Showing posts with label Osiris-Rex Asteroid Proposal. Show all posts
Showing posts with label Osiris-Rex Asteroid Proposal. Show all posts

Thursday, June 16, 2011

A Preview of What OSIRIS-REx May Return


Origin and Evolution of Prebiotic Organic Matter As Inferred from the Tagish Lake Meteorite Christopher D. K. Herd, et al. Science 332, 1304 (2011); DOI: 10.1126/science.1203290

Chance has provided us with a preview of the types of scientific analysis the samples returned by the just approved OSIRIS-REx asteroid sample return mission may provide.  In early 2000, a fragment from a primitive asteroid entered the Earth's atmosphere.  It is rare for scientists to be able to examine fairly pristine samples of these asteroids.    In this case, the fragments landed on the frozen Tagish Lake in the Yukon region of Canada.  A local resident spotted the samples lying on the ice, carefully retrieved them, and kept them frozen until they could be delivered to scientists.  (Scientists also later retrieved additional samples in the spring before the ice had thawed.)   (See http://en.wikipedia.org/wiki/Tagish_Lake_(meteorite) for more on this meteorite.)

Last week, a paper in the journal Science published the latest findings from this meteorite (see the press release below).  The opening of the paper explains why carbonaceous chondrite samples -- the type of material in the Tagish Lake meteorite -- are so important to scientists wanting to understand the early solar system: these samples come from primitive asteroids that preserve the materials of the early solar nebula and results of the processes that occurred within those early building blocks.

The conditions for finding carbonaceous condrite meteorites in pristine condition are rare.  Instead of waiting for a random sample to come to us, the OSIRIS-REx asteroid sample return mission will go to the asteroid to carefully select its samples to return to Earth.  

Dante Lauretta, Deputy PI for the mission, has been kind enough to send me material on the mission over the past two years that have formed the basis for posts on this mission in this blog.  I asked him if the the Tagish Lake samples are representative of the type of material they hope to return and whether baking by the sun might degrade the sample.  He wrote back, "Tagish Lake is a good analog for the type of material that we are interested in. Our spectral analysis of 1999 RQ36 suggests it is most similar to the CM1 chondrites. 

"We are interested in the interaction of the organic material with solar radiation. Organic does not always mean volatile and it is likely that even a heavily space weathered surface would have interesting organic chemistry. One of our objectives is to understand the effect of this 'space weathering' on carbonaceous material. However, we have evidence that the surfaces of near-Earth objects may be refreshed during exceptionally close planetary encounters. Tidal forces are strong enough to turn small bodies inside out, especially if they are rubble piles. This is good news for us since 1999 RQ36 is likely to have had multiple close encounters with the Earth in its recent history. If these theories are correct, NEOs with Earth close approaches may be ideal material to sample relatively fresh, low-space-weathering material right on the surface. These are some of the hypotheses that our mission will be testing."

The following press release from NASA's Goddard Space Flight Center gives more background on the Tagish Lake meteorite has reveal and possibly previews the kinds of discoveries to be enabled by the OSIRIS-REx samples.



Some asteroids may have been like "molecular factories" cranking out life's ingredients and shipping them to Earth via meteorite impacts, according to scientists who've made discoveries of molecules essential for life in material from certain kinds of asteroids and comets. Now it appears that at least one may have been less like a rigid assembly line and more like a flexible diner that doesn't mind making changes to the menu. 

In January, 2000, a large meteoroid exploded in the atmosphere over northern British Columbia, Canada, and rained fragments across the frozen surface of Tagish Lake. Because many people witnessed the fireball, pieces were collected within days and kept preserved in their frozen state. This ensured that there was very little contamination from terrestrial life. 

A fragment from the Tagish Lake meteorite fallThis is one of the Tagish Lake meteorite fragments. Credit: Michael Holly, Creative Services, University of Alberta.
Full-resolution copy 
"The Tagish Lake meteorite fell on a frozen lake in the middle of winter and was collected in a way to make it the best preserved meteorite in the world," said Dr. Christopher Herd of the University of Alberta, Edmonton, Canada, lead author of a paper about the analysis of the meteorite fragments published June 10 in the journal Science. 

