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Aerocapture Technology - 123SeminarsOnly

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<strong>Aerocapture</strong> <strong>Technology</strong><br />

www.nasa.gov<br />

Dr. Thomas Spilker<br />

Planetary Scientist / Engineer, Jet Propulsion Laboratory / Caltech<br />

Michelle M. Munk<br />

In-Space Propulsion <strong>Aerocapture</strong> Manager, NASA-Langley Research Center<br />

Decadal Survey Steering Committee Meeting | February 22, 2010<br />

1


Introduction to <strong>Aerocapture</strong><br />

Mission Benefits / Missions Enabled<br />

Current Status of <strong>Aerocapture</strong><br />

Plan and Costs to Flight<br />

Outline<br />

2


Atmospheric<br />

Drag<br />

Reduces Orbit<br />

Period<br />

Hyperbolic<br />

Approach<br />

Aerobraking<br />

Orbit<br />

Insertion<br />

Burn<br />

Aerobraking vs <strong>Aerocapture</strong><br />

Many Passes<br />

Through Upper<br />

Atmosphere<br />

Entry<br />

targeting<br />

burn<br />

Periapsis<br />

raise<br />

maneuver<br />

(propulsive)<br />

<strong>Aerocapture</strong><br />

Jettison<br />

Aeroshell<br />

Energy<br />

dissipation/<br />

Autonomous<br />

guidance<br />

Target<br />

orbit<br />

<strong>Aerocapture</strong>: A vehicle uses active<br />

control to autonomously guide itself<br />

to an atmospheric exit target,<br />

establishing a final, low orbit about a<br />

body in a single atmospheric pass.<br />

3


The !V necessary to slow from a<br />

hyperbolic approach trajectory to a<br />

useful science orbit is<br />

!V = V phyp - V circ<br />

The rocket equation shows why<br />

aerocapture is so advantageous,<br />

masswise:<br />

For a propulsive capture, the mass<br />

increases exponentially with the !V;<br />

for aerocapture, the mass of the<br />

aeroshell is linear with !V.<br />

The <strong>Aerocapture</strong> Advantage<br />

Examples for Circular Orbit Insertion<br />

Mars<br />

Titan<br />

Venus<br />

Neptune<br />

Saturn<br />

4


<strong>Aerocapture</strong>’s Advantages to Science<br />

• Advantage: greater delivered mass into orbit at the<br />

destination<br />

• It’s all about mass – more mass yields better science<br />

• More instruments, or higher-performance instruments<br />

• More mass for higher-performance subsystems that support the<br />

science<br />

• Power – for the instruments, and other support subsystems<br />

• Telecommunications – to downlink larger data volumes<br />

• Propulsion – to get the spacecraft to locations it wouldn’t access<br />

otherwise<br />

• Onboard data storage<br />

• Etc…<br />

• Structure – to hold all this together<br />

• Advantage: reduced trip times to distant destinations<br />

• Spend less time in the cruise phase, more in the science phase<br />

• Stay within the lifetimes of lifetime-limited components<br />

5


Sample <strong>Aerocapture</strong> Benefits for Robotic Missions<br />

Mission - Science Orbit<br />

Nominal<br />

Orbit<br />

Insertion<br />

!V, km/s<br />

Best A/C<br />

Mass, kg<br />

Best<br />

non-A/C<br />

Mass, kg<br />

A/C %<br />

Increase<br />

Launch<br />

Vehicle<br />

Decrease?<br />

Venus V1 - 300 km circ 4.6 5078 2834 79 Yes<br />

Venus V2 - 8500 x 300 km 3.3 5078 3542 43 Yes<br />

Mars M1 - 300 km circ 2.4 5232 4556 15 No<br />

Mars M2 - ~1 Sol ellipse 1.2 5232 4983 5 No<br />

Jupiter J1 - 2000 km circ 17.0 2262


Titan <strong>Aerocapture</strong> Systems Study Concept<br />

“Titan Explorer”-type mission based on SSE<br />

Roadmap circa 2001 – direct Titan orbit<br />

Detailed analysis by multi-Center team of<br />

discipline experts (many published refs)<br />

Using <strong>Aerocapture</strong> and SEP,<br />

• fit on smaller launch vehicle<br />

• cut trip time in half<br />

versus a chemical mission.<br />

2.4 m diameter HGA<br />

3.75 m diameter<br />

Aeroshell<br />

Ref: “<strong>Aerocapture</strong> Systems Analysis for a Titan Mission”, NASA TM 2006-214273, March 2006.<br />

