SlideShare a Scribd company logo
1 of 62
Download to read offline
Planetary Circumnavigation
Mission Concept Definition and Technology
Assessment for Global Surface Exploration
of the Terrestrial Planets
David Wettergreen
The Robotics Institute
Carnegie Mellon University
NIAC Fellows Meeting, October 23, 2002
Carnegie Mellon ©2002
Outline
Planetary Circumnavigation
Mission Concepts
•Mercury
•Venus
•Moon
•Mars
Rover Technology Assessment
Carnegie Mellon ©2002
Planetary Circumnavigation
Circumnavigation is travel completely around
a planet returning to the starting location (or
longitude)
Global surface exploration is the science -
driven objective but in many scenarios
circumnavigation is a natural result or an
operational advantage of a long-duration
mission.
Carnegie Mellon ©2002
Global Surface Exploration
Scientific Motivations
•Map composition, resources, and habitats and
their planetary distributions
•Compare regions, encounter boundaries, study
processes to understand planetary evolution
•Understand tectonic, magmatic, hydrologic, etc.
features and their formation
•Conduct in situ analysis including biogenic material
and age dating
Carnegie Mellon ©2002
Planetary Circumnavigation
Technical Motivations
•Maximize solar power through sun-synchrony
•Moderate temperature by terminator following
•Utilize planetary properties for propulsion and
energy (temperature and pressure gradients)
•Scout vast areas and prepare for future
development
Carnegie Mellon ©2002
Progression of Planetary Exploration
Focused Science
Missions
•Focused Investigation
•Single Measurements
•Flybys and Landers
Comprehensive
Science Missions
•Global Exploration
•Regional, Seasonal
Measurements
•Long-duration
Orbiters and Rovers
Discovery Science
Missions
•Broad Investigation
•Multiple Repeated
Measurements
•Orbiters and Rovers
Venera 13 Lander
Lunar Prospector
Carnegie Mellon ©2002
Global Surface Exploration
Past and near-term surface missions explore only
specific locations, less even than a planetary region,
and engage in discovery science.
Someday surface missions may conduct
comprehensive global exploration of Mercury,
Venus, Moon and Mars.
Global surface exploration faces technical and
programmatic challenges. Missions would be
decades hence.
Carnegie Mellon ©2002
Magellan’s Expedition
Magellan’s expedition completed its 3-year circumnavigation
in 1522 with significant discoveries in astronomy, geography,
biology, culture and commerce
Carnegie Mellon ©2002
Rover Expeditions
1973 Lunakhod 2
27 km
56 days
Teleoperated
1997 Sojourner
100m
30 days
Supervisory Control
1972 LRV 17
35.9 km, 16kph
3hrs 2 min
Manned
2003 MER
1km, 1cm/s
90 sols
Supervisory Control
2009 MSL
7+km
180+ sols
Limited Autonomy
Carnegie Mellon ©2002
Increasing Rover Distances
Total
Distance
(km)
10
15
20
25
30
35
5
Lunakhod
1
1970
Lunakhod
2
1973
LRV
15
1973
LRV
16
1974
LRV
17
1976
Sojourner
1997
MER
1
2003
MER
2
2003
MSL
(short)
2009
MSL
(long)
2009
Human Driver
12
27 27.8 26.7
35 .9
Peak
Velocity
(KPH)
7
?
0.1
3 3
Mission distances insufficient to circumnavigation but velocities relevant
Carnegie Mellon ©2002
Increasing Mission Duration
Power cognizance Thermal cognizance
and control
Passive propulsion
and reconfigurable
mobility
In situ resource
extraction and
component
manufacturing
Mission
Duration
Thermal cycles
wear out parts
Reachable terrain
limited by mobility
Components
reach end of life
Enabling Capability:
Limited renewable
power
Mission durations will increase as key capabilities develop over coming decades
Carnegie Mellon ©2002
Expanding Science
Global surface exploration can revolutionize planetary
science just as long-duration orbiters have done
•Massive temporal and spatial data sets
Direct assessment of composition and structure
•Elemental and mineralogical analysis of surface and subsurface
•Age-dating and weathered/unweathered isotopes
Regional measurements and correlations
•Volcanism and tectonics
•Aqueous formation
•Biogenic material and habitats
Carnegie Mellon ©2002
Mission Concepts
Global surface exploration of each of the
terrestrial planets will initiate a new era in
planetary science and will require advances
in key technology areas.
Carnegie Mellon ©2002
Mercury
Notable Characteristics
•High solar irradiance
•Extreme diurnal temperatures
•High Radiation and periodic
solar wind exposure
•Unweathered cratering
•High density
•Slow period of rotation and 3-2
spin-orbit coupling
•Solar retrograde at the
perihelion
Planetary Parameters
Radius 2440 km
Minimum Temperature -173 o
C
Mean Temperature 167 o
C
Maxmum Temperature 427 o
C
Solar Irradiance 9127 W/m2
Surface gravity 65.12 m/s2
Diurnial period 176 days
Carnegie Mellon ©2002
Mercury
Exploration Objectives
•Determine elemental and mineralogical
surface compositions and their variation
and distribution
•Measure surface-bounded atmosphere
•Age-date surface features
•Determine composition and source of
volatiles in polar regions
•Determine compositional variations
and structure of crust
•Quantify regolith processes
•Conduct seismic and heat-flow analysis
Caloris Basin
Carnegie Mellon ©2002
Mercury
Mission Scenario
•Equatorial circumnavigation
•Dawn-following in terminator
•Solar power
•Passive thermal regulation
Mission Options
•High-latitude excursion during perihelion
Mission Predecessors and Precursors
•NASA Messenger 2003, ESA BepiColombo 2009
•Mercury soft lander
Equatorial Circumnavigation Specfications
Distance 15327 km
Rover Speed 3.6 kph, 1 m/s
Duration 4224 hrs
Minimum Comm Lag 04m 18s
Maximum Comm Lag 12m 20s
Carnegie Mellon ©2002
Mercury
Technology
•Extreme temperature electronics
•Thermal transfer and regulation
•Radiation / solar wind hardening
•Localization and navigation
•Multi-rover collaboration
•Health and resource maintenance
•In situ age dating
•High-bandwidth communication
Carnegie Mellon ©2002
Venus
Notable Characteristics
•High temperature at surface
•Atmosphere
High pressure at surface
Acidic / corrosive
High winds at altitude (>60km)
•No Magnetosphere but
ionospheric solar wind deflection
•Smooth volcanic surface
75% Plains
20% Ridges, Volcanoes
Planetary Parameters
Planet Radius 6052 km
Average Temperature 464 o
C
Surface gravity 8.87 m/s2
Diurnial period - 243 days
Atmospheric pressure 90 Atm
Altitude
Day Night
0 km 464 o
C 464 o
C
50 km 80 o
C 80 o
C
100 km - 100 o
C -100 o
C
150 km 30 o
C - 150 o
C
> 150 30 o
C - 150 o
C
Temperature
Carnegie Mellon ©2002
False color Image from Venera 13
Venus
Exploration Issues
•Determine elemental and mineralogical surface composition
and processes of atmosphere/surface interaction
•Observe atmospheric processes and dynamics
Greenhouse effect
Super-rotational winds
•Measure atmospheric composition
•Assess distribution
and age of
volcanism
Carnegie Mellon ©2002
Venus
Mission Scenario
•Global Multi-lander
•20 day cycle of 4 landings each:
1/2 day decent to landing site
2 days on surface
1 day ascent to 100km (transport, cooling, comm.)
1/2 day drifting with wind (45° rotation)
One 2 day drift to traverse night side (180° rotation)
•Passive thermal regulation and atmospheric propulsion
Mission Predecessors and Precursors
•Vega 1 and 2 balloons
•Venera 12 (survived 110 minutes)
•Balloon Ascent/Decent
•Survivable Surface Lander
Multi Lander Circumnavigation
Distance 38025.8 km
Wind Speed 350 kph
Duration 480 hrs
Minimum Communication Lag 02m 07s
Maximum Communication Lag 14m 31s
Venusian clouds,
Galileo
Carnegie Mellon ©2002
Venus
Technology
•Insulation and passive thermal regulation
•Super-pressure balloon
•Passive / environmental propulsion
High speed winds
Temperature and pressure gradients
•Miniaturized in situ sampling and instruments