"The first Tagish Lake samples -- the ones we used in our study that were collected within days of the fall -- are the closest we have to an asteroid sample return mission in terms of cleanliness," adds Dr. Michael Callahan of NASA's Goddard Space Flight Center in Greenbelt, Md., a co-author on the paper. 

The Tagish Lake meteorites are rich in carbon and, like other meteorites of this type, the team discovered the fragments contained an assortment of organic matter including amino acids, which are the building blocks of proteins. Proteins are used by life to build structures like hair and nails, and to speed up or regulate chemical reactions. What's new is that the team found different pieces had greatly differing amounts of amino acids. 

"We see that some pieces have 10 to 100 times the amount of specific amino acids than other pieces," said Dr. Daniel Glavin of NASA Goddard, also a co-author on the Science paper. "We've never seen this kind of variability from a single parent asteroid before. Only one other meteorite fall, called Almahata Sitta, matches Tagish Lake in terms of diversity, but it came from an asteroid that appears to be a mash-up of many different asteroids." 

By identifying the different minerals present in each fragment, the team was able to see how much each had been altered by water. They found that various fragments had been exposed to different amounts of water, and suggest that water alteration may account for the diversity in amino acid production. 

"Our research provides new insights into the role that water plays in the modification of pre-biotic molecules on asteroids," said Herd. "Our results provide perhaps the first clear evidence that water percolating through the asteroid parent body caused some molecules to be formed and others destroyed. The Tagish Lake meteorite provides a unique window into what was happening to organic molecules on asteroids four-and-a-half billion years ago, and the pre-biotic chemistry involved." 

If the variability in Tagish Lake turns out to be common, it shows researchers have to be careful in deciding whether meteorites delivered enough bio-molecules to help jump-start life, according to the team. 

"Biochemical reactions are concentration dependent," says Callahan. "If you're below the limit, you're toast, but if you're above it, you're OK. One meteorite might have levels below the limit, but the diversity in Tagish Lake shows that collecting just one fragment might not be enough to get the whole story." 

Although the meteorites were the most pristine ever recovered, there is still some chance of contamination though contact with the air and surface. However, in one fragment, the amino acid abundances were high enough to show they were made in space by analyzing their isotopes. 

Isotopes are versions of an element with different masses; for example, carbon 13 is a heavier, and less common, variety of carbon. Since the chemistry of life prefers lighter isotopes, amino acids enriched in the heavier carbon 13 were likely created in space. 

"We found that the amino acids in a fragment of Tagish Lake were enriched in carbon 13, indicating they were probably created by non-biological processes in the parent asteroid," said Dr. Jamie Elsila of NASA Goddard, a co-author on the paper who performed the isotopic analysis. 

The team consulted researchers at the Goddard Astrobiology Analytical Lab for their expertise with the difficult analysis. "We specialize in extraterrestrial amino acid and organic matter analysis," said Dr. Jason Dworkin, a co-author on the paper who leads the Goddard laboratory. "We have top-flight, extremely sensitive equipment and the meticulous techniques necessary to make such precise measurements. We plan to refine our techniques with additional challenging assignments so we can apply them to the OSIRIS-REx asteroid sample return mission." 

OSIRIS-REx (Origins, Spectral Interpretation, Resource Identification, Security -- Regolith Explorer) is a Goddard-managed mission, led by the University of Arizona, that will be launched toward asteroid "1999 RQ36" in 2016 and return a sample to Earth in 2023. The OSIRIS-REx team is led by Dr. Michael Drake, Director of the University of Arizona's Lunar and Planetary Laboratory. 

The Tagish Lake research was funded by the Natural Sciences and Engineering Research Council of Canada, the Alberta Ingenuity Fund, and NASA. 

