Mars Science Laboratory Mission and Science Investigation

AbstractScheduled to land in August of 2012, the Mars Science Laboratory (MSL) Mission was initiated to explore the habitability of Mars. This includes both modern environments as well as ancient environments recorded by the stratigraphic rock record preserved at the Gale crater landing site. The Curiosity rover has a designed lifetime of at least one Mars year (∼23 months), and drive capability of at least 20 km. Curiosity’s science payload was specifically assembled to assess habitability and includes a gas chromatograph-mass spectrometer and gas analyzer that will search for organic carbon in rocks, regolith fines, and the atmosphere (SAM instrument); an x-ray diffractometer that will determine mineralogical diversity (CheMin instrument); focusable cameras that can image landscapes and rock/regolith textures in natural color (MAHLI, MARDI, and Mastcam instruments); an alpha-particle x-ray spectrometer for in situ determination of rock and soil chemistry (APXS instrument); a laser-induced breakdown spectrometer to remotely sense the chemical composition of rocks and minerals (ChemCam instrument); an active neutron spectrometer designed to search for water in rocks/regolith (DAN instrument); a weather station to measure modern-day environmental variables (REMS instrument); and a sensor designed for continuous monitoring of background solar and cosmic radiation (RAD instrument). The various payload elements will work together to detect and study potential sampling targets with remote and in situ measurements; to acquire samples of rock, soil, and atmosphere and analyze them in onboard analytical instruments; and to observe the environment around the rover.The 155-km diameter Gale crater was chosen as Curiosity’s field site based on several attributes: an interior mountain of ancient flat-lying strata extending almost 5 km above the elevation of the landing site; the lower few hundred meters of the mountain show a progression with relative age from clay-bearing to sulfate-bearing strata, separated by an unconformity from overlying likely anhydrous strata; the landing ellipse is characterized by a mixture of alluvial fan and high thermal inertia/high albedo stratified deposits; and a number of stratigraphically/geomorphically distinct fluvial features. Samples of the crater wall and rim rock, and more recent to currently active surface materials also may be studied. Gale has a well-defined regional context and strong evidence for a progression through multiple potentially habitable environments. These environments are represented by a stratigraphic record of extraordinary extent, and insure preservation of a rich record of the environmental history of early Mars. The interior mountain of Gale Crater has been informally designated at Mount Sharp, in honor of the pioneering planetary scientist Robert Sharp.The major subsystems of the MSL Project consist of a single rover (with science payload), a Multi-Mission Radioisotope Thermoelectric Generator, an Earth-Mars cruise stage, an entry, descent, and landing system, a launch vehicle, and the mission operations and ground data systems. The primary communication path for downlink is relay through the Mars Reconnaissance Orbiter. The primary path for uplink to the rover is Direct-from-Earth. The secondary paths for downlink are Direct-to-Earth and relay through the Mars Odyssey orbiter. Curiosity is a scaled version of the 6-wheel drive, 4-wheel steering, rocker bogie system from the Mars Exploration Rovers (MER) Spirit and Opportunity and the Mars Pathfinder Sojourner. Like Spirit and Opportunity, Curiosity offers three primary modes of navigation: blind-drive, visual odometry, and visual odometry with hazard avoidance. Creation of terrain maps based on HiRISE (High Resolution Imaging Science Experiment) and other remote sensing data were used to conduct simulated driving with Curiosity in these various modes, and allowed selection of the Gale crater landing site which requires climbing the base of a mountain to achieve its primary science goals.The Sample Acquisition, Processing, and Handling (SA/SPaH) subsystem is responsible for the acquisition of rock and soil samples from the Martian surface and the processing of these samples into fine particles that are then distributed to the analytical science instruments. The SA/SPaH subsystem is also responsible for the placement of the two contact instruments (APXS, MAHLI) on rock and soil targets. SA/SPaH consists of a robotic arm and turret-mounted devices on the end of the arm, which include a drill, brush, soil scoop, sample processing device, and the mechanical and electrical interfaces to the two contact science instruments. SA/SPaH also includes drill bit boxes, the organic check material, and an observation tray, which are all mounted on the front of the rover, and inlet cover mechanisms that are placed over the SAM and CheMin solid sample inlet tubes on the rover top deck.

