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Martian Cave Utilization 
System Feasibility Demonstrations 
R.D. Frederick © 2001 
& 
Scientific Exploration Technologies 
P.J. Boston 
CSR, Inc.
Living on Mars: 
The Surface Paradigm 
Why is this not such a good idea? 
•• Radiation shielding problems 
•• Payload mass intensive 
•• No obvious access to resources 
•• No protection from dust storms 
•• No protection from meteorite impacts
Living on Mars: 
The Subsurface Paradigm 
P.J. Boston © 2001 
Why is this such a GREAT idea? 
•• Radiation shielding 
•• Natural pressure vessel 
•• Potential access to many resources 
•• Closer access to subsurface drilling 
•• Protection from dust storms 
•• Protection from meteorite impacts 
•• High scientific value: geology, biology, etc.
Mars Lava Tubes 
•• Jumbo-sized 
•• Numerous 
•• Clearly visible 
Alba Patera
Garden-variety 
Earth Lava Tube
Rift Tube Serial Flows 
(After Macdonald, 1965) 
Trapped 
Ice Lenses
Lava Tubes are often smooth!
Desert Surfaces 
On Earth 
•• High intensity sunlight and UV 
•• Low humidity (5-40% typically) 
•• Temperature extremes 
•• Low nutrients (usually) 
•• Mineral-rich (usually) 
•• Extensive weather, 
e.g. high winds, flash floods, frost, etc.
Desert Caves 
On Earth 
•• No sunlight 
•• High humidity (99-100%) 
•• Temperatures relatively 
Photo by David Jagnow 
constant 
•• Low nutrients (usually) 
•• Mineral-rich (usually) 
•• No weather
Cozy!
Limestone Caves
Tafonated Caves 
•• Typically in sandstones 
•• Desert environments 
thermal weathering 
aeolian weathering 
•• Seacoast water erosion
Big enough for Teddy Bears……
Big enough for Humans…… 
From inside…….
Spalling Caves 
Beginning to form 
Amphitheater-sized……
Photo by L. Hose 
Photo by Kathy Duchene 
Mineral Resources
Water on Mars: 
Known Sources 
••Atmosphere is saturated at global mean 
pressure of 8.1 millibars 
••Water vapour = 0.03% of current 
atmosphere (~1-3% for Earth) 
••Water ice at north pole 
••Water and CO2 ice at south pole
Recent Surface Water Evidence 
•• When? Yesterday to a few million years ago 
•• How deep? 100-400 m (300-1300 ft) 
•• How much? 2500 cubic m, about (90,000 cubic ft. 
•• Where? 30o-70o 
Most in the south, a few in the northern hemisphere
Proposed 
Mechanisms
Material on Mars
Material in Utah
Mars Polar Ice/Dust Caves? 
Iceland
New, Shallow 
Hydrogen Detection 
Hydrogen is there 
Is it in water ice? 
Are there subsurface 
liquid H2O zones?
Lava tube forms Condensation 
Rain 
Groundwater 
Tube neck collapses  Basaltic insulation 
Ice 
Particles 
Organics? 
Microbes? 
Permanent  
Cave Ice Lakes
The Perfect Building Site 
R.D. Frederick © 2001
Photo by Steve Alvarez 
Cave Aquaculture?
R.D. Frederick © 2001 
Robotic 
Cave Exloration
Location and Mapping 
R.D. Frederick © 2001
In-cave Location 
and Mapping
Access 
R.D. Frederick © 2001
Operational Protocols 
R.D. Frederick © 2002
Inflatables  Liners 
R.D. Frederick © 2002
Novel Airlock Technology 
R.D. Frederick © 2002
Mars-derived Breathing Mixes 
Image © Val Hildreth-Werker
Mouse Mission 
to Inner Space
Controlled Ecological 
Mouse Support 
System
MATERIAL RESOURCES 
The Atmosphere 
MARS EARTH 
CO2 95% 0.03% 
(10 Bars outgassed) 
N2 2.7% 78% 
Argon 1.6% 0.93% 
O2 0.13% 20.9% 
CO 0.07% 0.12ppm 
Neon 
Krypton ppm on both planets 
Xenon
Mars-derived 
Breathing Mixes 
40% N2 
40% 
Argon 
20% O2
Progress Summary 
•• Mouse Mission to Inner Space 
Version 1 in testing 
Version 2 under construction 
Duckweed experiments advanced 
Lighting for plants in design and planning 
Breathing mixture experiments beginning 
Gas balance, water  waste recycling in design 
Cave selection continues 
•• Human Mission to Inner Space 
Inflatables in design 
Airlock in design 
In cave communication system in design 
Access via suits –– HOPING FOR HELP!!!!! 
Operational protocols developing in real-time 
Lighting system in prototype 
Cave selection narrowed to 3
Humans in Caves: 
The Past
Humans in Caves: 
The Present 
Humans in Caves: 
The Future?
Other Collaborators: 
U. New Mexico SLIME Team 
Equinox Interscience, Denver, CO 
Institute of Meteoritics, UNM 
USDA Forest Service 
The Mars Society 
Thanks, NIAC! 
