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    R.D. Frederick 200

    Martian Cave UtilizationMartian Cave Utilization

    System Feasibility DemonstrationsSystem Feasibility Demonstrations&&

    Scientific Exploration TechnologiesScientific Exploration Technologies

    P.J. BostonP.J. BostonCSR, Inc.CSR, Inc.

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    Living on Mars:Living on Mars:

    The Surface ParadigmThe Surface ParadigmWhy is this not such a good idea?Why is this not such a good idea? Radiation shielding problemsRadiation shielding problems Payload mass intensivePayload mass intensive

    No obvious access to resourcesNo obvious access to resources No protection from dust stormsNo protection from dust storms No protection from meteorite impactsNo protection from meteorite impacts

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    P.J . BostonP.J . BostonP.J . BostonP.J . Boston 2001200120012001

    Living on Mars:Living on Mars:

    The Subsurface ParadigmThe Subsurface ParadigmWhy is this such a GREAT idea?Why is this such a GREAT idea?

    Radiation shieldingRadiation shielding Natural pressure vesselNatural pressure vessel Potential access to many resourcesPotential access to many resources Closer access to subsurface drillingCloser access to subsurface drilling Protection from dust stormsProtection from dust storms Protection from meteorite impactsProtection from meteorite impacts

    High scientific value: geology, biology, etc.High scientific value: geology, biology, etc.

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    Mars Lava TubesMars Lava Tubes

    JumboJumbo--sizedsized

    NumerousNumerous

    ClearlyClearly visiblevisible

    AlbaAlba PateraPatera

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    GardenGarden--varietyvariety

    Earth Lava TubeEarth Lava Tube

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    (After Macdonald, 1965)

    Rift Tube Serial Flows

    Trapped

    Ice Lenses

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    Lava Tubes are often smooth!Lava Tubes are often smooth!

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    Desert SurfacesDesert Surfaces

    On EarthOn Earth

    High intensity sunlight and UVHigh intensity sunlight and UV

    Low humidity (5Low humidity (5--40% typically)40% typically)

    Temperature extremesTemperature extremes

    Low nutrients (usually)Low nutrients (usually)

    MineralMineral--rich (usually)rich (usually)

    Extensive weatherExtensive weather,,e.g. high winds, flash floods, frost, etc.e.g. high winds, flash floods, frost, etc.

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    Photo by DavidPhoto by David JagnowJagnow

    Desert CavesDesert Caves

    On EarthOn Earth

    No sunlightNo sunlight

    High humidity (99High humidity (99--100%)100%)

    Temperatures relativelyTemperatures relativelyconstantconstant

    Low nutrients (usually)Low nutrients (usually) MineralMineral--rich (usually)rich (usually)

    No weatherNo weather

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    Cozy!Cozy!

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    Limestone CavesLimestone Caves

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    TafonatedTafonated CavesCaves

    Typically in sandstonesTypically in sandstones Desert environmentsDesert environments

    thermal weatheringthermal weatheringaeolianaeolian weatheringweathering

    Seacoast water erosioSeacoast water erosion

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    Big enough for Teddy BearsBig enough for Teddy Bears

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    Big enough for HumansBig enough for Humans

    From inside.From inside.

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    SpallingSpalling CavesCaves

    Beginning to formBeginning to form

    AmphitheaterAmphitheater--sizedsized

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    Photo by Kathy DuchenePhoto by Kathy Duchene

    Photo by L. HosPhoto by L. Hose

    Mineral ResourcesMineral Resources

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    Water on Mars:Water on Mars:Known SourcesKnown Sources

    Atmosphere is saturated at global meanAtmosphere is saturated at global mean

    pressure of 8.1pressure of 8.1 millibarsmillibars

    WaterWater vapourvapour = 0.03% of current= 0.03% of currentatmosphere (~1atmosphere (~1--3% for Earth)3% for Earth)

    Water ice at north poleWater ice at north poleWater and COWater and CO22 ice at south poleice at south pole

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    Recent Surface Water EvidenceRecent Surface Water Evidence

    When? Yesterday to a few million years agoWhen? Yesterday to a few million years ago

    How deep? 100How deep? 100--400 m (300400 m (300--1300 ft)1300 ft)

    How much? 2500 cubic m, about (90,000 cubic ft.How much? 2500 cubic m, about (90,000 cubic ft. Where? 30Where? 30oo--7070oo

    Most in the south, a few in the northern hemisphereMost in the south, a few in the northern hemisphere

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    ProposedProposedMechanismsMechanisms

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    Material on MarsMaterial on Mars

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    Material in UtahMaterial in Utah

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    Mars Polar Ice/Dust Caves?Mars Polar Ice/Dust Caves?

