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NRC Planetary Science Decadal Survey

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Title: NRC Planetary Science Decadal Survey


1
NRC Planetary Science Decadal Survey
  • Wendy Calvin
  • Prof. Geological Sci Eng,
  • University of Nevada - Reno
  • Vice-Chair Mars Sub-Panel

for Western Space Grant Directors Meeting DRI,
18.Sept.09
2
Decadal Surveys
  • Chartered by NASA, but provided by NRC as
    advisory arm of the NAS.
  • Independent assessment of scientific priorities
    in a given area.
  • Earth Science just completed (2007).
  • Astronomy/Astrophysics and Planetary currently
    underway.
  • Identify and Prioritize flight investigations
    believed to be gt 450M life cycle cost.
  • Include infrastructure, RA, education,
    technology

3
New Frontiers in the Solar System (2003)
  • Fundamental Science Questions
  • 1st Billion Years of Solar System History
  • Volatiles and Organics stuff of life
  • Origin and Evolution of Habitable Worlds
  • How Planetary Systems Work
  • Example Recommended Missions
  • Europa Geophysical Explorer
  • Venus In-Situ
  • Jupiter Polar Orbiter
  • S. Pole Aiken (Lunar) Sample Return
  • Mars Network
  • Mars Sample Return

4
Planetary Science 2013-2022
  • Overview of planetary science.
  • Survey the state of knowledge, recent
    discoveries.
  • Inventory top-level science questions that guide
    flight missions.
  • Small (Discovery), Medium (New Frontiers), Large
    (Flagship) mission classes.
  • (New) priorities for Mars and Earths Moon to be
    integrated with the rest of the Solar System.
  • (New) assessment and cost modeling of flight
    concepts.
  • (New) Astrobiology included in sub panels rather
    than separate sub-panel.

5
Committee Structure
  • Steering Committee (Squyres, Soderblom)
  • Vice-Chair of each sub panel (5)
  • 9 others not affiliated with any subpanel
  • Sub-Panels
  • Primitive Bodies (Asteroids, Comets, KBOs,
    Meteorites, IDPs)
  • Inner Planets (Mercury, Venus, Moon)
  • Mars
  • Giant Planets (JSUN, exoplanets, rings, fields)
  • Satellites (Europa, Ganymede, Titan Enceladus,
    and many, many others)

http//sites.nationalacademies.org/SSB/CurrentProj
ects/ssb_052412
6
Mars Panel
  • 13 Members
  • Represent science from core to atmosphere
  • Strategic missions and design well-considered
    through MEPAG community process.
  • Goals and Objectives Living Document
  • Life, Climate, Geology/Geophysics, Human
    Exploration
  • Plans for 2016, 2018 Missions relatively stable
  • 2016 Trace Gas Orbiter, 2018 Rover (Astrobio)
  • International collaboration developing
  • Exo-Mars, Mars Sample Return
  • Just had 1st meeting, briefings from MEPAG
    community and mission studies.
  • Community white papers just delivered.

7
Process/Timeline
  • Sub panels meet, gather information, propose
    missions for study.
  • Include White papers from community
  • Each sub-panel has 2 meetings between Aug-Nov
    2009
  • Steering committee prioritizes input from
    sub-panels into cross-solar system themes and
    goals.
  • Strive for consensus and community ownership
  • Fit within current budget constraints
  • Draft document from sub panels Spring 2010
  • Draft full report Fall/Winter 2010
  • External review and release of final report
    summer 2011.

8
2003 Mars Themes / Key Questions
  • Mars as a potential abode of life
  • Does/Did life exist, how habitable?
  • Water, atmosphere, and climate
  • Sources, sinks, volatile reservoirs
  • Atm evolution, dynamics, atm escape
  • 3D distribution of water in the crust
  • Structure and evolution of Mars
  • Rock types, origin of crustal magnetism
  • Internal structure, core dynamo
  • Chronology, oxidation with depth

9
Why Mars?
  1. Mars offers crucial information about the early
    evolution, internal structure, and origin of the
    terrestrial planets, including Earth.
  2. Timeframe for evolution of life on Earth is
    largely absent from the rock record, but this era
    is preserved on Mars.
  3. Mars provides a means to approach, and possibly
    answer, origin and evolution of life questions.
  4. Excellent opportunity to investigate short- and
    long-term climate change.
  5. Mars science has benefitted from a focused,
    dedicated program of exploration.

