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Thermal Mining of Lunar Ices - Space Resources Program · 2020. 6. 30. · •One model...

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Thermal Mining of Lunar Ices June 2020 George Sowers
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  • Thermal Mining of Lunar Ices

    June 2020

    George Sowers

  • 6/24/2020

    Agenda

    • Background

    • Ice at the lunar poles

    • From resource to reserve

    • Propellant production architecture

    • Ice extraction system

    • Proof of concept testing

    • Conclusions

    2

  • • Mounting evidence that water ice exists in large quantities near the lunar poles

    • Water has many uses for sustainable space exploration & development• Essential for all life• Oxygen for breathing air• Radiation shielding• LO2/LH2 rocket propellant

    • Use of space-sourced propellant dramatically lowers the cost of all beyond Low Earth Orbit (LEO) transportation• Enables the commercialization of cislunar space• Enables affordable Mars missions

    6/24/2020

    Background

    3

  • • Surface ice indications of up to 30wt%

    6/24/2020

    Lunar Polar Surface Ice

    Li, S, Lucey, P.G., Milliken, R.E., Hayne, P.O., Fisher, E., Williams, J.P., Hurley, D.M., Elphic, R.C., Direct evidence of surface exposed water ice in the lunar polar regions. PNAS (2018). https://doi.org/10.1073/pnas.1802345115

    4

    https://doi.org/10.1073/pnas.1802345115

  • 6/24/2020

    Developing a Proven Reserve

    CRIRSCO, Committee for Mineral Reserves International Reporting Standards, Standard Definitions, 2012.

    http://www.crirsco.com/news_items/CRIRSCO_standard_definitions_oct2012.pdf

    We are here

    Where we need to be

    5

  • 6/24/2020

    Lunar Ice Resource Exploration Roadmap2020 2021 2022 2023 2024 2025 2026 2027 2028 2029 2030 2031

    Mine dev.

    Modeling

    Ground truth mission(s)

    Cubesat & impactor swarms

    Tethered sensor lander(s)

    Rover/ sampler

    Technology development

    Full scaleindustrial

    production

    Mining HW developmentDeployment & set-up

    HW development

    Technology demonstrations

    Launch Mission Ops

    Geologic modeling & resource mapping

    Technology development

    HW development

    Launch Mission Ops

    Technology development

    HW development

    Launch Mission Ops

    Technology development

    HW development

    Launch Mission Ops 6

  • • Discrete Element Modeling initiated at both Colorado School of Mines (CSM) and University of Central Florida (UCF)

    • Initial uniform distribution of ice on lunar surface

    • Evolution through impact gardening over billions of years

    • Heterogenous distribution of ice, but stays near surface

    6/24/2020

    Lunar Polar Ice Modeling

    7

    4wt%

    UCF Model

    (10cm initial ice layer)

    CSM Model

  • • The Veritas mission concept developed by CSM to determine ground truth in a deep, cold PSR location

    • Existing CLPS lander using only battery power

    6/24/2020

    Veritas

    8

    • High TRL instruments

    • Squirrels: ejectablesensor packages with ground penetrating radar

    Instrumentation layout on LM McCandless Lander

    Squirrel ejection concept

  • 6/24/2020

    Veritas Site Selection

    9

    23 days per year line of site to Earth

  • Propellant production system

    Ice extraction system

    Capture Tent

    Cold Traps

    Secondary Optics

    Mobility systemsWater to

    propellant processing system

    Storage systemsSolar energy

    systemPower system

    Communications link

    Propellant Production System Elements

    6/24/2020

    Credit: ULA

    Sized for 1100 mT/year

    10

    Thermal Mining NIAC

    Paragon ISRU BAAOxEon Tipping PointBlue Origin Tipping

    Point

    Transformers NIAC

  • 6/24/2020

    Ice Extraction Concept

    Sublimation

    sunlight from crater rim

    Impermeable walls with reflective inner surface

    Not to scaleOptional conducting rods or heating elements

    Cold Trap

    Ice hauler

    Cold Trap

    Ice hauler

    Transparent membrane (IR reflective inner surface)

    11

    Secondary optics (mirror)

  • 6/24/2020

    Ice Extraction System in a Lunar PSR

    12

  • 6/24/2020

    Overall Process Flow

    Launch & LandDeploy &

    Set-up(re)Position

    tent & mirrors

    Collect ice in cold trap

    Transport iceto refinery

    Purification

    Heat surface with reflected

    sunlight

    ElectrolysisPropellantstorage & handling

    Active

    Passive

    Non-recurring

    Liquefaction

    13

  • 6/24/2020

    Deployment & Setup TimelineYear 1 Year 2

    Launches(Vulcan)

    Landings (XEUS)

    Heliostats

    Landing pad const.

