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Planetary Science Deep Space SmallSat Studies

Planetary Science Deep Space SmallSat Studies (PSDS3)

Small Bodies Assessment Group June 13, 2017

Carolyn Mercer NASA Headquarters

1 SMD CubeSat/SmallSat Approach

Planetary Science Deep Space SmallSat Studies National Academies Report (2016) concluded that have proven their ability to produce high- value science: • Useful as targeted investigations to augment the capabilities of larger missions • Useful to make highly-specific measurements • Constellations of 10-100 CubeSat/SmallSat spacecraft have the potential to enable transformational science

SMD is developing a directorate-wide approach to: • Identify high-priority science objectives in each discipline that can be addressed with CubeSats/SmallSats • Manage program with appropriate cost and risk • Establish a multi-discipline approach and collaboration that helps science teams learn from experiences and grow capability, while avoiding unnecessary duplication • Leverage and partner with a growing commercial sector to collaboratively drive instrument and sensor innovation 2 PLANETARY SCIENCE DEEP SPACE SMALLSAT STUDIES (PSDS3)

• ROSES Appendix C.23 was released on August 19, 2017

• Solicited concept studies for potential CubeSat and SmallSat missions – Focus is on defining planetary science investigations that can be accomplished with small secondary payloads – Concepts sought for 1U to ESPA-class (180kg) missions – Up to $100M mission concepts – Not constrained to fly with any specific existing mission – Will generate ideas to inform future mission planning – Will quantify technology gaps – 6 to 15 awards expected – 10 Selections announced March 20, 2017 – 9 additional selections announced June 9, 2018

Planetary Science Deep Space SmallSat Studies: Awards

Venus Valeria Cottini, CUVE - Cubesat UV Experiment Attila Komjathy, Seismicity Investigation on Using Measurements Tibor Kremic, Seismic and Atmospheric Exploration of Venus (SAEVe) Christophe Sotin, Cupid's Arrow

Moon David Draper, Innovative Strategies for Lunar Surface Exploration Charles Hibbitts, Lunar Water Assessment, Transportation, and Resource Mission (WATER) Noah Petro, Mini Lunar Volatiles (MiLUV) Mission Suzanne Romaine, CubeSat X-ray Telescope (CubeX) Timothy Stubbs, Bi-sat Observations of the Lunar Atmosphere above Swirls (BOLAS)

Small Bodies Benton Clark, CAESAR: CubeSat Encounters for Science and Reconnaissance Tilak Hewagama, Primitive Object Volatile Explorer (PrOVE) Jeffrey Plescia, APEX: Asteroid Probe Experiment

Mars Anthony Colaprete, Aeolus - to study the thermal and wind environment of Michael Collier, PRISM: Regolith Ion Sample Mission Robert Lillis, Mars Ion and Sputtering Escape Network (MISEN) David Minton, Chariot to the of Mars Luca Montabone, Mars Aerosol Tracker (MAT)

Icy Bodies and Outer Kunio Sayanagi, SNAP: Small Next-generation Atmospheric Probe Robert Ebert, MagnetosPheric boundary ExploreR (JUMPER) 4 Cubesat Asteroid Encounters for Science And CAESAR Reconnaissance

Planetary Science Deep Space SmallSat Studies

Build and launch several CAESAR cubesats together or Team Members/Institutions: separately, as secondary payloads on trans-lunar trajectories (e.g., SLS) and use lunar gravity assists to target flybys of Benton Clark, P.I., Lockheed Martin selected . Robert Jedicke, Co-I, University of Hawaii Michael Ravine, Co-I, Malin Space Science Systems Inc. Initial scouting of Flyby Driss Takir, Co-I, SETI Institute diverse asteroid population

Example mission to asteroid 1989 ML ’s shown Orbit

Science Objectives: Mission Overview: 1. Evaluate bulk physical characteristics of several 6U based on LM SkyFire asteroids in 10 m to 1 km size range to provide lunar cubesat on EM-1 constraints on their formation and evolution 2. Determine the thermal properties of these asteroids Visible and IR imaging to evaluate Yarkovsky and YORP effects on trajectory dispersions. 3. Characterize objects that may pose a threat to Lunar gravity assist to target or offer resources for exploration asteroid flyby

APEX Asteroid Probe Experiment

Planetary Science Deep Space SmallSat Studies Team Members/Institutions:

Eric Asphaug – Arizona State Univ. Olivier Barnouin – JHU/APL Mark Boslough – Sandia National Lab. Apophis shape model (Pravec, 2014) Brett Denevi – JHU/APL Carolyn Ernst – JHU/APL Jeff Plescia – JHU/APL Derrick Richardson – Univ. Maryland Andy Rivkin – JHU/APL Nicholas Schmerr – Univ. Maryland Possible spacecraft Seismometer draft configuration – Hongyu Yu – Arizona State Univ. configuration with deployment includes sensor, solar cells, arm extended. electronics and comm.

