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Reconciling Methane Variations on Mars

mars-esa

Since the discovery of its presence in the Martian atmosphere, methane has remained an intriguing atmospheric component which source (either of biotic or abiotic origin) is not yet fully understood. The recently reported variations in the concentration of atmospheric methane have proven difficult to explain with 3-D numerical models of the atmosphere that include the known chemical and physical processes.

In a paper published this week in Nature, Franck Lefèvre and François Forget present their study to derive the implications of the observed methane concentrations on Mars and their variability. They conclude that there needs to be both an intense localised source of methane and a destruction mechanism that is much more efficient than the known atmospheric processes that break down methane.

Further, if this efficient destruction of methane occurs only close to the surface, these findings imply a very harsh environment for organic molecules to survive on the surface of Mars.

The Martian atmosphere is composed mainly of CO2 (95%), with nitrogen and argon forming the largest contributions to the remainder. Methane (CH4) was discovered to be among the other trace components as reported in 2004 from observations by both the PFS instrument on board Mars Express (Formisano et al.) and ground based telescopes (Krasnopolsky et al.). These observations also indicated that the distribution of methane was not uniform across the planet.

Explore this topic further at ESA.


Mars Dust Devil Has Colorful Effect in Image Series

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(Above) While the panoramic camera (Pancam) on NASA’s Mars Exploration Rover Spirit was taking exposures with different color filters during the 1,919th Martian day of the rover’s mission (May 27, 2009), dust devils moved across the field of view.

Scientists have combined a trio of shots taken seconds apart through different colored filters to create a special-effects portrait of a moving dust devil on Mars.

The panoramic camera on NASA’s Mars Exploration Rover Spirit was taking exposures through different filters during the 1,919th Martian day of Spirit’s mission (May 27, 2009) as part of constructing a large color panorama. Three westward shots, with several seconds intervening between them, caught a whirlwind in motion. A composite image combining the three exposures to make a color image of the Martian ground shows the dust devil in different colors, according to where it was on the horizon when each exposure was taken.

Dust devils occur on both Mars and on Earth when solar energy heats the surface, resulting in a layer of warm air just above the surface. Since the warmed air is less dense than the cooler atmosphere above it, it rises, making a swirling thermal plume that picks up the fine dust from the surface and carries it up into the atmosphere. This plume of dust moves with the local wind.

More than 650 dust devils have been recorded by Spirit since its operations began in 2004. The mission is currently in its third season of dust devils on Mars, which typically begin in Martian spring.


Largest Heat Shield Ever Built Readied for Next Mars Rover

Mars Science Lab Heatshield

(Above) The finished heat shield for NASA’s Mars Science Laboratory, with a diameter of 4.5 meters (14 feet, 9 inches), is the largest ever built for descending through the atmosphere of any planet. This image shows the heat shield and a spacecraft worker at Lockheed Martin Space Systems, Denver, which built and tested the heat shield.

Lockheed Martin completed production and testing of the heatshield for NASA’s Mars Science Laboratory (MSL). The heatshield is half of the large and sophisticated two-part aeroshell that will encapsulate and protect the Curiosity rover during its deep space cruise to Mars, and from the intense heat and friction that will be generated as the system descends through the Martian atmosphere.

In October 2008, Lockheed Martin delivered the other half of the aeroshell, the backshell, to NASA’s Jet Propulsion Laboratory in Pasadena, Calif. where it is being integrated with other flight systems. The heatshield will be stored at Lockheed Martin facilities near Denver, Colo. until early 2011 when it will be shipped to Kennedy Space Center.

The aeroshell/heatshield is the largest ever built to be flown at 4.5 meters (nearly 15 feet) in diameter. In contrast, the aeroshells/heatshields of the Spirit and Opportunity Mars Exploration Rovers measured 8.5 feet and Apollo capsule heatshields measured just less than 13 feet.

Because of the unique entry trajectory profile that could create external temperatures up to 3,800 degrees Fahrenheit, the heatshield uses a tiled Phenolic Impregnated Carbon Ablator (PICA) thermal protection system instead of the Mars heritage Super Lightweight Ablator (SLA) 561V. This will be the first time PICA has flown on a Mars mission. Invented by NASA Ames Research Center, PICA was first flown as the thermal protection system on the heatshield of the Stardust Sample Return Capsule that is now in the Smithsonian Air and Space Museum.