•Durable electronics
Thermal cycling
Extreme temperature
•Low-mass power source
•Localization and navigation (no celestial, solar, or magnetic)
Carnegie Mellon ©2002
Moon
Notable Characteristics
•Low surface gravity
•Moderate insolation
•Moderate rotational period
•Lunar dust
•Surface-bounded atmosphere
•Extreme diurnal temperature variation
Planetary Parameters
Planet Radius 1737 km
Minimum Temperature - 260 o
C
Mean Temperature - 53 o
C
Maxmum Temperature - 20 o
C
Surface Gravity 1.57 m/s2
Solar Irradiance 1367 W/m2
Diurnal period 28 days
Carnegie Mellon ©2002
Moon
Exploration Objectives
•Measure elemental and
mineralogical composition of
mantle material in South-Pole
Aitken Basin
•Assess volatile and mineral resources
•Measure surface-bounded atmosphere
•Quantify regolith processes
Clementine 1994
Lunar South Pole
Carnegie Mellon ©2002
Rover in Terminator
Polar Circumnavigation
Latitude 85°
Distance 1895.2 km
Duration 28 days
Speed 2.8 KPH, 0.8 m/s
Comm Lag ~3s
Moon
Mission Scenario
•Polar circumnavigation
•Dawn-following in terminator
•Orbiter for communication
Mission Options
•Lower latitude at higher speed
•Transit between peaks of perpetual light
Mission Predecessors and Precursors
•Lunar Prospector Polar Orbiter
Carnegie Mellon ©2002
Moon
Technology
•High efficiency solar cells
•Extreme surface mobility
•Resource-cognizant navigation
•Billion-cycle components
•Electrostatic dust mitigation
•Subsurface access and shallow drilling
•Miniaturized in situ sample processing and
instruments
Carnegie Mellon ©2002
Mars
Notable Characteristics
•Low solar irradiance
•Tenuous atmosphere
•Global dust storms
•Smooth northern hemisphere,
rough southern hemisphere
•Polar caps with water and CO2 ice
Planetary Parameters
Planet Radius 3393 km
Maximum Temperature - 89 o
C
Mean Temperature - 65 o
C
Minimum Temperature - 31 o
C
Surface gravity 3.72 m/s2
Solar Irradiance 589 W/m2
Diurnal period 1.03 days
North Days South
Summer 183 Winter
Autumn 147 Spring
Winter 158 Summer
Spring 199 Autumn
687
Carnegie Mellon ©2002
Mars
Exploration Objectives
•Determine composition and distribution of surface
features; volcanics, impact structures, aqueous features
•Map distribution of water/ice
including subsurface
•Observe and age date
aqueous features
•Seek and characterize
biogenic material
•Assess mineral and volatile resources for future missions
MOLA Image of H2 distribution
Carnegie Mellon ©2002
Mars
Mission Scenario
•Mid-to-high latitude circumnavigation
moves south during northern winter
•Solar power
•Migrate between 30°and 80°annually
•Moderate seasonal temperatures
•Hibernation at night
•6134 km annually (+ 100% margin)
Mission Options
•South polar circumnavigation
•Variations to reduce distance and duration
Migratory Traverse
Distance 61337 km
Speed 4.3 KPH, 1.2 m/s
Duration 10 years
Minimum Comm Lag ~4min
Maximum Comm Lag ~12min
Carnegie Mellon ©2002
Mars
Technology
•Rough terrain navigational autonomy
•Resource cognizance
•Low-mass, long-life components
• Redundant modes
• Motors - lubrication
• Solar cells - degradation
•Electrostatic / dust resistance
•Miniaturized instruments and subsurface access
Martian North Polar Cap
Carnegie Mellon ©2002
Physical parameters describe planetary environment
Assessing Challenges
• Gravity
• Mean Distance from Earth
• Mean Insolation
• Surface Pressure
• Solar Wind / Radiation at
Surface
• Ambient Temperature
• Diurnal Temperature Cycle
• Mean Wind Force
• Obstacle Distribution
• Slope Distribution
Carnegie Mellon ©2002
Gravity
Mean
Distance
from
Earth
Mean
Insolation
Pressure
at
Surface
Solar
Wind
/
Radiation
at
Surface
Ambient
Temperature
Diurnal
Temperature
Cycling
Mean
Wind
Force
Obstacle
Distribution
Slope
Distribution
MERCURY -0.7 0.8 0.9 0.0 1.0 0.3 1.0 -0.6 0.9 0.9
VENUS -0.1 0.8 -0.1 1.0 0.0 1.0 0.0 0.4 -0.1 -0.1
MOON -1.0 0.0 0.1 0.0 0.8 0.1 0.4 -0.6 0.7 0.7
MARS -0.7 1.0 0.0 0.0 0.6 0.2 0.1 -0.4 0.4 0.4
PLANET
ENVIRONMENTAL
Planetary Environments
Numbers are based on planetary parameters or estimates
Normalized over the range of values and offset to Earth equals 0
Green: high magnitude and Red: low magnitude
Carnegie Mellon ©2002
Relate the impact of the environment on rover
performance metrics:
Assessing Challenges
• Power Balance
• Mass
• Volume
• Trafficability
• Maneuverability
• Terrainability
• Speed
• Usability
• Data Volume
• Reliability
• Sustainability
• Survivability
Carnegie Mellon ©2002
Environment and Performance
Identify
relationships
between rover
performance and
environment
Green: directly
proportional
Red: inversely
proportional
Gravity
Average
Distance
from
Earth
Insolation
Pressure
at
Surface
Solar
Wind
/
Radiation
Ambient
Temperature
Diurnal
Temperature
Cycling
Mean
Wind
Force
Obstacle
Distribution
Slope
Distribution
m
/
s2
Light-seconds
W
/
m2
atm
K
(from
operating)
K
(amplitude)
N
Power Balance n P N
Minimized Mass
Minimized Volume
Trafficability N N N
Maneuverability N N
Terrainability N N
Speed N N
Usability
Data Volume N N
Reliability N N N N N N N N
Sustainability P N N
Survivability N N N N N n N
PERFORMANCE
METRICS
ENVIRONMENTAL
Carnegie Mellon ©2002
Performance Correlations
Consider
performance
metrics that are
correlated
Green: directly
proportional
Red: inversely
proportional
Power
Balance
Minimized
Mass
Minimized
Volume
Trafficability
Maneuverability
Terrainability
Speed
Usability
Data
Volume
Reliability
Sustainability
Survivability
Power Balance P N N
Minimized Mass P
Minimized Volume P
Trafficability P
Maneuverability P
Terrainability P
Speed P P P
Usability P P P
Data Volume P
Reliability P P P P N P
Sustainability P
Survivability P P P N
PERFORMANCE
METRICS
PERFORMANCE METRICS
Carnegie Mellon ©2002
Assessing Challenges
Derive the challenges posed by planetary
environments in terms of rover performance
MERCURY
Power Balance 3.7
Trafficability 0.0
Maneuverability -0.7
Terrainability -0.3
Speed -3.4
Usability -8.5
Data Volume -2.8
Reliability -4.4
Sustainability -0.1
Survivability -3.8
PERFORMANCE
METRICS
VENUS
-1.7
-0.6
-0.7
-0.3
0.0
-6.0
-0.8
-3.7
-1.0
-2.2
MOON
2.3
0.0
-1.0
-0.1
-2.8
-3.4
-1.9
-2.2
-0.6
-1.1
MARS
1.1
0.0
-0.7
0.0
-1.7
-5.0
-2.3
-2.3
-0.6
-1.3
Relationships of
Environment to
Performance
Metrics
Descriptions
of Planetary
Environments
Relationships
between
Performance
Metrics
Challenges
of Planetary
Environments
Carnegie Mellon ©2002
Performance Metrics
With Respect to Earth
-10.0
-8.0
-6.0
-4.0
-2.0
0.0
2.0
4.0
6.0 MERCURY
VENUS
MOON
MARS
`
Power
Balance
Trafficability
Maneuverability
Terrainability
Speed
Usability
Data
Volume
Reliability
Sustainability
Survivability
EARTH
Carnegie Mellon ©2002
Assesing Challenges
Relate rover configuration parameters and
performance metrics—what technologies most effect
the environmental challenges posed
Select configuration parameters that improve
performance metrics and do not negatively impact
performance that the environment already supports
Relationships of
Configuration to
Performance
Metrics
Challenges
of Planetary
Environments
Technologies
that Effect
Challenges
Carnegie Mellon ©2002
Configuration and Performance
Output
Longevity
Center
of
Mass
Hieght
Wheel
Base
Mass
Volume
Max
Continuous
Torque
Max
Peak
Torque
Speed
Power
Consumption
MTTF
Redundant
Components
Chassis
Steering
Power
Loss
Data
Rate
Transmitted
Power
Availability
Computation
Memory
MTBF
Output
Mass
Volume
MTTF
Input
from
Environment
Mission
/
Goal
Planning
Resource
Monitoring
Health
Monitoring
Navigation
/
Obstacle
Avoidance
Control
Localization
Site
Mapping
Sample
Acquisition
and
Handling
Science
Data
Understanding
Exploration
and
Discovery
W
s
m
m
kg
m3
N
m
N
m
m
/
s
W
W
%
W
/
deg
bits
/
s
W
%