Monday, June 6, 2011

OSIRIS-REx: More than a Sample Return Mission


The Martian moon Phobos, which may be a captured asteroid.  This image shows the complexity of the surfaces of small, primitive bodies.  Phobos, with a mean diameter of 11.1 km is many times larger than the OSIRIS-REx target, asteroid 1999 RQ36.  Credit: HiRISE, MRO, LPL (U. Arizona), NASA


"The Near-Earth Asteroid Rendevous (NEAR) mission to 433 Eros demonstrated that even small asteroids are covered with complex and substantial regoliths, which are heterogeneous in texture and detailed in composition.  To understand the geologic evolution of asteroids, regoliths must be studied in detail, and their variability must be characterized both vertically and horizontally... To maximize the science return from such a mission, it is essential to select the most interesting locales on the asteroid, a goal that implies a global reconnaissance of the target body."
-- New Frontiers in the Solar System An Integrated Exploration Strategy [2003 Planetary Decadal Survey]

[An asteroid sample return mission] "should have the following science objectives...":
  • "Map the surface texture, spectral properties (e.g., color, albedo), and geochemistry of the surface of an asteroid at sufficient spatial resolution to resolve geologic features (e.g., craters, fractures, lithologic units) necessary to decipher the geologic history of the asteroid and provide context for returned samples.
  • "Document the regolith at the sampling site in situ with emphasis on, e.g., lateral and vertical textural, mineralogical, and geochemical heterogeneity at scales down to the submillimeter.
  • "Return a sample to Earth in an amount sufficient for molecular (or organic) and mineralogical analyses, including documentation of possible sources of contamination throughout the collection, return, and curation phases of the mission."
-- Opening New Frontiers in Space: Choices for the Next New Frontiers Announcement of Opportunity [2008]

The selection of the OSIRIS-REx New Frontiers mission to return a sample from a near-Earth asteroid has been widely reported.  As the quotes that open this post state, simply returning a sample of an asteroid is only part of a robust sample return mission.  It is also important to try to understand the history of the asteroid.  While OSIRIS-REx's target asteroid, 1999 RQ36, is believed to represent a primitive composition that will likely tell us much about conditions in the early, pre-planet solar system, the body has experienced over four billions years' worth of events.  This tiny body, 575 m in diameter, is likely a fragment of a larger asteroid.  Since its separation from its original parent body, this asteroid will have been pounded by numerous collisions and may well be a pile of rubble with materials from various depths of its parent body jumbled together and exposed on the surface.  That material on the surface from which the sample will be taken has been exposed for an unknown period of time to the baking and irradiation of the sun, which may have modified its composition.

All of these factors require that a robust sample return mission also be able to fully characterize the surface and interior of its target asteroid.  Earlier versions of this mission, then called only OSIRIS, focused only on the sample return.  The recently approved version of the mission includes a suite of instruments to remotely study this body:

  • Camera Suite (OCAMS) Provides long-range acquisition of 1999 RQ36, along with global mapping, sample-site characterization, sample acquisition documentation, and sub-mm imaging
  • Visible and IR Spectrometer (OVIRS) Provides mineral and organic spectral maps and local spectral information of candidate sample sites from 0.4 - 4.3 μm•
  • Thermal Emission Spectrometer (OTES) Provides mineral and thermal emission spectral maps and local spectral information of candidate sample sites from 4 - 50 μm
  • X-ray Imaging Spectrometer (REXIS) instrument as a student collaboration experiment. This instrument will be built by MIT and Harvard students and is designed to map the abundances of major elements on the surface of the asteroid
  • Laser Altimeter (OLA) Provides ranging data; global topographic mapping; and local topographic maps of candidate sample sites
  • Spacecraft Telecom Radio science provides RQ36 mass and gravity field maps
OSIRIS-REx Spacecraft and Instruments

The suite of instruments are synergistic.  The cameras, for example, will document the physical structure of the surface, providing clues to past events.  The OVIRS and OTES instruments will measure different portions of the visible and infrared spectra to understand the composition of the surface minerals.  The REXIS instrument, by contrast, will look at the elemental composition of the surface.  (A simple analogy of the difference between elemental and mineralogical composition: Bread and cake have similar 'elemental' compositions based on flour, water, and sugar, but the combination of those elements result in distinct 'mineralogies'.)  The laser altimeter and radio science together will map the shape of the surface and distribution of mass inside RQ36, which together will provide clues to the interior structure.