“The Mars Science Laboratory aeroshell is the most complex capsule to fly to Mars,” said Rich Hund, MSL program manager at Lockheed Martin Space Systems Company. “The design had to address the large size and weight of the rover, the largest ever sent to Mars, and the requirement for landing at a more-precise point on Mars.”

The aeroshell has a steering capability that is produced by ejecting ballast that off-sets the center-of-mass prior to entry into the atmosphere. This off-set creates lift as it interacts with the thin Martian atmosphere and allows roll control and autonomous steering through the use of thrusters.

Prior to shipping to Kennedy Space Center, engineers will install the MSL Entry Descent and Landing Instrumentation (MEDLI) suite on the heatshield. Developed by NASA Langley Research Center, the MEDLI instrumentation will measure heatshield temperatures and atmospheric pressures as the aeroshell descends through the Martian atmosphere.

Scheduled for launch in the fall of 2011, the Curiosity rover – built by the Jet Propulsion Laboratory – will support the Mars Exploration Program’s strategy of “follow the water” and will have the science goals of determining whether the planet was ever habitable, characterizing the climate and geology of Mars, and preparing for human exploration.


NASA & ESA Establish Joint Mars Exploration Initiative

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Last month the ESA Director of Science and Robotic Exploration, David Southwood, met NASA’s Associate Administrator for Science, Ed Weiler, in Plymouth, UK, to establish a framework for future exploration of the Red Planet.

The outcome of the bilateral meeting was an agreement to create a Mars Exploration Joint Initiative (MEJI) that will provide a framework for the two agencies to define and implement their scientific, programmatic and technological goals at Mars.

Discussions between ESA and NASA began in December 2008, driven by the ESA Ministerial Council’s recommendation to seek international cooperation to complete the ExoMars mission and to prepare further Mars robotic exploration missions. At the same time, NASA was reassessing its Mars Exploration Program portfolio after the launch of its Mars Science Laboratory was delayed from 2009 to 2011.

This provided ESA and NASA with an opportunity to increase cooperation and expand collective capabilities. To investigate the options in depth, a joint ESA/NASA engineering working group was established, along with a joint executive board to steer the efforts and develop final recommendations on how to proceed.

At the bilateral meeting in Plymouth, the executive board recommended NASA and ESA establish MEJI spanning launch opportunities in 2016, 2018 and 2020, with landers and orbiters conducting astrobiological, geological, geophysical and other high-priority investigations, and leading to the return of samples from Mars in the 2020s. The Director and Associate Administrator agreed, in principle, to establish the Initiative and continue studies to determine the most viable joint mission architectures.

ESA and NASA also agreed to establish a joint architecture review team to assist the agencies in planning the mission portfolio. As plans develop, they will be reviewed by ESA member states for approval and by the US National Academy of Sciences. This unique collaboration of missions and technologies will pave the way for exciting discoveries at Mars.


Free Spirit: Mars Rover Extraction Tests Begin

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(Above) After commanding five of a test rover’s six wheels to drive forward, rover driver Paolo Bellutta (left) measures how much the rover moved sideways, downslope, during the maneuver.

Using a test rover in a sandbox at JPL with special soil simulating Spirit’s predicament on Mars, engineers are assessing possible maneuvers for getting Spirit out and onto firmer ground. The tests began on Monday, July 6, with the simplest maneuver on their list of options: driving forward with all five operable wheels.

In the first set of tests, the wheels turned enough to cover tens of meters, or yards, if there had been no slippage. The test rover moved slightly forward and sideways downslope. Weeks of further testing and analysis of results are expected before engineers identify the best moves to command Spirit to make.


SPACE ART: Mars Nuclear Electric-Propelled Vehicle

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(Above) This artist’s concept shows a nuclear electric-propelled vehicle, about the size of a football field, firing banks of ion thrusters in order to circularize its orbit around Mars.

Assembled in Earth orbit, the transfer vehicle with its 10 megawatt power plant could transport 130 metric ton payloads to Mars in 6 1/2 months, and could repeat its circuit every 52 months.

This artwork was done for NASA by Patrick Rawlings.


