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
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• 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
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Background
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• Surface ice indications of up to 30wt%
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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
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https://doi.org/10.1073/pnas.1802345115
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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
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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
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Lunar Polar Ice Modeling
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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
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Veritas
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• High TRL instruments
• Squirrels: ejectablesensor packages with ground penetrating radar
Instrumentation layout on LM McCandless Lander
Squirrel ejection concept
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Veritas Site Selection
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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
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Credit: ULA
Sized for 1100 mT/year
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Thermal Mining NIAC
Paragon ISRU BAAOxEon Tipping PointBlue Origin Tipping
Point
Transformers NIAC
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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)
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Secondary optics (mirror)
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Ice Extraction System in a Lunar PSR
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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
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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
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• Key parameters: Tent diameter 30m, dwell time 44hr, Tent placements 156/yr, Average ice sublimation 16.1 kg/m2, 10% vapor loss
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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
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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
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Icy Regolith Simulants
Ice Regolith
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Surface Heating of Icy Regolith Simulant
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Block 1 Test ApparatusSample container: 8.25cm diameter, 6.4 cm depth
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CSM Medium Vacuum Chamber
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Example Sublimation Results
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• 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”
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The Straw Concept
0.704
Desiccated regolith
Unaffected icy regolith
Heat affected icy regolith
Straw
Container wall
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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
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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
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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
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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, $12B per Mars Mission
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Updated Business Results
Cost Element Cost ($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
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Conclusions
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