MIPS
bits
s
J
kg
m3
s
W
Power Balance P N N N N N N N P
Minimized Mass N N P N
Minimized Volume N N N P
Trafficability P P P
Maneuverability N P P
Terrainability P P P
Speed P P P
Usability P P P P P P P P P P P
Data Volume P P P P P P P P
Reliability P P P P P P P P P P P
Sustainability P P P P P
Survivability P N P P P P P
CONFIGURATION PARAMETERS CONFIGURATION PARAMETERS
PERFORMANCE
METRICS
AUTONOMY
POWER LOCOMOTION COMM COMPUTING THERMAL
Carnegie Mellon ©2002
Mission Technology Needs
Output
Longevity
Center
of
Mass
Hieght
Wheel
Base
Mass
Volume
Max
Continuous
Torque
Max
Peak
Torque
Speed
Power
Consumption
MTTF
Redundant
Components
Chassis
Steering
Power
Loss
Data
Rate
Transmitted
Power
Availability
Computation
Memory
MTBF
Output
Mass
Volume
MTTF
Mission
/
Goal
Planning
Resource
Monitoring
Health
Monitoring
Navigation
/
Obstacle
Avoidance
Control
Localization
Site
Mapping
Sample
Acquisition
and
Handling
Science
Data
Understanding
Exploration
and
Discovery
MERCURY 0.0 0.0 0.1 0.1 0.0 0.0 -0.9 0.0 -0.1 -0.9 0.0 1.0 -1.0 2.7 0.2 3.7 1.8 2.7 4.0 1.1 0.0 0.0 0.0 1.0 0.0 1.0 2.9 5.0 3.1 2.7 3.7 2.7 2.7
VENUS 0.6 0.4 0.1 0.1 0.0 0.0 -0.4 0.4 -0.8 -0.6 0.4 1.4 -0.9 2.5 0.7 3.9 1.9 2.5 4.4 1.6 0.0 0.0 0.4 1.4 1.0 1.4 2.5 5.0 3.6 2.5 3.9 2.5 2.5
MOON 0.0 0.3 0.1 0.1 0.0 0.0 -1.1 -0.6 0.8 -1.1 0.3 1.0 -1.6 2.5 -0.1 3.5 1.4 2.5 3.2 0.4 0.0 0.0 0.3 1.0 0.3 1.0 3.3 5.0 2.6 2.5 3.5 2.5 2.5
MARS 0.0 0.3 0.0 0.0 0.0 0.0 -0.5 0.1 0.2 -0.5 0.3 1.0 -0.8 3.3 0.5 4.4 2.8 3.3 3.9 1.1 0.0 0.0 0.3 1.0 0.3 1.0 2.7 5.0 3.3 3.3 4.4 3.3 3.3
CONFIGURATION PARAMETERS
POWER LOCOMOTION COMM COMPUTING AUTONOMY
THERMAL
Technology positively effects many performance challenges
Technology positively effects few performance challenges
Focus on rover configuration parameters that
improve performance
Carnegie Mellon ©2002
Rover Technology Issues
Sufficient Power
• Reliable, low-mass, long-duration power sources
• Resource cognizance
Thermal Extremes and Cycling
• Extreme temperature components
• Efficient thermal regulation, heat flow in the terminator
Reliable Mobility
• Reliable, low-mass mobility mechanisms
• Stable extreme terrain locomotion
Necessary Autonomy
• Autonomy in localization, navigation, and control
• Brain versus brawn, minimal communication and oversight
Long-term Sustainability
• Very long-duration components and algorithms
• High bandwidth and availability communication
Carnegie Mellon ©2002
Exploration Issues
Miniturized Instruments
•In Situ Observation
•Age Dating
•Biogenic Organic Detection
Sample Acquisition and Preparation
Science Data Understanding
•Automated calibration and data quality assessment
•Automated sample selection
Carnegie Mellon ©2002
Summary
Global surface exploration, which is largely
complete for the Earth, is appropriate for all
the terrestrial planets.
Planetary circumnavigation results from long-
duration exploration in some scenarios
Planetary circumnavigation has scientific,
technological and programmatic advantages
Thank You
Questions?
Additional Material
Carnegie Mellon ©2002
Velocity of One-day Circumnavigation
Velocity Required For Single Day Circumnavigation
1669.756 1644.389 1569.058 1446.052 1279.108
1073.299
834.878
571.090
289.950
145.529
862.413 849.311 810.403 746.872 660.647
554.348
431.206
294.963
149.756
75.164
0.100
1.000
10.000
100.000
1000.000
10000.000
0 10 20 30 40 50 60 70 80 90
latitude (degrees)
velocity
(km/hr)
Earth Mars Mercury Venus Moon
Carnegie Mellon ©2002
NRC Solar System Exploration Study
Objectives
Solar System Formation
Volatiles & Organics
Habitable Worlds
Planetary Processes
Missions (Inner Planets)
Mercury Orbiter
South Pole-Aitken Basin Sample
Return
Venus In-Situ Explorer
Mars Long-Lived Lander Network
Mercury Sample Return
Venus Surface Sample Return
Articulate important investigations in planetary
science and prioritize missions
Carnegie Mellon ©2002
NEXT Space Robotics Study
Assess the current and projected state-of-the-art in space
robotics including surface exploration
Challenges relative to circumnavigation:
Minor Moderate Major
Obstacle Detection Map Building Localization
Obstacle Avoidance Health Monitoring Terrain Detection
Path Execution Path Planning Science Autonomy
Coverage Planning Resource Planning Exploration
Mission Planning
Carnegie Mellon ©2002
F
o
l
l
o
w
p
l
a
n
u
n
a
w
a
r
e
D
e
t
e
c
t
s
u
n
u
s
u
a
l
p
a
t
t
e
r
n
s
C
o
l
l
e
c
t
u
n
u
s
u
a
l
d
a
t
a
I
n
v
e
s
t
i
g
a
t
e
o
p
p
o
r
t
u
n
i
t
i
e
s
S
e
e
k
s
a
n
o
m
a
l
i
e
s
G
e
n
e
r
a
t
e
d
i
s
c
o
v
e
r
y
p
l
a
n
G
e
n
e
r
a
t
e
s
c
i
e
n
t
i
f
i
c
h
y
p
o
t
h
e
s
e
s
Current
Nominal 10year
Intense 10year
Breakthrough
0
2
4
6
8
10
12
14
NEXT Space Robotics Study
Robotic
exploration is
complicated by
the demands of
autonomous
science
investigation
Carnegie Mellon ©2002
Next Space Robotics Study
Localization requires significant prior
knowledge
Using proprioception
Visual odometry
Using fixed beacons
Using natural features
Without global map
Current
Nominal 10years
Intense 10years
Breakthrough
0
2
4
6
8
10
12
14
Carnegie Mellon ©2002
Solar Powered Circumnavigation
Perpetual exploration through synchronization
with the Sun to provide continuous energy
Remain in favorable sun position and avoid
extreme temperatures by following dawn in the
terminator
Carnegie Mellon ©2002
Conditions Favorable to Solar Power
High solar flux
•Providing abundant solar energy
Moderate gravity
•Resulting in lower locomotive power
Small planetary diameter
Long rotational period
•Less speed required for planetary circumnavigation
High planetary axial tilt
•Long summer for polar exploration
Carnegie Mellon ©2002
Kilometers
Arctic Field Experiment
Demonstrate concept of sun-
synchronous navigation and
quantify performance
Conduct 24-hour experiments in
planetary-analog terrain
Carnegie Mellon ©2002
Carnegie Mellon ©2002
Sun-Synchronous Experiment
Von Braun Planitia
•7% (max 34%) obstacle density
Operation
•No intervention
•Autonomous 90%
Power
•Completed on schedule
with batteries charged
Distance: 6.1km
Carnegie Mellon ©2002
Sun-Synchronous Experiment
Sun-synchrony
•Average heading
tracks path with
average near zero
•Some deviation
including reversals
Relative Occurance of Heading Error
0
1
2
3
4
5
6
7
8
9
10
-179
-169
-159
-149
-139
-129
-119
-109
-99
-89
-79
-69
-59
-49
-39
-29
-19
-9
1
11
21
31
41
51
61
71
81
91
101
111
121
131
141
151
161
171
Heading Error
%
Occurrence
Carnegie Mellon ©2002
Reliability, Sustainability, Survivability
Time t = tsustainability
Fault
Probability,
P
F
Reliability is the
probability of correct
operation: 1 – PF(t)
Survivability is the
probability that a fault will
end the mission
Sustainability is the time after
which faults become
unacceptably likely
PF = max_allowable
Carnegie Mellon ©2002
Trafficability, Maneuverability,
Terrainability
Trafficability
• The ability for a vehicle to drive through terrain
• Effected by traction, torque, power
Maneuverability
• The ability for a vehicle to drive around obstacles
• Effected by steering response, minimum turning radius
Terrainability
• The ability for a vehicle to remain stable
• Effected by center-of-gravity, statics, dynamics
Carnegie Mellon ©2002
Improving Technology Assessment
Include more quantitative relationships between configuration
parameters and performance metrics
•More subtle than “direct” or “inverse” proportionality is needed to
made design decisions
Enrich the model with more parameters
•A more complete set of environmental parameters
•Configuration parameters that better cover design space
•Performance metrics that better cover launch, landing and science
Add the ability to evaluate particular mission scenarios

