content of the stars and choose interesting ones for followup study.

These followup observations were done with high resolution spectroscopy and showed that the star had less than one one-thousandth the amount of iron that the Sun does ([Fe/H] = -3.4), placing it among the most metal poor stars ever discovered. However, iron is the end of the elements produced by the s-process. When going beyond that atomic number, the relative abundances drop off very quickly. While the drop off in SDSS J2357-0052 was still steep, it wasn’t near as dramatic as in most other stars. This star had a dramatic enhancement of the r-process elements.

Yet this wasn’t exceptional in and of itself. Several metal poor stars have been discovered with such r-process enhancements. But none coupled with such an extreme deficiency of iron. The implication of this combination is that this star was very close to a supernova. The authors suggest two scenarios that can explain the observations. In the first, the supernova occurred before the star formed, and SDSS J2357-0052 was formed in the immediate vicinity before the enhanced material would be able to disperse and mix into the interstellar medium. The second is that SDSS J2357-0052 was an already formed star in a binary orbit with a star that became a supernova. If the latter case is true, it would likely give the smaller star a large “kick” as the mass holding the system would change dramatically. Although no exceptional radial velocity was detected for SDSS J2357-0052, the motion (if it exists) could be in the plane of the sky requiring proper motion studies to either confirm or refute this possibility.

The authors also note that the first star with somewhat similar characteristics (although not as extreme), was discovered first in the outer halo where the likelihood of the necessary supernova occurring is low. As such, it is more likely that that star was ejected in such a process establishing some credibility for the scenario in general, even if not the case for SDSS J2357-0052.

Water Ice Found on Another Asteroid

Artists concept of an asteroid around a planetary body. Credit: Gabriel Pérez, Instituto de Astrofisica de Canarias, Spain

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There could be a lot more water out there than anyone thought. A second asteroid has been found to contain water ice. In April of this year, water ice and organics was found on 24 Themis, a 200-kilometer wide asteroid. Now, the two teams of researchers made who made the first discovery have now found the same materials on asteroid 65 Cybele.

“This discovery suggests that this region of our solar system contains more water ice than anticipated,” said University of Central Florida Professor Humberto Campins. “And it supports the theory that asteroids may have hit Earth and brought our planet its water and the building blocks for life to form and evolve here.”

Asteroid 65 Cybele is somewhat larger than asteroid 24 Themis, with a diameter of 290 km (180 miles). Both asteroids are located in the asteroid belt that sits halfway between Mars and Jupiter.

Generally, asteroids were thought to be very dry, but it now appears that when the asteroids and planets were first forming in the very early Solar System, ice extended far into the Main Belt region, which could mean water and organics may be more common near each star‘s habitable zone.

See our article from yesterday about molecules of life’s building blocks in Titan’s atmosphere and how it could add a third way for life to spring up on a planet (one being asteroid delivery, two being rising from the primordial soup thought to exist on early Earth).

The team’s paper will be published in the European Journal “Astronomy and Astrophysics,” and Campins presented his findings at the American Astronomical Society’s Division of Planetary Sciences meeting this week.

Source: University of Central Florida