    IcelandIceland

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    IceIce

    ParticlesParticles

    Organics?Organics?

    Microbes?Microbes?

    Lava tube formsLava tube formsCondensationCondensation

    RainRain

    GroundwaterGroundwater

    PermanentPermanent

    Cave Ice LakesCave Ice Lakes

    Tubeneckcollapse

    sTubenec

    kcollapses

    Basalticinsu

    lation

    Basalticinsu

    lation

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    R.D. Frederick 2001

    The Perfect Building SiteThe Perfect Building Site

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    R.D. Frederick 2001R.D. Frederick 2001

    RoboticRoboticCaveCave ExlorationExloration

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    R.D. Frederick 2001

    Location and MappingLocation and Mapping

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    InIn--cave Locationcave Location

    and Mappingand Mapping

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    AccessAccess

    R.D. Frederick 2001R.D. Frederick 2001

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    Operational ProtocolsOperational Protocols

    R.D. Frederick 2002R.D. Frederick 2002

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    InflatablesInflatables & Liners& Liners

    R.D. Frederick 2002R.D. Frederick 2002

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    R.D. Frederick 2002R.D. Frederick 2002

    Novel Airlock TechnologyNovel Airlock Technology

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    Image ValImage Val HildrethHildreth--WerkerWerker

    MarsMars--derived Breathing Mixesderived Breathing Mixes

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    Mouse MissionMouse Mission

    to Inner Spaceto Inner Space

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    Controlled EcologicalControlled EcologicalMouse SupportMouse Support

    SystemSystem

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    MATERIAL RESOURCESMATERIAL RESOURCES

    The AtmosphereThe AtmosphereMARSMARS EARTHEARTH

    COCO22 95%95% 0.03%0.03%

    (10 Bars(10 Bars outgassedoutgassed))NN22 2.7%2.7% 78%78%

    ArgonArgon 1.6%1.6% 0.93%0.93%

    OO22 0.13%0.13% 20.9%20.9%

    COCO 0.07%0.07% 0.12ppm0.12ppm

    NeonNeon

    KryptonKrypton ppmppm on both planetson both planets

    XenonXenon

    MM d i dd i d

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    MarsMars--derivedderivedBreathing MixesBreathing Mixes

    40% N240% N240%40%ArgonArgon

    20% O220% O2

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    Mouse Mission to Inner SpaceMouse Mission to Inner SpaceVersion 1 in testingVersion 1 in testingVersion 2 under constructionVersion 2 under constructionDuckweed experiments advancedDuckweed experiments advancedLighting for plants in design and planningLighting for plants in design and planningBreathing mixture experiments beginningBreathing mixture experiments beginningGas balance, water & waste recycling in designGas balance, water & waste recycling in designCave selection continuesCave selection continues

    Progress SummaryProgress Summary

    Human Mission to Inner SpaceHuman Mission to Inner SpaceInflatablesInflatables in designin design

    Airlock in designAirlock in designIn cave communication system in designIn cave communication system in designAccess via suitsAccess via suits HOPING FOR HELP!!!!!HOPING FOR HELP!!!!!Operational protocols developing in realOperational protocols developing in real--timetimeLighting system in prototypeLighting system in prototype

    Cave selection narrowed to 3Cave selection narrowed to 3

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    Humans in Caves:Humans in Caves:The PastThe Past

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    Humans in Caves:Humans in Caves:The PresentThe Present

    Humans in Caves:Humans in Caves:The Future?The Future?

    Other Collaborators:Other Collaborators: Illustrations:Illustrations:

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    Thanks, NIAC!Thanks, NIAC!

    Other Collaborators:Other Collaborators:U. New Mexico SLIME TeamU. New Mexico SLIME Team

    EquinoxEquinox InterscienceInterscience, Denver, CO, Denver, COInstitute ofInstitute of MeteoriticsMeteoritics, UNM, UNM

    USDA Forest ServiceUSDA Forest Service

    The Mars SocietyThe Mars Society

    Illustrations:Illustrations:Gus (R.D.) FrederickGus (R.D.) FrederickSlawek WojtowiczSlawek WojtowiczHajimeHajime SorayamaSorayama

    Additional Support:Additional Support:NSF Life in Extreme Environments ProgramNSF Life in Extreme Environments Program

    National Geographic SocietyNational Geographic Society

    National Speleological SocietyNational Speleological SocietyN b lNASA A bi l I i