More Related Content

What's hot

S/C in Heliosynchronous Orbit - Spacecraft Environment Analysis
S/C in Heliosynchronous Orbit - Spacecraft Environment AnalysisS/C in Heliosynchronous Orbit - Spacecraft Environment Analysis
S/C in Heliosynchronous Orbit - Spacecraft Environment AnalysisPau Molas Roca
 
Geophysical methods brief summary
Geophysical methods brief summaryGeophysical methods brief summary
Geophysical methods brief summaryJyoti Khatiwada
 
Gravity and magmetic method
Gravity and magmetic methodGravity and magmetic method
Gravity and magmetic methodShah Naseer
 
Space Environment & It's Effects On Space Systems course sampler
Space Environment & It's Effects On Space Systems course samplerSpace Environment & It's Effects On Space Systems course sampler
Space Environment & It's Effects On Space Systems course samplerJim Jenkins
 
High Resolution Earth's Gravitational Field
High Resolution Earth's Gravitational FieldHigh Resolution Earth's Gravitational Field
High Resolution Earth's Gravitational FieldAli Osman Öncel
 
Time dependent probabilistic seismic hazard assessment
Time dependent probabilistic seismic hazard assessmentTime dependent probabilistic seismic hazard assessment
Time dependent probabilistic seismic hazard assessmentIIT Roorkee
 
Measuring Ice Mass Loss from Melting Ice Sheets
Measuring Ice Mass Loss from Melting Ice SheetsMeasuring Ice Mass Loss from Melting Ice Sheets
Measuring Ice Mass Loss from Melting Ice SheetsChristopher Harig
 
A precise water_abundance_measurement_for_the_hot_jupiter_wasp_43b
A precise water_abundance_measurement_for_the_hot_jupiter_wasp_43bA precise water_abundance_measurement_for_the_hot_jupiter_wasp_43b
A precise water_abundance_measurement_for_the_hot_jupiter_wasp_43bSérgio Sacani
 
Geophysical methods
Geophysical methodsGeophysical methods
Geophysical methodsFands-llc
 
Phys revlett.106.221101
Phys revlett.106.221101Phys revlett.106.221101
Phys revlett.106.221101Sérgio Sacani
 
Land Seismic Sources - Explosives Vs. Vibroseis
Land Seismic Sources - Explosives Vs. Vibroseis Land Seismic Sources - Explosives Vs. Vibroseis
Land Seismic Sources - Explosives Vs. Vibroseis Alex TX
 
Subsurface geophysical methods
Subsurface geophysical methodsSubsurface geophysical methods
Subsurface geophysical methodsMohit Kumar
 
Site-dependent Spectra: Ground Motion Records in Turkey
Site-dependent Spectra: Ground Motion Records in TurkeySite-dependent Spectra: Ground Motion Records in Turkey
Site-dependent Spectra: Ground Motion Records in TurkeyAli Osman Öncel
 
Space Radiation & It's Effects On Space Systems & Astronauts Course Sampler
Space Radiation & It's Effects On Space Systems & Astronauts Course SamplerSpace Radiation & It's Effects On Space Systems & Astronauts Course Sampler
Space Radiation & It's Effects On Space Systems & Astronauts Course SamplerJim Jenkins
 
Gravity and Magnetic Mapping
Gravity and  Magnetic MappingGravity and  Magnetic Mapping
Gravity and Magnetic MappingBrenton Garside
 
What is-geophysics
What is-geophysicsWhat is-geophysics
What is-geophysicsAbdul Basit
 

What's hot (19)

S/C in Heliosynchronous Orbit - Spacecraft Environment Analysis
S/C in Heliosynchronous Orbit - Spacecraft Environment AnalysisS/C in Heliosynchronous Orbit - Spacecraft Environment Analysis
S/C in Heliosynchronous Orbit - Spacecraft Environment Analysis
 
3D Seismic Refraction
3D Seismic Refraction3D Seismic Refraction
3D Seismic Refraction
 
Geophysical methods brief summary
Geophysical methods brief summaryGeophysical methods brief summary
Geophysical methods brief summary
 
Gravity and magmetic method
Gravity and magmetic methodGravity and magmetic method
Gravity and magmetic method
 
Space Environment & It's Effects On Space Systems course sampler
Space Environment & It's Effects On Space Systems course samplerSpace Environment & It's Effects On Space Systems course sampler
Space Environment & It's Effects On Space Systems course sampler
 
High Resolution Earth's Gravitational Field
High Resolution Earth's Gravitational FieldHigh Resolution Earth's Gravitational Field
High Resolution Earth's Gravitational Field
 
Time dependent probabilistic seismic hazard assessment
Time dependent probabilistic seismic hazard assessmentTime dependent probabilistic seismic hazard assessment
Time dependent probabilistic seismic hazard assessment
 
Measuring Ice Mass Loss from Melting Ice Sheets
Measuring Ice Mass Loss from Melting Ice SheetsMeasuring Ice Mass Loss from Melting Ice Sheets
Measuring Ice Mass Loss from Melting Ice Sheets
 
A precise water_abundance_measurement_for_the_hot_jupiter_wasp_43b
A precise water_abundance_measurement_for_the_hot_jupiter_wasp_43bA precise water_abundance_measurement_for_the_hot_jupiter_wasp_43b
A precise water_abundance_measurement_for_the_hot_jupiter_wasp_43b
 
Geophysical methods
Geophysical methodsGeophysical methods
Geophysical methods
 
Phys revlett.106.221101
Phys revlett.106.221101Phys revlett.106.221101
Phys revlett.106.221101
 
Land Seismic Sources - Explosives Vs. Vibroseis
Land Seismic Sources - Explosives Vs. Vibroseis Land Seismic Sources - Explosives Vs. Vibroseis
Land Seismic Sources - Explosives Vs. Vibroseis
 
Subsurface geophysical methods
Subsurface geophysical methodsSubsurface geophysical methods
Subsurface geophysical methods
 