Lander<br />

Orbiter<br />

SEP Prop<br />

Module<br />

Solar<br />

Arrays<br />

7


Characterizing Atmospheric Uncertainties<br />

Variability We Can Model (season, latitude, etc.)<br />

Measurement Uncertainty (Big improvement for Titan after Huygens/Cassini)<br />

Residual Uncertainty (Monte-Carlo-modeled waves, turbulence, etc.)<br />

Neptune<br />

Titan<br />

Titan<br />

Mars<br />

Earth<br />

0 10 20 30 40 50 60 70<br />

Variation, % of Mean<br />

Post Cassini / Huygens<br />

Density Variation, % of Mean (at <strong>Aerocapture</strong> altitudes)<br />

• Residual uncertainty about the same for Mars and Titan; higher for Neptune<br />

• Titan’s overall variation roughly same as Earth, after Cassini/Huygens<br />

8


Trajectory Simulations Include Realistic Global<br />

Reference Atmosphere Models<br />

Global Reference Atmosphere<br />

Models (GRAM)<br />

• Provides atmosphere parameters<br />

(density, pressure, temperature)<br />

vs. altitude, latitude, longitude,<br />

season, and time of day<br />

• Earth GRAM used for Space<br />

Shuttle, Genesis, Stardust<br />

• Mars GRAM used for Pathfinder,<br />

MER, MGS, Odyssey, MRO, MSL<br />

• Titan, Neptune, Venus GRAM<br />

modeled using same approach<br />

as Mars GRAM<br />

• Titan GRAM profiles validated<br />

against Cassini/Huygens<br />

measurements<br />

Models include variability and<br />

random perturbations for Monte<br />

Carlo trajectory analysis<br />

• Includes uncertainties in current<br />

estimates derived from scientific<br />

measurements<br />

• Includes perturbations based on<br />

models of dynamic processes<br />

2000 Perturbed Density Profiles<br />

from Mars GRAM<br />

Aerobraking Altitudes<br />

<strong>Aerocapture</strong><br />

Altitudes<br />

9


Titan-GRAM Model vs Cassini-Huygens Data<br />

<strong>Aerocapture</strong><br />

min alt<br />

<strong>Aerocapture</strong> Minimum Alt Range <strong>Aerocapture</strong> to Orbit Alt Range<br />

Titan-GRAM conservatively bounds the density observations<br />

from HASI and INMS<br />

Ref.: Justh and Justus, “Comparisons of Huygens Entry Data and Titan Remote Sensing Observations with the<br />

Titan Global Reference Atmospheric Model (Titan-GRAM)”<br />

10


!<br />

!<br />

!<br />

!<br />

!<br />

!<br />

!<br />

Titan <strong>Aerocapture</strong> Technologies - Ready!<br />

Enabling Technologies - No new enabling technology required<br />

Strongly Enhancing Technologies<br />

Aeroheating methods development, validation<br />

• Large uncertainties existed at time of analysis, further work and Cassini data all but<br />

eliminated<br />

TPS Material Testing<br />

• TPS materials were not tested against then-expected radiative heating at Titan;<br />

testing was done AND radiative environment reduced significantly in models<br />

Atmosphere Modeling<br />

• Model validated against Cassini/Huygens data<br />

Enhancing Technologies<br />

Aeroshell lightweight structures - reduced aerocapture mass<br />

Guidance - Existing guidance algorithms have been demonstrated to<br />

provide acceptable performance, improvements could provide<br />

increased robustness<br />

Simulation - Huygens trajectory reconstruction, statistics and modeling<br />

upgrades<br />

Mass properties/structures tool - systems analysis capability<br />

improvement, concept trades<br />

11


300 x 300 km<br />

<strong>Aerocapture</strong> Benefit for a Venus Mission<br />

1165 kg Launch Vehicle Capability<br />

Delta 2925H-10, C3 = 8.3 km 2 /s 2<br />

Into 300 x 300 km Venus orbit with same launch vehicle, <strong>Aerocapture</strong> delivers:<br />