NASA Phoenix Results Point to Martian Climate Cycles

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(Above) This mosaic of images from the Surface Stereo Imager camera on NASA’s Phoenix Mars Lander shows several trenches dug by Phoenix, plus a corner of the spacecraft’s deck and the Martian arctic plain stretching to the horizon.

Favorable chemistry and episodes with thin films of liquid water during ongoing, long-term climate cycles may sometimes make the area where NASA’s Phoenix Mars mission landed last year a favorable environment for microbes.

Interpretations of data that Phoenix returned during its five months of operation on a Martian arctic plain fill four papers in this week’s edition of the journal Science, the first major peer-reviewed reports on the mission’s findings. Phoenix ended communications in November 2008 as the approach of Martian winter depleted energy from the lander’s solar panels.

“Not only did we find water ice, as expected, but the soil chemistry and minerals we observed lead us to believe this site had a wetter and warmer climate in the recent past — the last few million years — and could again in the future,” said Phoenix Principal Investigator Peter Smith of the University of Arizona, Tucson.

A paper about Phoenix water studies, for which Smith is the lead author with 36 coauthors from six nations, cites clues supporting an interpretation that the soil has had films of liquid water in the recent past. The evidence for water and potential nutrients “implies that this region could have previously met the criteria for habitability” during portions of continuing climate cycles, these authors conclude.

The mission’s biggest surprise was finding a multi-talented chemical named perchlorate in the Martian soil. This Phoenix finding caps a growing emphasis on the planet’s chemistry, said Michael Hecht of NASA’s Jet Propulsion Laboratory, Pasadena, Calif., who has 10 coauthors on a paper about Phoenix’s soluble-chemistry findings.

“The study of Mars is in transition from a follow-the-water stage to a follow-the-chemistry stage,” Hecht said. “With perchlorate, for example, we see links to atmospheric humidity, soil moisture, a possible energy source for microbes, even a possible resource for humans.”

Perchlorate, which strongly attracts water, makes up a few tenths of a percent of the composition in all three soil samples analyzed by Phoenix’s wet chemistry laboratory. It could pull humidity from the Martian air. At higher concentrations, it might combine with water as a brine that stays liquid at Martian surface temperatures. Some microbes on Earth use perchlorate as food. Human explorers might find it useful as rocket fuel or for generating oxygen.

Another surprise from Phoenix was finding ice clouds and precipitation more Earth-like than anticipated. The lander’s Canadian laser instrument for studying the atmosphere detected snow falling from clouds. In one of this week’s reports, Jim Whiteway of York University, Toronto, and 22 coauthors say that, further into winter than Phoenix operated, this precipitation would result in a seasonal buildup of water ice on and in the ground.

“Before Phoenix we did not know whether precipitation occurs on Mars,” Whiteway said. “We knew that the polar ice cap advances as far south as the Phoenix site in winter, but we did not know how the water vapor moved from the atmosphere to ice on the ground. Now we know that it does snow, and that this is part of the hydrological cycle on Mars.”

Evidence that water ice in the area sometimes thaws enough to moisten the soil comes from finding calcium carbonate in soil heated in the lander’s analytic ovens or mixed with acid in the wet chemistry laboratory. The University of Arizona’s William Boynton and 13 coauthors report that the amount of calcium carbonate “is most consistent with formation in the past by the interaction of atmospheric carbon dioxide with liquid films of water on particle surfaces.”

The new reports leave unsettled whether soil samples scooped up by Phoenix contained any carbon-based organic compounds. The perchlorate could have broken down simple organic compounds during heating of soil samples in the ovens, preventing clear detection.

The heating in ovens did not drive off any water vapor at temperatures lower than 295 degrees Celsius (563 degrees Fahrenheit), indicating the soil held no water adhering to soil particles. Climate cycles resulting from changes in the tilt and orbit of Mars on scales of hundreds of thousands of years or more could explain why effects of moist soil are present.

The Phoenix mission was led by Smith at the University of Arizona with project management at JPL and development partnership at Lockheed Martin, Denver.


Mars Spirit Test Rover Sinks into Prepared Soil

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(Above) Rover team members Colette Lohr (left) and Kim Lichtenberg (center) eye the wheels digging into the soil and Paolo Bellutta enters the next driving command.