[1]  E. Opik,et al.  The Martian Surface , 1966, Science.

[2]  A. Turkevich,et al.  Determination of the chemical composition of Martian soil and rocks: The alpha proton X ray spectrometer , 1997 .

[3]  M. Malin,et al.  Sedimentary rocks of early Mars. , 2000, Science.

[4]  D. D. Marais Isotopic Evolution of the Biogeochemical Carbon Cycle During the Precambrian , 2001 .

[5]  M. Malin,et al.  Martian sedimentary rock stratigraphy: Outcrops and interbedded craters of northwest Sinus Meridiani and southwest Arabia Terra , 2002 .

[6]  A. Knoll The geological consequences of evolution , 2003 .

[7]  M. Klimesh,et al.  Mars Exploration Rover engineering cameras , 2003 .

[8]  Kenneth S Edgett,et al.  Evidence for Persistent Flow and Aqueous Sedimentation on Early Mars , 2003, Science.

[9]  Steven W. Squyres,et al.  The new Athena alpha particle X‐ray spectrometer for the Mars Exploration Rovers , 2003 .

[10]  Christopher P. McKay,et al.  Mars-Like Soils in the Atacama Desert, Chile, and the Dry Limit of Microbial Life , 2003, Science.

[11]  D. Sumner Poor preservation potential of organics in Meridiani Planum hematite-bearing sedimentary rocks , 2004 .

[12]  R. E. Arvidson,et al.  Phyllosilicates on Mars and implications for early martian climate , 2005, Nature.

[13]  J. Moore,et al.  Large alluvial fans on Mars , 2005 .

[14]  Donald M. Hunten,et al.  Possible oxidant sources in the atmosphere and surface of Mars , 1979, Journal of Molecular Evolution.

[15]  D.S. Bass,et al.  Choosing Mars time: analysis of the Mars Exploration Rover experience , 2005, 2005 IEEE Aerospace Conference.

[16]  Andrew H. Mishkin,et al.  Working the Martian night shift - the MER surface operations process , 2006, IEEE Robotics & Automation Magazine.

[17]  Steven W. Squyres,et al.  Alpha Particle X‐Ray Spectrometer (APXS): Results from Gusev crater and calibration report , 2006 .

[18]  S. Squyres,et al.  Mineralogy of the light-toned outcrop at Meridiani Planum as seen by the Miniature Thermal Emission Spectrometer and implications for its formation , 2006 .

[19]  Paul R. Mahaffy,et al.  Methane and related trace species on Mars: Origin, loss, implications for life, and habitability , 2007 .

[20]  Therese Errigo,et al.  Mitigation of the impact of terrestrial contamination on organic measurements from the Mars Science Laboratory. , 2006, Astrobiology.

[21]  S. McLennan,et al.  The Martian Surface: The sedimentary rock cycle of Mars , 2008 .

[22]  Hazen,et al.  Review Paper. Mineral evolution , 2008 .

[23]  A. Chen,et al.  Mars Science Laboratory Entry, Descent, and Landing System Overview , 2008, 2008 IEEE Aerospace Conference.

[24]  John F. Mustard,et al.  Clay minerals in delta deposits and organic preservation potential on Mars , 2008 .

[25]  S. I. Bragin,et al.  The Dynamic Albedo of Neutrons (DAN) experiment for NASA's 2009 Mars Science Laboratory. , 2008, Astrobiology.

[26]  D. Ming,et al.  Geochemical properties of rocks and soils in Gusev Crater, Mars: Results of the Alpha Particle X-Ray Spectrometer from Cumberland Ridge to Home Plate , 2008 .