Site-dependent Spectra: Ground Motion Records in Turkey
Site-dependent Spectra: Ground Motion Records in TurkeySite-dependent Spectra: Ground Motion Records in Turkey
Site-dependent Spectra: Ground Motion Records in Turkey
 
Space Radiation & It's Effects On Space Systems & Astronauts Course Sampler
Space Radiation & It's Effects On Space Systems & Astronauts Course SamplerSpace Radiation & It's Effects On Space Systems & Astronauts Course Sampler
Space Radiation & It's Effects On Space Systems & Astronauts Course Sampler
 
Gravity and Magnetic Mapping
Gravity and  Magnetic MappingGravity and  Magnetic Mapping
Gravity and Magnetic Mapping
 
Seismic Microzonation
Seismic MicrozonationSeismic Microzonation
Seismic Microzonation
 
Unit 5
Unit 5Unit 5
Unit 5
 
What is-geophysics
What is-geophysicsWhat is-geophysics
What is-geophysics
 

Similar to Planetary circumnavigation

Senior Design - Europa Lander Mission Presentation
Senior Design - Europa Lander Mission PresentationSenior Design - Europa Lander Mission Presentation
Senior Design - Europa Lander Mission PresentationMatt Bergman
 
Using Time Domain Reflectometry (TDR) to Monitor the Geophysical Properties o...
Using Time Domain Reflectometry (TDR) to Monitor the Geophysical Properties o...Using Time Domain Reflectometry (TDR) to Monitor the Geophysical Properties o...
Using Time Domain Reflectometry (TDR) to Monitor the Geophysical Properties o...DART Project
 
Sara Seager - Lecture1 - MIT
Sara Seager - Lecture1 - MITSara Seager - Lecture1 - MIT
Sara Seager - Lecture1 - MITAtner Yegorov
 
MARS HABITAT DESIGN
MARS HABITAT DESIGNMARS HABITAT DESIGN
MARS HABITAT DESIGNArnob Foysal
 
Mars Geophysical Lander Proposal Authorization Review
Mars Geophysical Lander Proposal Authorization ReviewMars Geophysical Lander Proposal Authorization Review
Mars Geophysical Lander Proposal Authorization ReviewBrian Shiro
 
Space Weather: Forecasting, Tracking, and the Effects of Earth Directed Solar...
Space Weather: Forecasting, Tracking, and the Effects of Earth Directed Solar...Space Weather: Forecasting, Tracking, and the Effects of Earth Directed Solar...
Space Weather: Forecasting, Tracking, and the Effects of Earth Directed Solar...Emily Schomp
 
Geophysical Challenge in Oil and Gas Project
Geophysical Challenge in Oil and Gas ProjectGeophysical Challenge in Oil and Gas Project
Geophysical Challenge in Oil and Gas ProjectGilang Wiranda
 
4- Geophysics and exploration
4- Geophysics and exploration4- Geophysics and exploration
4- Geophysics and explorationElsayed Amer
 
Stratospheric satellitesjun01
Stratospheric satellitesjun01Stratospheric satellitesjun01
Stratospheric satellitesjun01Clifford Stone
 
Extraterrestrial atmospheres
Extraterrestrial atmospheresExtraterrestrial atmospheres
Extraterrestrial atmospheresrahulporuri
 

Similar to Planetary circumnavigation (20)

Senior Design - Europa Lander Mission Presentation
Senior Design - Europa Lander Mission PresentationSenior Design - Europa Lander Mission Presentation
Senior Design - Europa Lander Mission Presentation
 
Nock nov99
Nock nov99Nock nov99
Nock nov99
 
Using Time Domain Reflectometry (TDR) to Monitor the Geophysical Properties o...
Using Time Domain Reflectometry (TDR) to Monitor the Geophysical Properties o...Using Time Domain Reflectometry (TDR) to Monitor the Geophysical Properties o...
Using Time Domain Reflectometry (TDR) to Monitor the Geophysical Properties o...
 
Sara Seager - Lecture1 - MIT
Sara Seager - Lecture1 - MITSara Seager - Lecture1 - MIT
Sara Seager - Lecture1 - MIT
 
Bahan kuliah kontek
Bahan kuliah kontekBahan kuliah kontek
Bahan kuliah kontek
 
MARS HABITAT DESIGN
MARS HABITAT DESIGNMARS HABITAT DESIGN
MARS HABITAT DESIGN
 
Mars Geophysical Lander Proposal Authorization Review
Mars Geophysical Lander Proposal Authorization ReviewMars Geophysical Lander Proposal Authorization Review
Mars Geophysical Lander Proposal Authorization Review
 
TECHNOLOGY MISSIONS
TECHNOLOGY MISSIONSTECHNOLOGY MISSIONS
TECHNOLOGY MISSIONS
 
Space Weather: Forecasting, Tracking, and the Effects of Earth Directed Solar...
Space Weather: Forecasting, Tracking, and the Effects of Earth Directed Solar...Space Weather: Forecasting, Tracking, and the Effects of Earth Directed Solar...
Space Weather: Forecasting, Tracking, and the Effects of Earth Directed Solar...
 
Geophysical Challenge in Oil and Gas Project
Geophysical Challenge in Oil and Gas ProjectGeophysical Challenge in Oil and Gas Project
Geophysical Challenge in Oil and Gas Project
 
1207 angel[1]
1207 angel[1]1207 angel[1]
1207 angel[1]
 
4- Geophysics and exploration
4- Geophysics and exploration4- Geophysics and exploration
4- Geophysics and exploration
 
Orbital Debris Mapping
Orbital Debris MappingOrbital Debris Mapping
Orbital Debris Mapping
 
Stratospheric satellitesjun01
Stratospheric satellitesjun01Stratospheric satellitesjun01
Stratospheric satellitesjun01
 
Goddard 2015: James Green, NASA
Goddard 2015: James Green, NASAGoddard 2015: James Green, NASA
Goddard 2015: James Green, NASA
 
LCROSS Mission Overview & Results (
LCROSS Mission Overview & Results (LCROSS Mission Overview & Results (
LCROSS Mission Overview & Results (
 
Facts About Venus
Facts About VenusFacts About Venus
Facts About Venus
 
Extraterrestrial atmospheres
Extraterrestrial atmospheresExtraterrestrial atmospheres
Extraterrestrial atmospheres
 
1059 maise[2]
1059 maise[2]1059 maise[2]
1059 maise[2]
 
Kepler Mission
Kepler MissionKepler Mission
Kepler Mission
 

More from Clifford Stone (20)

Zubrin nov99
Zubrin nov99Zubrin nov99
Zubrin nov99
 
Xray telescopeconcept
Xray telescopeconceptXray telescopeconcept
Xray telescopeconcept
 
Xray interferometry
Xray interferometryXray interferometry
Xray interferometry
 
Wpafb blue bookdocuments
Wpafb blue bookdocumentsWpafb blue bookdocuments
Wpafb blue bookdocuments
 
What gov knows_about_ufos
What gov knows_about_ufosWhat gov knows_about_ufos
What gov knows_about_ufos
 
Welcome oct02
Welcome oct02Welcome oct02
Welcome oct02
 
Weather jun02
Weather jun02Weather jun02
Weather jun02
 
Wassersug richard[1]
Wassersug richard[1]Wassersug richard[1]
Wassersug richard[1]
 
Washington, d.c., jul 26 27, 1952
Washington, d.c., jul 26 27, 1952Washington, d.c., jul 26 27, 1952
Washington, d.c., jul 26 27, 1952
 
Wash dc jul 19 to 20 1952
Wash dc jul 19 to 20 1952Wash dc jul 19 to 20 1952
Wash dc jul 19 to 20 1952
 