• 1.8x more mass into orbit than aerobraking<br />

• 6.2x more mass into orbit than all chemical<br />

Reference: “Systems Analysis for a Venus <strong>Aerocapture</strong> Mission”, NASA TM 2006-214291, April 2006<br />

Mass savings will<br />

scale up for<br />

Flagship-class<br />

mission<br />

Venus Orbiter<br />

(OML Design Only)<br />

Ø 2.65 m<br />

12


Example Monte Carlo Simulation Results:<br />

Venus <strong>Aerocapture</strong><br />

100%<br />

successful<br />

capture<br />

97.7% !V performed<br />

by <strong>Aerocapture</strong><br />

13


Neptune Orbiter <strong>Aerocapture</strong> System Concept<br />

Mass margin provides opportunity for<br />

• Third probe<br />

• Increased aeroshell size for possible reduction in<br />

aeroheating rates/loads, TPS thickness<br />

requirements, surface recession<br />

Propulsive mission is too massive for Delta IV-H<br />

<strong>Aerocapture</strong> is ENABLING<br />

Orbiter<br />

2.88 m Length<br />

Flattened Ellipsled<br />

Aeroshell<br />

2 Probes<br />

Orbiter<br />

Reference: “Systems Analysis for a Neptune <strong>Aerocapture</strong> Mission”, NASA TM 2006-214300, May 2006<br />