After several days of preparing a sloped area of soft, fine soil to simulate Spirit’s current sandtrap on Mars, the rover team drove a test rover into the material on June 30, 2009. The test rover became embedded in the soil, as planned. The rover team will use this setup at NASA’s Jet Propulsion Laboratory, Pasadena, Calif., during the next few weeks to test possible extraction moves Spirit might use on Mars.

The team plans to make a few adjustments to more closely match Spirit’s situation, such as placing a rock beneath the test rover, and then intended to begin assessing possible maneuvers for Spirit to use getting free from Troy.


Mars Rover Yielding New Clues While Trapped in Place

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NASA’s Mars rover Spirit, lodged in Martian soil that is causing traction trouble, is taking advantage of the situation by learning more about the Red Planet’s environmental history.

In April, Spirit entered an area composed of three or more layers of soil with differing pastel hues hiding beneath a darker sand blanket. Scientists dubbed the site “Troy.” Spirit’s rotating wheels dug themselves more than hub deep at the site. The rover team has spent weeks studying Spirit’s situation and preparing a simulation of this Martian driving dilemma to test escape maneuvers using an engineering test rover at NASA’s Jet Propulsion Laboratory in Pasadena, Calif.

A rock seen beneath Spirit in images from the camera on the end of the rover’s arm may be touching Spirit’s belly. Scientists believe it appears to be a loose rock not bearing the rover’s weight. While Spirit awaits extraction instructions, the rover is keeping busy examining Troy, which is next to a low plateau called Home Plate, approximately 3.2 kilometers (2 miles) southeast of where Spirit landed in January 2004.

“By serendipity, Troy is one of the most interesting places Spirit has been,” said Ray Arvidson of Washington University in St. Louis. Arvidson is deputy principal investigator for the science payloads on Spirit and its twin rover, Opportunity. “We are able here to study each layer, each different color of the interesting soils exposed by the wheels.”

One of the rover’s wheels tore into the site, exposing colored sandy materials and a miniature cliff of cemented sands. Some disturbed material cascaded down, evidence of the looseness that will be a challenge for getting Spirit out. But at the edge of the disturbed patch, the soil is cohesive enough to hold its shape as a steep cross-section.

Spirit has been using tools on its robotic arm to examine tan, yellow, white and dark-red sandy soil at Troy. Stretched-color images from the panoramic camera show the tints best.

“The layers have basaltic sand, sulfate-rich sand and areas with the addition of silica-rich materials, possibly sorted by wind and cemented by the action of thin films of water. We’re still at a stage of multiple working hypotheses,” said Arvidson. “This may be evidence of much more recent processes than the formation of Home Plate…or is Home Plate being slowly stripped back by wind, and we happened to stir up a deposit from billions of years ago before the wind got to it?”

Team members from NASA’s Johnson Space Center in Houston feel initial readings suggest that iron is mostly present in an oxidized form as ferric sulfate and that some of the differences in tints at Troy observed by the panoramic camera may come from differences in the hydration states of iron sulfates.

While extraction plans for the rover are developed and tested during the coming weeks, the team plans to have Spirit further analyze the soil from different depths. This research benefits from having time and power. In April and May, winds blew away most of the dust that had accumulated on Spirit’s solar panels.

“The exceptional amount of power available from cleaning of Spirit’s solar arrays by the wind enables full use of all of the rover’s science instruments,” said Richard Moddis of the Johnson team. “If your rover is going to get bogged down, it’s nice to have it be at a location so scientifically interesting.”

The rover team has developed a soil mix for testing purposes that has physical properties similar to those of the soil under Spirit at Troy. This soil recipe combines diatomaceous earth, powdered clay and play sand. A crew is shaping a few tons of that mix this week into contours matching Troy’s. The test rover will be commanded through various combinations of maneuvers during the next few weeks to validate the safest way to proceed on Mars.

Spirit’s right-front wheel has been immobile for more than three years, magnifying the challenge. While acknowledging a possibility that Spirit might not be able to leave Troy, the rover team remains optimistic. Diagnostic tests on Spirit in early June provided encouragement that the left-middle wheel remains useable despite an earlier stall.

“With the improved power situation, we have the time to explore all the possibilities to get Spirit out,” said JPL’s John Callas, project manager for Spirit and Opportunity. “We are optimistic. The last time Spirit spun its wheels, it was still making progress. The ground testing will help us avoid doing things that could make Spirit’s situation worse.”