Vol4ch03
Vol4ch03Vol4ch03
Vol4ch03
 
Vol4ch02
Vol4ch02Vol4ch02
Vol4ch02
 
Vol4ch01
Vol4ch01Vol4ch01
Vol4ch01
 
Vol3ch16
Vol3ch16Vol3ch16
Vol3ch16
 
Vol3ch14
Vol3ch14Vol3ch14
Vol3ch14
 
Vol3ch13
Vol3ch13Vol3ch13
Vol3ch13
 
Vol3ch12
Vol3ch12Vol3ch12
Vol3ch12
 
Vol3ch11
Vol3ch11Vol3ch11
Vol3ch11
 
Vol3ch10
Vol3ch10Vol3ch10
Vol3ch10
 
Vol3ch09
Vol3ch09Vol3ch09
Vol3ch09
 

Planetary circumnavigation

  • 1. Planetary Circumnavigation Mission Concept Definition and Technology Assessment for Global Surface Exploration of the Terrestrial Planets David Wettergreen The Robotics Institute Carnegie Mellon University NIAC Fellows Meeting, October 23, 2002
  • 2. Carnegie Mellon ©2002 Outline Planetary Circumnavigation Mission Concepts •Mercury •Venus •Moon •Mars Rover Technology Assessment
  • 3. Carnegie Mellon ©2002 Planetary Circumnavigation Circumnavigation is travel completely around a planet returning to the starting location (or longitude) Global surface exploration is the science - driven objective but in many scenarios circumnavigation is a natural result or an operational advantage of a long-duration mission.
  • 4. Carnegie Mellon ©2002 Global Surface Exploration Scientific Motivations •Map composition, resources, and habitats and their planetary distributions •Compare regions, encounter boundaries, study processes to understand planetary evolution •Understand tectonic, magmatic, hydrologic, etc. features and their formation •Conduct in situ analysis including biogenic material and age dating
  • 5. Carnegie Mellon ©2002 Planetary Circumnavigation Technical Motivations •Maximize solar power through sun-synchrony •Moderate temperature by terminator following •Utilize planetary properties for propulsion and energy (temperature and pressure gradients) •Scout vast areas and prepare for future development
  • 6. Carnegie Mellon ©2002 Progression of Planetary Exploration Focused Science Missions •Focused Investigation •Single Measurements •Flybys and Landers Comprehensive Science Missions •Global Exploration •Regional, Seasonal Measurements •Long-duration Orbiters and Rovers Discovery Science Missions •Broad Investigation •Multiple Repeated Measurements •Orbiters and Rovers Venera 13 Lander Lunar Prospector
  • 7. Carnegie Mellon ©2002 Global Surface Exploration Past and near-term surface missions explore only specific locations, less even than a planetary region, and engage in discovery science. Someday surface missions may conduct comprehensive global exploration of Mercury, Venus, Moon and Mars. Global surface exploration faces technical and programmatic challenges. Missions would be decades hence.
  • 8. Carnegie Mellon ©2002 Magellan’s Expedition Magellan’s expedition completed its 3-year circumnavigation in 1522 with significant discoveries in astronomy, geography, biology, culture and commerce
  • 9. Carnegie Mellon ©2002 Rover Expeditions 1973 Lunakhod 2 27 km 56 days Teleoperated 1997 Sojourner 100m 30 days Supervisory Control 1972 LRV 17 35.9 km, 16kph 3hrs 2 min Manned 2003 MER 1km, 1cm/s 90 sols Supervisory Control 2009 MSL 7+km 180+ sols Limited Autonomy
  • 10. Carnegie Mellon ©2002 Increasing Rover Distances Total Distance (km) 10 15 20 25 30 35 5 Lunakhod 1 1970 Lunakhod 2 1973 LRV 15 1973 LRV 16 1974 LRV 17 1976 Sojourner 1997 MER 1 2003 MER 2 2003 MSL (short) 2009 MSL (long) 2009 Human Driver 12 27 27.8 26.7 35 .9 Peak Velocity (KPH) 7 ? 0.1 3 3 Mission distances insufficient to circumnavigation but velocities relevant
  • 11. Carnegie Mellon ©2002 Increasing Mission Duration Power cognizance Thermal cognizance and control Passive propulsion and reconfigurable mobility In situ resource extraction and component manufacturing Mission Duration Thermal cycles wear out parts Reachable terrain limited by mobility Components reach end of life Enabling Capability: Limited renewable power Mission durations will increase as key capabilities develop over coming decades
  • 12. Carnegie Mellon ©2002 Expanding Science Global surface exploration can revolutionize planetary science just as long-duration orbiters have done •Massive temporal and spatial data sets Direct assessment of composition and structure •Elemental and mineralogical analysis of surface and subsurface •Age-dating and weathered/unweathered isotopes Regional measurements and correlations •Volcanism and tectonics •Aqueous formation •Biogenic material and habitats
  • 13. Carnegie Mellon ©2002 Mission Concepts Global surface exploration of each of the terrestrial planets will initiate a new era in planetary science and will require advances in key technology areas.
  • 14. Carnegie Mellon ©2002 Mercury Notable Characteristics •High solar irradiance •Extreme diurnal temperatures •High Radiation and periodic solar wind exposure •Unweathered cratering •High density •Slow period of rotation and 3-2 spin-orbit coupling •Solar retrograde at the perihelion Planetary Parameters Radius 2440 km Minimum Temperature -173 o C Mean Temperature 167 o C Maxmum Temperature 427 o C Solar Irradiance 9127 W/m2 Surface gravity 65.12 m/s2 Diurnial period 176 days
  • 15. Carnegie Mellon ©2002 Mercury Exploration Objectives •Determine elemental and mineralogical surface compositions and their variation and distribution •Measure surface-bounded atmosphere •Age-date surface features •Determine composition and source of volatiles in polar regions •Determine compositional variations and structure of crust •Quantify regolith processes •Conduct seismic and heat-flow analysis Caloris Basin
  • 16.
  • 17. Carnegie Mellon ©2002 Mercury Mission Scenario •Equatorial circumnavigation •Dawn-following in terminator •Solar power •Passive thermal regulation Mission Options •High-latitude excursion during perihelion Mission Predecessors and Precursors •NASA Messenger 2003, ESA BepiColombo 2009 •Mercury soft lander Equatorial Circumnavigation Specfications Distance 15327 km Rover Speed 3.6 kph, 1 m/s Duration 4224 hrs Minimum Comm Lag 04m 18s Maximum Comm Lag 12m 20s
  • 18. Carnegie Mellon ©2002 Mercury Technology •Extreme temperature electronics •Thermal transfer and regulation •Radiation / solar wind hardening •Localization and navigation •Multi-rover collaboration •Health and resource maintenance •In situ age dating •High-bandwidth communication
  • 19. Carnegie Mellon ©2002 Venus Notable Characteristics •High temperature at surface •Atmosphere High pressure at surface Acidic / corrosive High winds at altitude (>60km) •No Magnetosphere but ionospheric solar wind deflection •Smooth volcanic surface 75% Plains 20% Ridges, Volcanoes Planetary Parameters Planet Radius 6052 km Average Temperature 464 o C Surface gravity 8.87 m/s2 Diurnial period - 243 days Atmospheric pressure 90 Atm Altitude Day Night 0 km 464 o C 464 o C 50 km 80 o C 80 o C 100 km - 100 o C -100 o C 150 km 30 o C - 150 o C > 150 30 o C - 150 o C Temperature
  • 20. Carnegie Mellon ©2002 False color Image from Venera 13 Venus Exploration Issues •Determine elemental and mineralogical surface composition and processes of atmosphere/surface interaction •Observe atmospheric processes and dynamics Greenhouse effect Super-rotational winds •Measure atmospheric composition •Assess distribution and age of volcanism
  • 21.
  • 22. Carnegie Mellon ©2002 Venus Mission Scenario •Global Multi-lander •20 day cycle of 4 landings each: 1/2 day decent to landing site 2 days on surface 1 day ascent to 100km (transport, cooling, comm.) 1/2 day drifting with wind (45° rotation) One 2 day drift to traverse night side (180° rotation) •Passive thermal regulation and atmospheric propulsion Mission Predecessors and Precursors •Vega 1 and 2 balloons •Venera 12 (survived 110 minutes) •Balloon Ascent/Decent •Survivable Surface Lander Multi Lander Circumnavigation Distance 38025.8 km Wind Speed 350 kph Duration 480 hrs Minimum Communication Lag 02m 07s Maximum Communication Lag 14m 31s Venusian clouds, Galileo