35% Dry<br />

Margin at<br />

Orbiter and<br />

SEP Level<br />

5m Fairing<br />

Solar<br />

arrays<br />

SEP Prop<br />

Module<br />

14


Total Heat Load (kJ/cm 2 )<br />

1.6<br />

1.4<br />

1.2<br />

1.0<br />

.8<br />

.6<br />

.4<br />

.2<br />

0<br />

Neptune <strong>Aerocapture</strong> Challenges: Aeroheating, TPS<br />

Zone 4<br />

(includes<br />

base)<br />

Low<br />

Zone 2<br />

2.88 m<br />

Zone 2 – Wind<br />

TPS Sizing<br />

Radiative<br />

Convective<br />

Ref<br />

Med<br />

Zone 3<br />

High<br />

Outside of<br />

Expected Range<br />

Zone 1<br />

~0.74 m<br />

16<br />

14<br />

12<br />

10<br />

8<br />

6<br />

4<br />

2<br />

0<br />

Total Peak Heat Rate (kW/cm 2 )<br />

• TPS developments and interfaces<br />

will require a significant effort<br />

• No facility exists for testing these<br />

heating levels, or the combined<br />

convective/radiative environment<br />

• Manufacturing and shape change<br />

due to recession is challenging<br />

• New aerodynamic shape<br />

Total Heat Load (kJ/cm 2 )<br />

4.0<br />

3.5<br />

3.0<br />

2.5<br />

2.0<br />

1.5<br />

1.0<br />

.5<br />

0<br />

Zone 1 – Nose<br />

TPS Sizing<br />

Radiative<br />

Convective<br />

Low<br />

Ref<br />

Med<br />

High<br />

Outside of<br />

Expected Range<br />

40<br />

35<br />

30<br />

25<br />

20<br />

15<br />

10<br />

5<br />

0<br />

Total Peak Heat Rate<br />

(kW/cm2 )<br />

15


Top-Level <strong>Aerocapture</strong> Infusion Roadmap<br />

In-Space Propulsion <strong>Technology</strong><br />

(2002+)<br />

Systems Analysis<br />

<strong>Technology</strong> Development<br />

Aeroshells and TPS<br />

Aerothermal Models<br />

Guidance, Navigation and Control<br />

Instrumentation<br />

Additional development:<br />

Aerothermal<br />

TPS/test facilities<br />

Aerodynamics<br />

Structures/manufacturing<br />

Earth Orbit Flight<br />

Test (2015)<br />

Inner Planet/OP Satellite<br />

<strong>Aerocapture</strong> Missions (2018+)<br />

(Low L/D, modest TPS needs)<br />

Mars Titan<br />

Venus<br />

Additional development:<br />

Aerothermal<br />

TPS/test facilities<br />

Aerodynamics<br />

Structures/manufacturing<br />

Giant Planet <strong>Aerocapture</strong> Missions (2025+)<br />

(High L/D, substantial TPS needs)<br />

Jupiter Saturn Uranus Neptune


ISPT’s Low-Risk Aeroshell Mass Improvements<br />

Warm Structure System Model - based on MER, MPF, validated with testing<br />

For environments up to 300 W/cm2 HT-424<br />

for adhesive<br />

Aluminum<br />

honeycomb<br />

MER SLA-561V System 250 deg C<br />

Areal Density = 2.07 lb/ft 2 Areal Density = 1.78 lb/ft 2<br />

Genesis Carbon-Carbon<br />

Warm Structure SLA-561V System 316 deg C<br />

Hot Structure System Model - based on Genesis, validated with testing<br />

For environments up to 700 W/cm2 Final System included<br />

backup aluminum<br />

Honeycomb structure<br />

Modified RS9<br />

for adhesive<br />

Graphite polycyanate<br />

honeycomb<br />

Final System includes<br />

11-layer MLI<br />

and high-temp coating<br />

Hot Structure<br />

Carbon-Carbon/Calcarb<br />

Areal Density = 3.65 lb/ft 2 Areal Density = 2.50 lb/ft 2<br />

14%<br />

Improvement<br />

31%<br />

Improvement<br />

17


Aeroshell Manufacture and Test with Ablator<br />

Family System<br />

ARA Material Density Heating Range New Missions Features<br />

SRAM-17 0.27 g/cm 2 115 – 210 W/cm 2 Titan, Mars Robust Char<br />

SRAM-20 0.32 g/cm 2 140 – 260 W/cm 2 Earth Acap, Mars Low Recession<br />

PhenCarb-20 0.32 g/cm 2 200 – 500 W/cm 2 Large Mars, EEV High Heating<br />

PhenCarb-32 0.51 g/cm 2 500 – 1,100 W/cm 2 EEV, Venus, Neptune Severe Heating<br />