Mars Odyssey Alters Orbit to Study Warmer Ground

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NASA’s long-lived Mars Odyssey spacecraft has completed an eight-month adjustment of its orbit, positioning itself to look down at the day side of the planet in mid-afternoon instead of late afternoon.

This change gains sensitivity for infrared mapping of Martian minerals by the orbiter’s Thermal Emission Imaging System camera. Orbit design for Odyssey’s first seven years of observing Mars used a compromise between what worked best for the infrared mapping and for another onboard instrument.

“The orbiter is now overhead at about 3:45 in the afternoon instead of 5 p.m., so the ground is warmer and there is more thermal energy for the camera’s infrared sensors to detect,” said Jeffrey Plaut of NASA’s Jet Propulsion Laboratory, Pasadena, Calif., project scientist for Mars Odyssey.

Some important mineral discoveries by Odyssey stem from mapping done during six months early in the mission when the orbit geometry provided mid-afternoon overpasses. One key example: finding salt deposits apparently left behind when large bodies of water evaporated.

“The new orbit means we can now get the type of high-quality data for the rest of Mars that we got for 10 or 20 percent of the planet during those early six months,” said Philip Christensen of Arizona State University, Tempe, principal investigator for the Thermal Emission Imaging System.

Here’s the trade-off: The orbital shift to mid-afternoon will stop the use of one of three instruments in Odyssey’s Gamma Ray Spectrometer suite. The new orientation will soon result in overheating a critical component of the suite’s gamma ray detector. The suite’s neutron spectrometer and high-energy neutron detector are expected to keep operating. The Gamma Ray Spectrometer provided a dramatic 2002 discovery of water-ice near the Martian surface in large areas. The gamma ray detector has also mapped global distribution of many elements, such as iron, silicon and potassium.

Last year, before the start of a third two-year extension of the Odyssey mission, a panel of planetary scientists assembled by NASA recommended the orbit adjustment to maximize science benefits from the spacecraft in coming years.

Odyssey’s orbit is synchronized with the sun. Picture Mars rotating beneath the polar-orbiting spacecraft with the sun off to one side. The orbiter passes from near the north pole to near the south pole over the day-lit side of Mars. At each point on the Mars surface that turns beneath Odyssey, the solar time of day when the southbound spacecraft passes over is the same. During the five years prior to October 2008, that local solar time was about 5 p.m. whenever Odyssey was overhead. (Likewise, the local time was about 5 a.m. under the track of the spacecraft during the south-to-north leg of each orbit, on the night side of Mars.)

On Sept. 30, 2008, Odyssey fired thrusters for six minutes, putting the orbiter into a “drift” pattern of gradually changing the time-of-day of its overpasses during the next several months. On June 9, Odyssey’s operations team at JPL and at Denver-based Lockheed Martin Space Systems commanded the spacecraft to fire the thrusters again. This five-and-a-half-minute burn ended the drift pattern and locked the spacecraft into the mid-afternoon overpass time. “The maneuver went exactly as planned,” said JPL’s Gaylon McSmith, Odyssey mission manager.

In another operational change motivated by science benefits, Odyssey has begun in recent weeks making observations other then straight downward-looking. This more-flexible targeting allows imaging of some latitudes near the poles that are never directly underneath the orbiter, and allows faster filling-in of gaps not covered by previous imaging.

“We are using the spacecraft in a new way,” McSmith said.

In addition to extending its own scientific investigations, the Odyssey mission continues to serve as the radio relay for almost all data from NASA’s Mars Exploration Rovers, Spirit and Opportunity. Odyssey’s new orbital geometry helps prepare the mission to be a relay asset for NASA’s Mars Science Laboratory mission, scheduled to put the rover Curiosity on Mars in 2012.

Mars Odyssey, launched in 2001, is managed by JPL, a division of the California Institute of Technology, Pasadena, for NASA’s Science Mission Directorate, Washington. Lockheed Martin Space Systems is the prime contractor for the project. Investigators at Arizona State University operate the Thermal Emission Imaging System. Investigators at the University of Arizona, Tucson, head operation of the Gamma Ray Spectrometer. Additional science partners are located at the Russian Aviation and Space Agency, which provided the high-energy neutron detector, and at Los Alamos National Laboratories, New Mexico, which provided the neutron spectrometer.


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