  • 23. Carnegie Mellon ©2002 Venus Technology •Insulation and passive thermal regulation •Super-pressure balloon •Passive / environmental propulsion High speed winds Temperature and pressure gradients •Miniaturized in situ sampling and instruments •Durable electronics Thermal cycling Extreme temperature •Low-mass power source •Localization and navigation (no celestial, solar, or magnetic)
  • 24. Carnegie Mellon ©2002 Moon Notable Characteristics •Low surface gravity •Moderate insolation •Moderate rotational period •Lunar dust •Surface-bounded atmosphere •Extreme diurnal temperature variation Planetary Parameters Planet Radius 1737 km Minimum Temperature - 260 o C Mean Temperature - 53 o C Maxmum Temperature - 20 o C Surface Gravity 1.57 m/s2 Solar Irradiance 1367 W/m2 Diurnal period 28 days
  • 25. Carnegie Mellon ©2002 Moon Exploration Objectives •Measure elemental and mineralogical composition of mantle material in South-Pole Aitken Basin •Assess volatile and mineral resources •Measure surface-bounded atmosphere •Quantify regolith processes Clementine 1994 Lunar South Pole
  • 26.
  • 27. Carnegie Mellon ©2002 Rover in Terminator Polar Circumnavigation Latitude 85° Distance 1895.2 km Duration 28 days Speed 2.8 KPH, 0.8 m/s Comm Lag ~3s Moon Mission Scenario •Polar circumnavigation •Dawn-following in terminator •Orbiter for communication Mission Options •Lower latitude at higher speed •Transit between peaks of perpetual light Mission Predecessors and Precursors •Lunar Prospector Polar Orbiter
  • 28. Carnegie Mellon ©2002 Moon Technology •High efficiency solar cells •Extreme surface mobility •Resource-cognizant navigation •Billion-cycle components •Electrostatic dust mitigation •Subsurface access and shallow drilling •Miniaturized in situ sample processing and instruments
  • 29. Carnegie Mellon ©2002 Mars Notable Characteristics •Low solar irradiance •Tenuous atmosphere •Global dust storms •Smooth northern hemisphere, rough southern hemisphere •Polar caps with water and CO2 ice Planetary Parameters Planet Radius 3393 km Maximum Temperature - 89 o C Mean Temperature - 65 o C Minimum Temperature - 31 o C Surface gravity 3.72 m/s2 Solar Irradiance 589 W/m2 Diurnal period 1.03 days North Days South Summer 183 Winter Autumn 147 Spring Winter 158 Summer Spring 199 Autumn 687
  • 30. Carnegie Mellon ©2002 Mars Exploration Objectives •Determine composition and distribution of surface features; volcanics, impact structures, aqueous features •Map distribution of water/ice including subsurface •Observe and age date aqueous features •Seek and characterize biogenic material •Assess mineral and volatile resources for future missions MOLA Image of H2 distribution
  • 31.
  • 32. Carnegie Mellon ©2002 Mars Mission Scenario •Mid-to-high latitude circumnavigation moves south during northern winter •Solar power •Migrate between 30°and 80°annually •Moderate seasonal temperatures •Hibernation at night •6134 km annually (+ 100% margin) Mission Options •South polar circumnavigation •Variations to reduce distance and duration Migratory Traverse Distance 61337 km Speed 4.3 KPH, 1.2 m/s Duration 10 years Minimum Comm Lag ~4min Maximum Comm Lag ~12min
  • 33. Carnegie Mellon ©2002 Mars Technology •Rough terrain navigational autonomy •Resource cognizance •Low-mass, long-life components • Redundant modes • Motors - lubrication • Solar cells - degradation •Electrostatic / dust resistance •Miniaturized instruments and subsurface access Martian North Polar Cap
  • 34. Carnegie Mellon ©2002 Physical parameters describe planetary environment Assessing Challenges • Gravity • Mean Distance from Earth • Mean Insolation • Surface Pressure • Solar Wind / Radiation at Surface • Ambient Temperature • Diurnal Temperature Cycle • Mean Wind Force • Obstacle Distribution • Slope Distribution
  • 35. Carnegie Mellon ©2002 Gravity Mean Distance from Earth Mean Insolation Pressure at Surface Solar Wind / Radiation at Surface Ambient Temperature Diurnal Temperature Cycling Mean Wind Force Obstacle Distribution Slope Distribution MERCURY -0.7 0.8 0.9 0.0 1.0 0.3 1.0 -0.6 0.9 0.9 VENUS -0.1 0.8 -0.1 1.0 0.0 1.0 0.0 0.4 -0.1 -0.1 MOON -1.0 0.0 0.1 0.0 0.8 0.1 0.4 -0.6 0.7 0.7 MARS -0.7 1.0 0.0 0.0 0.6 0.2 0.1 -0.4 0.4 0.4 PLANET ENVIRONMENTAL Planetary Environments Numbers are based on planetary parameters or estimates Normalized over the range of values and offset to Earth equals 0 Green: high magnitude and Red: low magnitude
  • 36. Carnegie Mellon ©2002 Relate the impact of the environment on rover performance metrics: Assessing Challenges • Power Balance • Mass • Volume • Trafficability • Maneuverability • Terrainability • Speed • Usability • Data Volume • Reliability • Sustainability • Survivability
  • 37. Carnegie Mellon ©2002 Environment and Performance Identify relationships between rover performance and environment Green: directly proportional Red: inversely proportional Gravity Average Distance from Earth Insolation Pressure at Surface Solar Wind / Radiation Ambient Temperature Diurnal Temperature Cycling Mean Wind Force Obstacle Distribution Slope Distribution m / s2 Light-seconds W / m2 atm K (from operating) K (amplitude) N Power Balance n P N Minimized Mass Minimized Volume Trafficability N N N Maneuverability N N Terrainability N N Speed N N Usability Data Volume N N Reliability N N N N N N N N Sustainability P N N Survivability N N N N N n N PERFORMANCE METRICS ENVIRONMENTAL
  • 38. Carnegie Mellon ©2002 Performance Correlations Consider performance metrics that are correlated Green: directly proportional Red: inversely proportional Power Balance Minimized Mass Minimized Volume Trafficability Maneuverability Terrainability Speed Usability Data Volume Reliability Sustainability Survivability Power Balance P N N Minimized Mass P Minimized Volume P Trafficability P Maneuverability P Terrainability P Speed P P P Usability P P P Data Volume P Reliability P P P P N P Sustainability P Survivability P P P N PERFORMANCE METRICS PERFORMANCE METRICS
  • 39. Carnegie Mellon ©2002 Assessing Challenges Derive the challenges posed by planetary environments in terms of rover performance MERCURY Power Balance 3.7 Trafficability 0.0 Maneuverability -0.7 Terrainability -0.3 Speed -3.4 Usability -8.5 Data Volume -2.8 Reliability -4.4 Sustainability -0.1 Survivability -3.8 PERFORMANCE METRICS VENUS -1.7 -0.6 -0.7 -0.3 0.0 -6.0 -0.8 -3.7 -1.0 -2.2 MOON 2.3 0.0 -1.0 -0.1 -2.8 -3.4 -1.9 -2.2 -0.6 -1.1 MARS 1.1 0.0 -0.7 0.0 -1.7 -5.0 -2.3 -2.3 -0.6 -1.3 Relationships of Environment to Performance Metrics Descriptions of Planetary Environments Relationships between Performance Metrics Challenges of Planetary Environments
  • 40. Carnegie Mellon ©2002 Performance Metrics With Respect to Earth -10.0 -8.0 -6.0 -4.0 -2.0 0.0 2.0 4.0 6.0 MERCURY VENUS MOON MARS ` Power Balance Trafficability Maneuverability Terrainability Speed Usability Data Volume Reliability Sustainability Survivability EARTH
  • 41. Carnegie Mellon ©2002 Assesing Challenges Relate rover configuration parameters and performance metrics—what technologies most effect the environmental challenges posed Select configuration parameters that improve performance metrics and do not negatively impact performance that the environment already supports Relationships of Configuration to Performance Metrics Challenges of Planetary Environments Technologies that Effect Challenges