1-m SRAM-20 aeroshell test at Solar Tower<br />

18


Power<br />

Supply<br />

Command &<br />

Telemetry<br />

Processing<br />

Main<br />

Simulation<br />

Processor<br />

Simulation I/O<br />

Cards for IMU<br />

& Thrusters<br />

GN&C Flight Testbed is Complete<br />

Spacecraft Computer with MOAB<br />

Card (Broad Reach Engineering)<br />

Command & Telemetry<br />

Workstation<br />

19


Status of <strong>Aerocapture</strong> <strong>Technology</strong><br />

• ISPT has made major strides in ground-based<br />

development over the past 8 years<br />

• GN&C Hardware-in-the-Loop Testbed (guidance coded in flight<br />

software)<br />

• Lighter, more robust structural and TPS concepts matured through<br />

arcjet, structural, and environmental testing and model validation,<br />

culminating in two 2-meter and larger aeroshell manufacturing<br />

demonstrations<br />

• Aerothermal and Atmospheric models greatly matured (better<br />

prediction capability)<br />

• High-fidelity statistical simulation capability applied to several<br />

destinations (same tool used for operational planetary entry<br />

missions)<br />

• Stoplight chart on next page show summary of “readiness”<br />

of each subsystem for key destinations<br />

20


Destination<br />

Subsystem<br />

Atmosphere<br />

Goal: Capture Physics<br />

Aerodynamics<br />

Goal: Errors ! 2%<br />

GN&C<br />

Goal: Robust<br />

performance for 4-6<br />

DOF simulations<br />

TPS<br />

Goal: Reduce SOA by<br />

30%+, expand TPS<br />

choices<br />

Structures<br />

Goal: Reduce SOA<br />

mass by 25%<br />

Aerothermal<br />

Goal: Models match<br />

within 15%<br />

System<br />

Goal: Robust<br />

performance with<br />

ready technology<br />

Venus-GRAM (2004)<br />

based on world-wide<br />

VIRA.<br />

Heritage shape, well<br />

understood aerodynamics<br />

CA =±3%, CN =±5%,<br />

" TRIM =±2%<br />

APC algorithm captures<br />

96% of corridor<br />

More testing needed on<br />

efficient mid-density TPS.<br />

Combined convective<br />

and radiative facility<br />

needed.<br />

High-temp systems will<br />

reduce mass by 31%.<br />

Convective models<br />

match within 20% laminar,<br />

45% with turbulence.<br />

Radiative models agree<br />

within 50%<br />

Accomplishes 97.7% of<br />

!V to achieve 300 x 300<br />

km orbit.<br />

<strong>Aerocapture</strong> <strong>Technology</strong> Subsystem<br />

Readiness<br />

Venus Earth Mars Titan Neptune<br />

Earth-GRAM (1974)<br />

validated by Space Shuttle<br />

Heritage shape, well<br />

understood aerodynamics<br />

CA =±3%, CN =±5%,<br />

" TRIM =±2%<br />

Small delivery errors. APC<br />

algorithm captures 97% of<br />

corridor<br />

<strong>Technology</strong> ready for ST9.<br />

LMA hot structure ready for<br />

arrivals > 10.5 km/s.<br />

High-temp systems will<br />

reduce mass by 14%-30%.<br />

Environment fairly wellknown<br />

from Apollo, Shuttle.<br />

Models match within 15%<br />

Accomplishes 97.2% of !V<br />

to achieve 300 x 130 km<br />

orbit. No known<br />

technology gaps.<br />

Mars-GRAM (1988)<br />

continuously updated with<br />

latest mission data.<br />

Heritage shape, well<br />

understood aerodynamics<br />

CA =±3%, CN =±5%,<br />

" TRIM =±2%<br />

Small delivery errors using<br />

!DOR. APC algorithm<br />

captures 99% of corridor<br />

ISPT investments have<br />

provided more materials<br />

ready for application to<br />

slow arrivals, and new<br />

ones for faster entries.<br />

High-temp systems will<br />

reduce mass by 14%-<br />

30%.<br />

Convective models agree<br />

within 15%. Radiative:<br />

predict models will agree<br />

within 50% where radiation is<br />

a factor.<br />

Accomplishes 97.8% of<br />

!V to achieve 1400 x 165<br />

km orbit. No known<br />

technology gaps.<br />

Titan-GRAM (2002) based on<br />

Yelle atmosp. Accepted<br />

worldwide to be updated with<br />

Cassini-Huygens data<br />

Heritage shape, well<br />

understood aerodynamics<br />

CA =±3%, CN =±5%,<br />

" TRIM =±2%<br />

Ephemeris accuracy<br />

improved by Cassini-<br />

Huygens. APC algorithm<br />

captures 98% of corridor<br />

ISPT investments have<br />

provided more materials<br />

ready for application.<br />

High-temp systems will<br />

reduce mass by 14%-30%.<br />

Convective models agree<br />

within 15%. Radiative no<br />

longer a concern.<br />

Accomplishes 95.8% of<br />

!V to achieve 1700 x 1700<br />

km orbit. No known<br />

technology gaps.<br />

Ready for Infusion Some Investment Needed Significant Investment Needed<br />

Neptune-GRAM (2003)<br />

developed from Voyager,<br />

other observations<br />

New shape; aerodynamics<br />

to be established.<br />

CA =±8%, CN =±8%,<br />

" TRIM =±10%<br />

APC algorithm with "<br />

control captures 95% of<br />

corridor.<br />

Zoned approach for<br />

mass efficiency. Needs<br />

more investment.<br />

Complex shape, large<br />

scale. Extraction<br />

difficult.<br />

Conditions cannot be<br />

duplicated on Earth in<br />

existing facilities. More<br />

work on models<br />

needed.<br />

Accomplishes 96.9% of<br />

!V to achieve Triton<br />

observ. orbit. ENABLING<br />

21


Status of <strong>Aerocapture</strong> <strong>Technology</strong> (cont’d.)<br />

