Curiosity Self Portrait from NASA site |
On August 6th 2012 at 1:32 am (eastern time) the rover
Curiosity, a large mobile laboratory, was set down on Mars inside the Gale
Crater by NASA’s Mars Science Laboratory, MSL, beginning a two-year
investigation of Mars, the Red Planet. The rover was designed to analyze samples
scooped from the soil and drilled from rocks. The record of the planet's
climate and geology is essentially "written in the rocks and soil" --
in their formation, structure, and chemical composition and this Mars mission
is designed to unveil some of those secrets. The rover's on-board laboratory
will study rocks, soils, and the local geologic setting in order to detect
forms of carbon, the chemical building blocks of life on Mars. Curiosity
carries a radioisotope power system that generates electricity from the heat of
plutonium's radioactive decay. This power source gives the mission an operating
lifespan on Mars' surface of a full Martian year (687 Earth days) or more and
hopefully be able to gather enough data to assess what the Martian environment
was like in the past.
For about three weeks NASA scientists put Curiosity
through its paces, testing its equipment and upgrading its software to the
exploration software. According to Ben Cichy chief software engineer for the
Mars Science Laboratory mission. The flight software for Curiosity was focused on
landing the vehicle. It included many capabilities that were no longer needed
once Curiosity was down, and contained only basic surface operation capabilities,
so the software was upgraded. Once the Curiosity rover was checked out and
ready to go the rover began it eastward trek toward Mount Sharp, a mountain
about 3 miles (5 kilometers) tall. The rover is conducting experiments along
the way, seeking clues in the rocks and soil that would indicate whether Mars
ever was capable of supporting microbial life. It is taking and sharing
pictures of the trip and using the Foursquare application.
The first Martian rock NASA's Curiosity rover
investigated was found to be a close match in chemical composition to an
unusual but well-known type of igneous rock found in many volcanic provinces on
Earth according to Edward Stolper of the California Institute of Technology in
Pasadena, Calif., who is working with the Curiosity team. On Earth, rocks with this
composition typically come from the planet's mantle beneath the crust, from
crystallization of relatively water-rich magma at elevated pressure and hints of a Mars past when there was water on the plant.
A set of instruments aboard the have analyzed samples of
the atmosphere collected near the "Rocknest" site in Gale Crater
where the rover stopped for research. Findings from the Sample Analysis at Mars
(SAM) instruments found an increase of 5
% in heavier isotopes of carbon in the
atmospheric carbon dioxide compared to scientists’ estimates of the isotopic
ratios present when Mars formed. These enriched ratios of heavier isotopes to
lighter ones suggest the top of the atmosphere may have been lost to
interplanetary space. Losses at the top of the atmosphere would deplete lighter
isotopes. Isotopes of argon also show enrichment of the heavy isotope, matching
previous estimates of atmosphere composition derived from studies of Martian
meteorites on Earth.
Scientists theorize that in Mars' distant past its
environment may have been quite different, with persistent water and a thicker
atmosphere. NASA's Mars Atmosphere and Volatile Evolution, or MAVEN, mission
will investigate possible losses from the upper atmosphere when it arrives at
Mars in 2014. The Opportunity rover that landed in 2004 is still operational in the southern hemisphere of Mars. The Spirit rover also landed in 2004 stopped communicating with NASA in 2010. Previous work on Mars found water carved channels and sediments that was once carried by water to form fans and deltas
within lake basins. Recent small craters discovered by the High Resolution
Imaging Science Experiment camera on NASA's Mars Reconnaissance Orbiter expose
buried ice in the middle latitudes of Mars. This ice is a record of past
climate change. Not stable today, it was deposited during a period of different
obliquity, or tilt, of the planet's axis.
So far Curiosity has traveled 0.42 mile (677 meters)
since Curiosity's landing stopping ever few meters to take samples and test rocks.
The Curiosity rover is parked for the holidays but continues testing the
Martian environment from its holiday location within Yellowknife Bay. The
mission's plans for most of 2013 center on driving toward the primary mission
destination, the 3-mile-high (5-kilometer) layered mound we are calling Mount Sharp to
determine if areas within the Gale Crater and specifically Mount Sharp ever
were a habitable environment for microbes. The mission, like all the Mars
missions is slow going. It is now
expected that the trek to Mount Sharp will not begin until end of January or
early February.
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