The instruments on OSIRIS-REx will have dual purposes.  While they will help us understand the composition and history of this body, they will also help mission planners to plan the sample acquisition.  The cameras and laser altimeter will reveal the physical geography of potential sample sites, while the spectrometers will reveal the composition.  (My guess: Mission controllers will select a site that has the best mixture of materials on the surface to sample the greatest heterogeneity.)

The OSIRIS-REx spacecraft will spend more than a year studying 1999 RQ36.  By the end of this period, it will probably be, square-meter-for-square-meter,  the most intensively studied body in the solar system.

OSIRIS-REx is not the only mission that aims to return a sample of a likely primitive small body.  Russia's Phobos-Grunt mission will leave this year on a round trip to the Martian moon Phobos, which may be a captured asteroid.  (RQ36 is a B-type asteroid, while Phobos is a likely C-type body, which are both believed to represent relatively unaltered samples of the non-volatile early solar system.)  Russia's mission will carry a number instruments to characterize its target moon.  In fact, it's instrument suite is more wide ranging than OSIRIS-REx's, with both remote sensing and surface instruments.  

OSIRIS-REx and Phobos-Grunt will be joined this decade by the Hayabusa 2 mission, which will also sample a primitive, C-type asteroid.  It appears that Hayabusa 2 will, like Hayabusa 1, carry a number of remote sensing instruments to characterize its target and plan for the sample acquisition.  The European Space Agency is also considering a primitive asteroid sample return mission, Marco Polo-R, for the 2020s that will likely carry several remote sensing instruments. 

The OSIRIS-REx mission will also carry a sampling mechanism.

Background: 

The OSIRIS-REx team has posted a fact sheet on the mission: http://uanews.org/files/osiris-rex/OSIRIS-REx_Factsheet.pdf  All images in this post, except the image of Phobos, are from the fact sheet and are reused with permission.



Several articles in Wikipedia provide background on the types of asteroids:



B-type asteroids (which are considered a sub-type of C-type asteroids): http://en.wikipedia.org/wiki/B-type_asteroid

Wednesday, May 25, 2011

Asteroid Sample Return Mission Selected



NASA announced the selection of the OSIRIS-REx near-Earth asteroid sample return for the next New Frontiers mission, beating out a Venus lander and a lunar sample return mission.  Bruce Moomaw wrote about the OSIRIS-REx mission for this blog, and his description can be found here.  There are also articles at Space News and at the Planetary Society's blog site.  NASA press release site also includes a video (which I can't watch with my current slow internet while I'm traveling): http://www.nasa.gov/topics/solarsystem/features/osiris-rex.html

With the two Japanese Hayabusa sample return missions (one completed and another in development), this means we'll have samples from three near-Earth asteroids.  ESA is also considering its own near-Earth asteroid sample return, Marco Polo.

The press release itself is copied below.  And congratulations to the winning team which submitted versions of this mission at least twice and I think perhaps three times.

May 25, 2011

Dwayne C. Brown 
Headquarters, Washington 
202-358-1726 
dwayne.c.brown@nasa.gov 

RELEASE: 11-163

NASA TO LAUNCH NEW SCIENCE MISSION TO ASTEROID IN 2016

WASHINGTON -- NASA will launch a spacecraft to an asteroid in 2016 and 
use a robotic arm to pluck samples that could better explain our 
solar system's formation and how life began. The mission, called 
Origins-Spectral Interpretation-Resource 
Identification-Security-Regolith Explorer, or OSIRIS-REx, will be the 
first U.S. mission to carry samples from an asteroid back to Earth. 