• <strong>Aerocapture</strong> is ready for either flight validation or mission<br />

implementation, except at Outer Planets<br />

• The community is somewhat divided on the need for a flight validation<br />

before mission infusion<br />

• The experts in the technical fields who understand the system say, “It’s<br />

ready to fly!”<br />

• The scientists/mission managers/proposal reviewers say, “It’s too risky!”<br />

• We have not yet been in a situation where <strong>Aerocapture</strong> enabled a key<br />

Roadmap mission. For small, competed missions, the perceived risk<br />

and cost have eliminated <strong>Aerocapture</strong> early on. The Discovery AO<br />

may remedy this—remains to be seen.<br />

• We do have a consensus: The proper flight validation will reduce<br />

the risk for the first user, and will add <strong>Aerocapture</strong> to the tool set for<br />

those small missions who can’t afford to be the first user.<br />

• We will also continue education and advocacy, to make the user<br />

community more comfortable with <strong>Aerocapture</strong> and its benefits.<br />

22


Resource Estimates for <strong>Aerocapture</strong><br />

Validation<br />

• NASA’s Chief Engineer requested an Issue Paper in June of 2009,<br />

to identify this cross-cutting technology as a gap in the current<br />

NASA budget<br />

• Was put on hold due to expectations of new technology program<br />

• Basis of Estimate:<br />

• NMP ST9 with margin for inflation and schedule lengthening (40 mo)<br />

• Phased with 60/40 beta curve<br />

• Includes post-flight analysis at higher level than ST9<br />

• Launch vehicle costs not included<br />

• 30% margin is included<br />

• This represents a heavily-instrumented vehicle with a new thermal<br />

protection system; some reductions could be realized<br />

If this validation reduces the launch vehicle class of just one mission,<br />

we’ve recovered our investment.<br />

For information purposes only. Pre-decisional.<br />

23


Top-Level <strong>Aerocapture</strong> Infusion Roadmap<br />

In-Space Propulsion <strong>Technology</strong><br />

(2002+)<br />

Systems Analysis<br />

<strong>Technology</strong> Development<br />

Aeroshells and TPS<br />

Aerothermal Models<br />

Guidance, Navigation and Control<br />

Instrumentation<br />

Additional development:<br />

Aerothermal<br />

TPS/test facilities<br />

Aerodynamics<br />

Structures/manufacturing<br />

$30-50M<br />

$100-150M<br />

(no LV)<br />

Earth Orbit Flight<br />

Test (2015)<br />

Inner Planet/OP Satellite<br />

<strong>Aerocapture</strong> Missions (2018+)<br />

(Low L/D, modest TPS needs)<br />

Mars Titan<br />

Venus<br />

Additional development:<br />

Aerothermal<br />

TPS/test facilities<br />

Aerodynamics<br />

Structures/manufacturing<br />

Giant Planet <strong>Aerocapture</strong> Missions (2025+)<br />

(High L/D, substantial TPS needs)<br />

Jupiter Saturn Uranus Neptune


<strong>Aerocapture</strong> Development Summary<br />

• <strong>Aerocapture</strong> is enabling or strongly enhancing<br />

for many of the destinations in the Solar System,<br />

saving launch mass, trip time, and cost.<br />

• <strong>Aerocapture</strong> is ready for flight infusion or<br />

validation.<br />

• A flight validation at Earth, immediately<br />

applicable to inner planets and outer planet<br />

satellites, would cost $100-150M, excluding<br />

launch vehicle.<br />

• Additional ground testing for application to giant<br />

planets would be $30-50M.<br />

• A flight validation would lower first-user cost<br />

and risk. If applicable missions will be on the<br />

Planetary Science Roadmap, we need advocacy<br />

for a flight validation.<br />

• Including entry system experts in mission studies<br />

and review boards could improve risk<br />

perception.<br />

25

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