10
MEPAn Integrated Set of ActivitiesCreating a
True Program Structure
Year of Launch
2007
2001
2003
2005
1996
2011
2013
Mars Reconnaissance Orbiter
MAVEN
Mars Global Surveyor
Mars Odyssey
Curiosity
Opportunity
Phoenix
Spirit
Mars Pathfinder
Strategic, Core Missions
Competitive PI-Led Missions
10
11
Last Decade Discoveries Diverse Planet with
Complex History
  • Mars has areas with diverse mineralogy, including
    alteration by water, with a change in mineralogy
    over time and spatial diversity of environments.
  • In situ confirmation of increased water activity
    in the past.
  • Pervasive water ice in globally distributed,
    near-surface reservoirs.
  • Sources, phase changes, and transport of
    volatiles (H2O, CO2) are known some are
    quantified.
  • Increasing evidence for geologically recent
    climate change.
  • Dynamic change occurring even today landslides,
    new gullies, new impact craters, changing ice
    cover.
  • Presence of methane indicative of active
    chemical processes either biogenic or abiotic.
  • Based on much of the above, the perception of
    Potential for past Life has increased, and Modern
    Life may still be possible.

12
Last Decade Discoveries Diversity of
Environments
PHX
  • Chemistry and morphology indicate changing
    environments throughout geologic history
  • Acidic waters at Meridiani
  • Basic waters at Phoenix landing site
  • Mineralogy clays to sulfates to oxides

MER
Steno
MRO
Smith
Lyell
Gilbert area
Victoria Crater
-12
Hesperian subsurface water, diagenesis
13
Past Decadal Results Wide variety of
sedimentary deposits
Delta, showing phyllosilicate layers
Melas Chasma
MRO
Meridiani
MER
MRO
Large-scale sedimentary structures
  • Depositional processes created a sedimentary
    record
  • Developed in topographically low areas
  • Spectacular stratification at multiple scales
  • Evidence of persistent standing water, lakes
  • Sediments systematically change in character with
    time
  • Multiple facies recognized

Eberswalde Delta
Fine-scale sedimentary structures
-13
14
Past Decadal Results Distribution of Modern
Water
Global Near-Surface Reservoirs of Water
ODY
  • Gamma Ray Spectrometer
  • Global hydrogen abundance and equivalent H2O
  • Ground ice to /-60 in high abundance

Phoenix results
PHX
  • SHARAD and MARSIS
  • Nearly pure water ice
  • Distinct layering
  • No deflection of crust
  • Ice-cored lobate debris aprons in mid-latitudes

MRO MEX
-14
15
Past Decadal Results Periodic Climate Change
  • Volatile-rich, latitude dependent deposits
    (mantle, glaciers, gullies, viscous flow) coupled
    to orbitally-forced climate change
  • Periodicity of layering in the north polar cap
    deposits as well as sedimentary deposits

MGS, ODY, MEX MRO
16
Past Decadal Results Modern Methane
courtesy Mark Allen
NAI, RA
Courtesy Mike Mumma
NAI
Detection of Methane on Mars
MEX NAI RA
Abiotic?
Biotic?
Evidence of an active subsurface?
courtesy Lisa Pratt
17
Past Decadal Results Mars Planetary Evolution
  • Hydrous Mineralogy Changed Over Time
  • Phyllosilicate minerals (smectite clay, chlorite,
    kaolinite) formed early
  • Evaporates dominated by sulfate formed later with
    opal/hydrated silica
  • Few hydrated mineral deposits since
  • Evolution of Aqueous, Fluvial and Glacial,
    Morphology with Time
  • Valley networks, lake systems
  • Gullies
  • Viscous flow, glaciers, latitude dependant mantle

acidic
Neutral pH
Sulfates
Anhydrous Ferric Oxides
Clays
18
Questions for the Next Decade
  • Integrating the MEPAG science priorities and the
    programmatic factors, these specific questions
    are highest priority for the next decade.
  • What is the diversity and nature of aqueous
    geologic environments? (Goal I, II, III--MSL will
    contribute)
  • What is the detailed mineralogy of the diverse
    suite of geologic units and what are their
    absolute ages? (Goal II, III)
  • Are reduced carbon compounds preserved and, if
    so, in what geologic environments? (Goal I--MSL
    may contribute)
  • What is the complement of trace gases in the
    atmosphere and what are the processes that govern
    their origin, evolution, and fate? (Goal I, II,
    III)
  • How does the planet interact with the space
    environment, and how has that affected its
    evolution? (Goal IIaddressed by MAVEN mission)
  • What is the record of climate change over the
    past 10, 100, and 1000 Myrs? (Goal II, III)
  • What is the internal structure and activity?
    (Goal III)
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