"This is a critical step in meeting the objectives outlined by 
President Obama to extend our reach beyond low-Earth orbit and 
explore into deep space," said NASA Administrator Charlie Bolden. 
"It's robotic missions like these that will pave the way for future 
human space missions to an asteroid and other deep space 
destinations." 

NASA selected OSIRIS-REx after reviewing three concept study reports 
for new scientific missions, which also included a sample return 
mission from the far side of the moon and a mission to the surface of 
Venus. 

Asteroids are leftovers formed from the cloud of gas and dust -- the 
solar nebula -- that collapsed to form our sun and the planets about 
4.5 billion years ago. As such, they contain the original material 
from the solar nebula, which can tell us about the conditions of our 
solar system's birth. 

After traveling four years, OSIRIS-REx will approach the primitive, 
near Earth asteroid designated 1999 RQ36 in 2020. Once within three 
miles of the asteroid, the spacecraft will begin six months of 
comprehensive surface mapping. The science team then will pick a 
location from where the spacecraft's arm will take a sample. The 
spacecraft gradually will move closer to the site, and the arm will 
extend to collect more than two ounces of material for return to 
Earth in 2023. The mission, excluding the launch vehicle, is expected 
to cost approximately $800 million. 

The sample will be stored in a capsule that will land at Utah's Test 
and Training Range in 2023. The capsule's design will be similar to 
that used by NASA's Stardust spacecraft, which returned the world's 
first comet particles from comet Wild 2 in 2006. The OSIRIS-REx 
sample capsule will be taken to NASA's Johnson Space Center in 
Houston. The material will be removed and delivered to a dedicated 
research facility following stringent planetary protection protocol. 
Precise analysis will be performed that cannot be duplicated by 
spacecraft-based instruments. 

RQ36 is approximately 1,900 feet in diameter or roughly the size of 
five football fields. The asteroid, little altered over time, is 
likely to represent a snapshot of our solar system's infancy. The 
asteroid also is likely rich in carbon, a key element in the organic 
molecules necessary for life. Organic molecules have been found in 
meteorite and comet samples, indicating some of life's ingredients 
can be created in space. Scientists want to see if they also are 
present on RQ36. 

"This asteroid is a time capsule from the birth of our solar system 
and ushers in a new era of planetary exploration," said Jim Green, 
director, NASA's Planetary Science Division in Washington. "The 
knowledge from the mission also will help us to develop methods to 
better track the orbits of asteroids." 

The mission will accurately measure the "Yarkovsky effect" for the 
first time. The effect is a small push caused by the sun on an 
asteroid, as it absorbs sunlight and re-emits that energy as heat. 
The small push adds up over time, but it is uneven due to an 
asteroid's shape, wobble, surface composition and rotation. For 
scientists to predict an Earth-approaching asteroid's path, they must 
understand how the effect will change its orbit. OSIRIS-REx will help 
refine RQ36's orbit to ascertain its trajectory and devise future 
strategies to mitigate possible Earth impacts from celestial objects. 

Michael Drake of the University of Arizona in Tucson is the mission's 
principal investigator. NASA's Goddard Space Flight Center in 
Greenbelt, Md., will provide overall mission management, systems 
engineering, and safety and mission assurance. Lockheed Martin Space 
Systems in Denver will build the spacecraft. The OSIRIS-REx payload 
includes instruments from the University of Arizona, Goddard, Arizona 
State University in Tempe and the Canadian Space Agency. NASA's Ames 
Research Center at Moffett Field, Calif., the Langley Research Center 
in Hampton Va., and the Jet Propulsion Laboratory in Pasadena, 
Calif., also are involved. The science team is composed of numerous 
researchers from universities, private and government agencies. 