[27]  N. Izenberg,et al.  Hydrated silicate minerals on Mars observed by the Mars Reconnaissance Orbiter CRISM instrument , 2008, Nature.

[28]  James F. Bell,et al.  Geologic mapping and characterization of Gale Crater and implications for its potential as a Mars Science Laboratory landing site , 2009 .

[29]  Michael D. Smith,et al.  Strong Release of Methane on Mars in Northern Summer 2003 , 2009, Science.

[30]  Eduardo Sebastián,et al.  Pyrometer model based on sensor physical structure and thermal operation , 2010 .

[31]  ChemCam LIBS Instrument: Complete Characterization of the Onboard Calibration Silicate Targets (MSL Rover) , 2010 .

[32]  F. Abilleira 2011 Mars Science Laboratory Mission Design Overview , 2010 .

[33]  M. Bourke,et al.  Aeolian processes and dune morphology in Gale Crater , 2010 .

[34]  J. Grotzinger,et al.  Paleoclimate of Mars as captured by the stratigraphic record in Gale Crater , 2010 .

[35]  Dawn Y Sumner,et al.  Preservation of martian organic and environmental records: final report of the Mars biosignature working group. , 2011, Astrobiology.

[36]  Moderator Christopher P McKay,et al.  The next phase in our search for life: an expert discussion. , 2011, Astrobiology.

[37]  Simon J. Hook,et al.  Constraints on the origin and evolution of the layered mound in Gale Crater, Mars using Mars Reconnaissance Orbiter data , 2011 .

[38]  G. Reitz,et al.  The Radiation Assessment Detector (RAD) Investigation , 2012 .

[39]  Reg G. Willson,et al.  Curiosity’s Mars Hand Lens Imager (MAHLI) Investigation , 2012 .

[40]  J. M. Rhodes,et al.  Ceramic ChemCam Calibration Targets on Mars Science Laboratory , 2012 .

[41]  N. Bridges,et al.  The ChemCam Instrument Suite on the Mars Science Laboratory (MSL) Rover: Body Unit and Combined System Tests , 2012 .

[42]  M. Watkins,et al.  Selection of the Mars Science Laboratory Landing Site , 2012 .

[43]  Ashwin R. Vasavada,et al.  Assessment of Environments for Mars Science Laboratory Entry, Descent, and Surface Operations , 2012 .

[44]  E. Sebastián,et al.  REMS: The Environmental Sensor Suite for the Mars Science Laboratory Rover , 2012 .

[45]  D. Ming,et al.  The Sample Analysis at Mars Investigation and Instrument Suite , 2012 .

[46]  M. Golombek,et al.  Surface Properties of the Mars Science Laboratory Candidate Landing Sites: Characterization from Orbit and Predictions , 2012 .

[47]  M. Saccoccio,et al.  The ChemCam Instrument Suite on the Mars Science Laboratory (MSL) Rover: Science Objectives and Mast Unit Description , 2012 .

[48]  J. Grotzinger,et al.  The Sedimentary Rock Record of Mars: Distribution, Origins, and Global Stratigraphy , 2012 .

[49]  R. Gellert,et al.  Calibration of the Mars Science Laboratory Alpha Particle X-ray Spectrometer , 2012 .

[50]  Hongwei Ma,et al.  Characterization and Calibration of the CheMin Mineralogical Instrument on Mars Science Laboratory , 2012 .

[51]  P. Conrad,et al.  The Mars Science Laboratory Organic Check Material , 2012 .

[52]  John P. Grotzinger,et al.  Sedimentary geology of mars , 2012 .

[53]  Justin N. Maki,et al.  The Mars Science Laboratory Engineering Cameras , 2012 .

[54]  Luther W. Beegle,et al.  Collecting Samples in Gale Crater, Mars; an Overview of the Mars Science Laboratory Sample Acquisition, Sample Processing and Handling System , 2012 .