    Processing plant

    Capture tent

    System checkout

    Production

    H #1 setup

    Crater rim

    PSR

    Landing pad construction

    H #2 setupH #3 setup

    H #1 ops

    H #2 opsH #3 ops

    Landing pad operations/launch pad construction

    setup

    setup

    Operations

    Operations

    9 launches6 landings

    Checkout

    Production

    18 month timeline: 1st launch to production

    3 PSR XEUS’s become propellant storage

    14

  • • Key parameters: Tent diameter 30m, dwell time 44hr, Tent placements 156/yr, Average ice sublimation 16.1 kg/m2, 10% vapor loss

    6/24/2020 15

    Ice Extraction Operations

    Collect iceIf ice level “full”

    detach haulerTransit to

    processing plant

    Heat & release ice

    Detach from processing plant

    Monitor ice level

    Attach to processing plant

    Transit to capture tent

    Hauler

    Attach Cold Trap

    ProcessingPlant

    All operations semi-autonomous/tele-operated from Earth

    Charge hauler

    Attach Cold trap

  • • Tent must be frequently moved to meet required annual production rate

    • Tent raises ontoskids

    • Ice haulers tow tent to adjacent location

    • Tent lowered to collection configuration

    6/24/2020 16

    Moving the Capture Tent

  • • Mud Pie• Liquid water mixed

    with regolith, then frozen

    • Water fills pore space, cements grains

    • Very hard, concrete-like

    • Granular Mix• Ice shaved and sieved

    to small grains• Mixed with dry regolith• Sand-like, porous• Various grain size

    distributions

    6/24/2020

    Icy Regolith Simulants

    Ice Regolith

    17

  • 6/24/2020

    Surface Heating of Icy Regolith Simulant

    18

    Block 1 Test ApparatusSample container: 8.25cm diameter, 6.4 cm depth

  • 6/24/2020 19

    CSM Medium Vacuum Chamber

  • 6/24/2020

    Example Sublimation Results

    20

    • 12wt% ice• Total ice sublimated vs time• Sublimation rate vs time

    Preliminary

  • • Ice extraction from surface heating inhibited by the formation of a desiccated layer at the surface• Insulating barrier

    • Vapor barrier

    • Both effects mitigated by adding conducting “straws”

    6/24/2020 21

    The Straw Concept

    0.704

    Desiccated regolith

    Unaffected icy regolith

    Heat affected icy regolith

    Straw

    Container wall

  • 6/24/2020 22

    Perforated Copper Straw

    0.704

    Post test with desiccated regolith removed

    Edge of desiccated zone

    Addition of Straw increased ice production by 2-3X

  • • Small sample and proximity of LN2 boundary limits total ice sublimated

    • No meaningful extrapolation to full scale

    • Block 2 apparatusincreases sample size 10X and moves coldboundary away from heating zone

    • Testing to begin July 2020

    6/24/2020 23

    Block 2 TestingHeat affected

    Thermal Sink – LN 77 K

    Lamp

    Desiccated

    Unaltered – 77K < T < 180 K

    Sample container Freezer

  • • Block 1 testing key results• Surface ice is rapidly sublimated• Surface heating sublimates ice within the subsurface

    • Desiccated layer at the surface grows over time• Heat affected zone at the sublimation boundary moves deeper

    over time• Thermo-physics is complex

    • Addition of straw(s) increases ice yield by 2-3X• Proximity of cold boundary artificially limits yield

    • Block 2 testing to begin July 2020• Larger sample size: 18.4cm diameter, 15.2cm depth

    • >10x volume

    • Cold boundary farther away from heating zone

    6/24/2020 24

    Preliminary Testing Conclusions

  • • Thermal modeling of icy regolith subject to surface and subsurface heating initiated in late 2017• Contract from ULA to UCF

    • Phil Metzger & Julie Brisset performed the analysis

    • Finite difference analysis, 1-d, 2-d and 3-d models• Recent 3-d results currently in peer review• Preprint results

    • Surface heating or solid subsurface heating elements• Surface heating seems more effective than just solid heating

    elements• One model configuration very similar to current Thermal Mining

    point design• 694W/m2 flux, 5wt% ice, 45hr dwell time produced 27.8 kg/m2 ice

    • This compares to 1360W/m2, 44hr dwell time for 16.1 kg/m2 ice used in the Thermal Mining point design and economic analysis

    6/24/2020 25

    Recent Analysis Results

  • • Detailed business case updated and included in NIAC report

    • Cost Update• 1100mt Propellant/yr

    • Business case scenarios• Commercial only (8.8% IRR)• Commercial Public Private Partnership (PPP) + NASA Artemis

    (15.8% IRR)• Commercial PPP + NASA Artemis + NASA Mars (15.4% IRR)

    • NASA Savings• Artemis: $470M/yr• Mars: $5200M/yr, $12B per Mars Mission

    6/24/2020 26

    Updated Business Results

    Cost Element Cost ($M)

    Development 883

    Production 614

    Launch 1,062

    Total 2,559

  • • Thermal Mining concept enhanced via Phase I NIAC study• Ice extraction system concept fleshed out• Con ops developed including deployment• Proof of concept testing validated basic Thermal Mining

    idea• Lunar ice deposition and evolution analysis shows most

    ice remains within the first meter• Thermal modeling indicates surface heating can produce

    economically viable yields• Business case analysis shows viable commercial business

    and enormous savings for NASA through public private partnership

    6/24/2020

    Conclusions

    27


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