This is the third mission in NASA's New Frontiers Program. The first, 
New Horizons, was launched in 2006. It will fly by the Pluto-Charon 
system in July 2015, then target another Kuiper Belt object for 
study. The second mission, Juno, will launch in August to become the 
first spacecraft to orbit Jupiter from pole to pole and study the 
giant planet's atmosphere and interior. NASA's Marshall Space Flight 
Center in Huntsville, Ala., manages New Frontiers for the agency's 
Science Mission Directorate in Washington. 

Tuesday, January 12, 2010

Osiris-Rex New Frontiers Proposal




The Osiris-Rex team was kind enough to send me a public version of a presentation describing the mission.  Because this is a public version, most mission details are not included.  Discovery and New Frontiers mission competitions are highly competitive, and most proposals are selected (if ever) after several submissions.  (All three New Frontiers proposals this time around have been finalists in previous mission selections.)  So teams keep the details close to the chest in case they have to submit again.  No point to enabling the competition in a future competition.

I'm at a busy point, so Bruce Moomaw was kind enough to go through the presentation and summarize key points:

(1)  The target asteroid is the same as for OSIRIS' previous incarnation as a Discovery-class mission: 1999 RQ36, a "B-class" carbonaceous asteroid made of primitive material from the Solar System's early history that has not undergone extensive heating and thus modification since it was incorporated into the original Main Belt asteroid of which RQ36 is a broken-away fragment.

(2)  1999 RQ36 has several important characteristics.  It's the darkest-colored asteroid yet measured (reflecting only 3% of the sunlight that hits it), which means that it must be made of particularly carbon-rich minerals exposed to minimal heating -- almost certainly including substantial amounts of fairly complex organic molecules.  It has been substantially examined and mapped both by the ground-based Arecibo radar observatory and the infrared Spitzer Space Telescope -- which have provided data both on its overall size, shape and rotation, and on its overall composition (the asteroid not only has "a spectral signature suggesting a carbon- and volatile-rich surface", but apparently has a good deal of loose regolith on its surface that can be easily sampled by a spacecraft). 

(3)  And 1999 RQ36 also happens to have "the highest probability of impacting the Earth of any known Potentially Hazardous Asteroid" -- specifically, a one-in-1800 chance of hitting Earth in 2170.  OSIRIS REx, during its year or so of orbiting the asteroid before finally dipping briefly to its surface for sampling, will allow Earth tracking stations to determine the asteroid's orbit with extreme precision -- thus further allowing forecasts of the probability of its striking Earth (as well as allowing the best measurements yet of the "Yarkovsky Effect" by which the absorption and reflection of sunlight by different parts of a rotating asteroid can actually produce a faint but significant thrust that modifies its orbit).

(4)  OSIRIS REx is scheduled to collect and return an absolute minimum of 60 grams (about two ounces) of material from the asteroid's surface -- but it has the ability, if conditions are favorable, to return as much as two kilograms of material (about 4 1/2 pounds).  It will not only map the global chemical, mineralogical and physical structure of the asteroid to put the returned sample in perspective, but will "document the texture, morphology, volatile chemistry, and spectral properties of the regolith at the sampling site in situ at scales down to the sub-millimeter" -- presumably using some instruments attached to the boom-mounted sampling device itself (which can flex like an arm to load the sample into the Earth return capsule mounted on the spacecraft's side).

(5)  The craft will use scanning lidar (laser radar) to steer itself to precise courses around the asteroid and down to appropriate spots on its surface, enabling it to acquire samples "with no time-critical events" -- that is, once it has descended to near the surface and matched the asteroid's rotation rate, it can collect its samples in a leisurely way according to what its navigational instruments tell it, instead of having to work against a tight time deadline.  It will also provide more practice to ground controllers in carrying out such precision movements around a small body such as an asteroid or comet nucleus.

(6)  OSIRIS REx is a cooperative effort by the Goddard Space Flight Center, the University of Arizona, and Lockheed Martin (which would build the craft) -- but it also includes one science instrument from Arizona State University (a thermal infrared spectrometer), and another unspecified one from the Canadian Space Agency.