Illustrations: 
Gus (R.D.) Frederick 
Slawek Wojtowicz 
Hajime Sorayama 
Additional Support: 
NSF Life in Extreme Environments Program 
National Geographic Society 
National Speleological Society 
NASA Astrobiology Institute

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Martian caveutilizationjun02

  • 1. Martian Cave Utilization System Feasibility Demonstrations R.D. Frederick © 2001 & Scientific Exploration Technologies P.J. Boston CSR, Inc.
  • 2. Living on Mars: The Surface Paradigm Why is this not such a good idea? •• Radiation shielding problems •• Payload mass intensive •• No obvious access to resources •• No protection from dust storms •• No protection from meteorite impacts
  • 3. Living on Mars: The Subsurface Paradigm P.J. Boston © 2001 Why is this such a GREAT idea? •• Radiation shielding •• Natural pressure vessel •• Potential access to many resources •• Closer access to subsurface drilling •• Protection from dust storms •• Protection from meteorite impacts •• High scientific value: geology, biology, etc.
  • 4. Mars Lava Tubes •• Jumbo-sized •• Numerous •• Clearly visible Alba Patera
  • 5.
  • 7.
  • 8. Rift Tube Serial Flows (After Macdonald, 1965) Trapped Ice Lenses
  • 9. Lava Tubes are often smooth!
  • 10. Desert Surfaces On Earth •• High intensity sunlight and UV •• Low humidity (5-40% typically) •• Temperature extremes •• Low nutrients (usually) •• Mineral-rich (usually) •• Extensive weather, e.g. high winds, flash floods, frost, etc.
  • 11. Desert Caves On Earth •• No sunlight •• High humidity (99-100%) •• Temperatures relatively Photo by David Jagnow constant •• Low nutrients (usually) •• Mineral-rich (usually) •• No weather
  • 12. Cozy!
  • 14. Tafonated Caves •• Typically in sandstones •• Desert environments thermal weathering aeolian weathering •• Seacoast water erosion
  • 15. Big enough for Teddy Bears……
  • 16. Big enough for Humans…… From inside…….
  • 17. Spalling Caves Beginning to form Amphitheater-sized……
  • 18. Photo by L. Hose Photo by Kathy Duchene Mineral Resources
  • 19. Water on Mars: Known Sources ••Atmosphere is saturated at global mean pressure of 8.1 millibars ••Water vapour = 0.03% of current atmosphere (~1-3% for Earth) ••Water ice at north pole ••Water and CO2 ice at south pole
  • 20. Recent Surface Water Evidence •• When? Yesterday to a few million years ago •• How deep? 100-400 m (300-1300 ft) •• How much? 2500 cubic m, about (90,000 cubic ft. •• Where? 30o-70o Most in the south, a few in the northern hemisphere
  • 24. Mars Polar Ice/Dust Caves? Iceland
  • 25. New, Shallow Hydrogen Detection Hydrogen is there Is it in water ice? Are there subsurface liquid H2O zones?
  • 26. Lava tube forms Condensation Rain Groundwater Tube neck collapses Basaltic insulation Ice Particles Organics? Microbes? Permanent Cave Ice Lakes
  • 27. The Perfect Building Site R.D. Frederick © 2001
  • 28. Photo by Steve Alvarez Cave Aquaculture?
  • 29.
  • 30. R.D. Frederick © 2001 Robotic Cave Exloration
  • 31. Location and Mapping R.D. Frederick © 2001
  • 34. Operational Protocols R.D. Frederick © 2002
  • 35. Inflatables Liners R.D. Frederick © 2002
  • 36. Novel Airlock Technology R.D. Frederick © 2002
  • 37. Mars-derived Breathing Mixes Image © Val Hildreth-Werker
  • 38. Mouse Mission to Inner Space
  • 39. Controlled Ecological Mouse Support System
  • 40.
  • 41. MATERIAL RESOURCES The Atmosphere MARS EARTH CO2 95% 0.03% (10 Bars outgassed) N2 2.7% 78% Argon 1.6% 0.93% O2 0.13% 20.9% CO 0.07% 0.12ppm Neon Krypton ppm on both planets Xenon
  • 42. Mars-derived Breathing Mixes 40% N2 40% Argon 20% O2
  • 43.
  • 44. Progress Summary •• Mouse Mission to Inner Space Version 1 in testing Version 2 under construction Duckweed experiments advanced Lighting for plants in design and planning Breathing mixture experiments beginning Gas balance, water waste recycling in design Cave selection continues •• Human Mission to Inner Space Inflatables in design Airlock in design In cave communication system in design Access via suits –– HOPING FOR HELP!!!!! Operational protocols developing in real-time Lighting system in prototype Cave selection narrowed to 3
  • 45. Humans in Caves: The Past
  • 46. Humans in Caves: The Present Humans in Caves: The Future?
  • 47. Other Collaborators: U. New Mexico SLIME Team Equinox Interscience, Denver, CO Institute of Meteoritics, UNM USDA Forest Service The Mars Society Thanks, NIAC! Illustrations: Gus (R.D.) Frederick Slawek Wojtowicz Hajime Sorayama Additional Support: NSF Life in Extreme Environments Program National Geographic Society National Speleological Society NASA Astrobiology Institute