  • 42. Carnegie Mellon ©2002 Configuration and Performance Output Longevity Center of Mass Hieght Wheel Base Mass Volume Max Continuous Torque Max Peak Torque Speed Power Consumption MTTF Redundant Components Chassis Steering Power Loss Data Rate Transmitted Power Availability Computation Memory MTBF Output Mass Volume MTTF Input from Environment Mission / Goal Planning Resource Monitoring Health Monitoring Navigation / Obstacle Avoidance Control Localization Site Mapping Sample Acquisition and Handling Science Data Understanding Exploration and Discovery W s m m kg m3 N m N m m / s W W % W / deg bits / s W % MIPS bits s J kg m3 s W Power Balance P N N N N N N N P Minimized Mass N N P N Minimized Volume N N N P Trafficability P P P Maneuverability N P P Terrainability P P P Speed P P P Usability P P P P P P P P P P P Data Volume P P P P P P P P Reliability P P P P P P P P P P P Sustainability P P P P P Survivability P N P P P P P CONFIGURATION PARAMETERS CONFIGURATION PARAMETERS PERFORMANCE METRICS AUTONOMY POWER LOCOMOTION COMM COMPUTING THERMAL
  • 43. Carnegie Mellon ©2002 Mission Technology Needs Output Longevity Center of Mass Hieght Wheel Base Mass Volume Max Continuous Torque Max Peak Torque Speed Power Consumption MTTF Redundant Components Chassis Steering Power Loss Data Rate Transmitted Power Availability Computation Memory MTBF Output Mass Volume MTTF Mission / Goal Planning Resource Monitoring Health Monitoring Navigation / Obstacle Avoidance Control Localization Site Mapping Sample Acquisition and Handling Science Data Understanding Exploration and Discovery MERCURY 0.0 0.0 0.1 0.1 0.0 0.0 -0.9 0.0 -0.1 -0.9 0.0 1.0 -1.0 2.7 0.2 3.7 1.8 2.7 4.0 1.1 0.0 0.0 0.0 1.0 0.0 1.0 2.9 5.0 3.1 2.7 3.7 2.7 2.7 VENUS 0.6 0.4 0.1 0.1 0.0 0.0 -0.4 0.4 -0.8 -0.6 0.4 1.4 -0.9 2.5 0.7 3.9 1.9 2.5 4.4 1.6 0.0 0.0 0.4 1.4 1.0 1.4 2.5 5.0 3.6 2.5 3.9 2.5 2.5 MOON 0.0 0.3 0.1 0.1 0.0 0.0 -1.1 -0.6 0.8 -1.1 0.3 1.0 -1.6 2.5 -0.1 3.5 1.4 2.5 3.2 0.4 0.0 0.0 0.3 1.0 0.3 1.0 3.3 5.0 2.6 2.5 3.5 2.5 2.5 MARS 0.0 0.3 0.0 0.0 0.0 0.0 -0.5 0.1 0.2 -0.5 0.3 1.0 -0.8 3.3 0.5 4.4 2.8 3.3 3.9 1.1 0.0 0.0 0.3 1.0 0.3 1.0 2.7 5.0 3.3 3.3 4.4 3.3 3.3 CONFIGURATION PARAMETERS POWER LOCOMOTION COMM COMPUTING AUTONOMY THERMAL Technology positively effects many performance challenges Technology positively effects few performance challenges Focus on rover configuration parameters that improve performance
  • 44. Carnegie Mellon ©2002 Rover Technology Issues Sufficient Power • Reliable, low-mass, long-duration power sources • Resource cognizance Thermal Extremes and Cycling • Extreme temperature components • Efficient thermal regulation, heat flow in the terminator Reliable Mobility • Reliable, low-mass mobility mechanisms • Stable extreme terrain locomotion Necessary Autonomy • Autonomy in localization, navigation, and control • Brain versus brawn, minimal communication and oversight Long-term Sustainability • Very long-duration components and algorithms • High bandwidth and availability communication
  • 45. Carnegie Mellon ©2002 Exploration Issues Miniturized Instruments •In Situ Observation •Age Dating •Biogenic Organic Detection Sample Acquisition and Preparation Science Data Understanding •Automated calibration and data quality assessment •Automated sample selection
  • 46. Carnegie Mellon ©2002 Summary Global surface exploration, which is largely complete for the Earth, is appropriate for all the terrestrial planets. Planetary circumnavigation results from long- duration exploration in some scenarios Planetary circumnavigation has scientific, technological and programmatic advantages
  • 49. Carnegie Mellon ©2002 Velocity of One-day Circumnavigation Velocity Required For Single Day Circumnavigation 1669.756 1644.389 1569.058 1446.052 1279.108 1073.299 834.878 571.090 289.950 145.529 862.413 849.311 810.403 746.872 660.647 554.348 431.206 294.963 149.756 75.164 0.100 1.000 10.000 100.000 1000.000 10000.000 0 10 20 30 40 50 60 70 80 90 latitude (degrees) velocity (km/hr) Earth Mars Mercury Venus Moon
  • 50. Carnegie Mellon ©2002 NRC Solar System Exploration Study Objectives Solar System Formation Volatiles & Organics Habitable Worlds Planetary Processes Missions (Inner Planets) Mercury Orbiter South Pole-Aitken Basin Sample Return Venus In-Situ Explorer Mars Long-Lived Lander Network Mercury Sample Return Venus Surface Sample Return Articulate important investigations in planetary science and prioritize missions
  • 51. Carnegie Mellon ©2002 NEXT Space Robotics Study Assess the current and projected state-of-the-art in space robotics including surface exploration Challenges relative to circumnavigation: Minor Moderate Major Obstacle Detection Map Building Localization Obstacle Avoidance Health Monitoring Terrain Detection Path Execution Path Planning Science Autonomy Coverage Planning Resource Planning Exploration Mission Planning
  • 53. Carnegie Mellon ©2002 Next Space Robotics Study Localization requires significant prior knowledge Using proprioception Visual odometry Using fixed beacons Using natural features Without global map Current Nominal 10years Intense 10years Breakthrough 0 2 4 6 8 10 12 14
  • 54. Carnegie Mellon ©2002 Solar Powered Circumnavigation Perpetual exploration through synchronization with the Sun to provide continuous energy Remain in favorable sun position and avoid extreme temperatures by following dawn in the terminator
  • 55. Carnegie Mellon ©2002 Conditions Favorable to Solar Power High solar flux •Providing abundant solar energy Moderate gravity •Resulting in lower locomotive power Small planetary diameter Long rotational period •Less speed required for planetary circumnavigation High planetary axial tilt •Long summer for polar exploration
  • 56. Carnegie Mellon ©2002 Kilometers Arctic Field Experiment Demonstrate concept of sun- synchronous navigation and quantify performance Conduct 24-hour experiments in planetary-analog terrain
  • 58. Carnegie Mellon ©2002 Sun-Synchronous Experiment Von Braun Planitia •7% (max 34%) obstacle density Operation •No intervention •Autonomous 90% Power •Completed on schedule with batteries charged Distance: 6.1km
  • 59. Carnegie Mellon ©2002 Sun-Synchronous Experiment Sun-synchrony •Average heading tracks path with average near zero •Some deviation including reversals Relative Occurance of Heading Error 0 1 2 3 4 5 6 7 8 9 10 -179 -169 -159 -149 -139 -129 -119 -109 -99 -89 -79 -69 -59 -49 -39 -29 -19 -9 1 11 21 31 41 51 61 71 81 91 101 111 121 131 141 151 161 171 Heading Error % Occurrence
  • 60. Carnegie Mellon ©2002 Reliability, Sustainability, Survivability Time t = tsustainability Fault Probability, P F Reliability is the probability of correct operation: 1 – PF(t) Survivability is the probability that a fault will end the mission Sustainability is the time after which faults become unacceptably likely PF = max_allowable
  • 61. Carnegie Mellon ©2002 Trafficability, Maneuverability, Terrainability Trafficability • The ability for a vehicle to drive through terrain • Effected by traction, torque, power Maneuverability • The ability for a vehicle to drive around obstacles • Effected by steering response, minimum turning radius Terrainability • The ability for a vehicle to remain stable • Effected by center-of-gravity, statics, dynamics
  • 62. Carnegie Mellon ©2002 Improving Technology Assessment Include more quantitative relationships between configuration parameters and performance metrics •More subtle than “direct” or “inverse” proportionality is needed to made design decisions Enrich the model with more parameters •A more complete set of environmental parameters •Configuration parameters that better cover design space •Performance metrics that better cover launch, landing and science Add the ability to evaluate particular mission scenarios