Mission Overview: Science Objectives: Baseline Spacecraft Configuration 1. Determine the structure of Apophis and observe the 3 axis stabilized, solar power tidal deformation during encounter with Earth 2029 Solar electric propulsion (or possible chemical) 1. Determine rotational dynamics Arm to deploy seismometer on surface 2. Establish physical dimensions Baseline Instrument Payload 3. Determine topography Panchromatic imager 4. Determine interior structure Seismometer 5. Define surface morphology Conops 2. Map Apophis before encounter to define the body Rendezvous with Apophis before encounter 3. Remap Apophis after encounter to detect changes Map and characterize Apophis resulting from tidal forces during encounter Deploy the seismometer Observe deformation during encounter Remap and recharacterize Apophis CubeSat X-ray Telescope for Elemental Abundance CubeX Mapping of Airless Bodies and X-ray Pulsar Navigation SAO Planetary Science Deep Space SmallSat Studies Team Members/Institutions:

PI: Suzanne Romaine1 Science-PI: JaeSub Hong2

Co-Is: Almus Kenter1, Rebecca Masterson3, Larry Nittler4, Keith Gendreau5

Collaborators: Branden Allen2, Ralph Kraft3, Ian Crawford6, Martin Elvis1, Image of Richard Binzel3,William Bonyton7, Jonanthan Grindlay2

Spacecraft 1 and/or Smithsonian Astrophysical Observatory – PI, MiXO, CMOS, SOC 2 Mission Harvard University – Instrument Design, MiXO, SXM 3MIT – Instrument Management, SDD 4Carnegie Inst. of Washington – XRF imaging 5GSFC -- XNAV 6Birkbeck College, UK – Moon science 7University of Arizona – Instrument Design NASA Ames Research Center – Mission Design, MOC

Science Objectives: Mission Overview: • Type, Mass: Secondary Mission, 18 kg in 12U (1 x 2 x 6U) 1. Map the surface elemental composition of >8 target • Solar Panel, Comm.: Max 89W, Iris V2 (Max 300MB/day) regions (~35 – 140 km) of special interest in the Moon • ADCS: ~2 km position knowledge for XNAV, ~30″ pointing using X-ray Fluorescence (XRF): (1) to identify outcrops knowledge for XRF imaging and XNAV of lunar mantles; (2) to study the vertical composition of • 1 year lifetime from a 2023 – 2027 launch for solar max. the lunar crust; (3) to understand the composition of • Elliptical Polar Lunar Orbit with ~14 hr period: insertion to discrete lava flows of a range of ages; (4) to measure the 4000 x 6000 km orbit via primary; low thrust trajectory with composition of permanently shadowed region. Hall thruster to 2000 x 8000 km after 1 year • Operation: 55% XRF, 16% XNAV, 2% Telemetry, 2% EP 2. Conduct the feasibility and performance test of X-ray • Payload: [1] X-ray Imaging Spectrometer (XIS): Miniature X- pulsar timing based deep space navigation (XNAV), to ray Optics (MiXO, >25 cm2 at 1 keV) + 2 CMOS X-ray sensors lower operation costs of space navigation and enable (<200 eV at 6 keV) + 1 high timing resolution SDD (1 µs) autonomous deep space navigation. [2] Solar X-ray Monitor (SXM) : SDD • Payload power, Data: 14W average, 8MB/day

BOLAS Bi-sat Observations of the Lunar Atmosphere above Swirls

Planetary Science Deep Space SmallSat Studies

Team Members/Institutions:

• PI: Timothy J. Stubbs (NASA/GSFC, 695) • GSFC Co-Is: Michael R. Collier, William M. Farrell, John W. Keller, Jared Espley, Michael A. Mesarch, Dean J. Chai, Michael K. Choi • Morehead State Univ. Co-I: Benjamin K. Malphrus Lunar • Tethers Unlimited Co-I: Robert P. Hoyt Swirl • Co., Inc. Co-I: Michael Tsay • GSFC Collaborator: Richard R. Vondrak

Science Objectives: Mission Overview: Investigate the hydrogen cycle (including surface Flight Configuration: BOLAS will deploy a thin, tens of km- hydroxylation/hydration) at the Moon by determining: long tether between two CubeSats enabling them to fly in a 1. the mechanisms and dynamics of lunar hydrogen gravity gradient formation. implantation, and their dependence on composition, The BOLAS center-of-mass (C.O.M.) will be in a quasi- regolith properties, local topography, plasma stable, low maintenance orbit, such that the lower CubeSat conditions, time-of-day, and crustal magnetic fields. can remain at low altitudes for long durations. 2. how this relates to the formation of the lunar “swirls” Mission Architecture: Two similar 12U CubeSats (24U total), collocated with magnetic anomalies (crustal fields) leveraging existing bus and miniaturized subsystems. and space weathering. Instrument Payload: Ion Spectrometer, Energetic Neutral Requires repeated in situ measurements at very low Atom Imager, Plasma Wave System, and . altitudes (<10 km) – orbit-maintenance propulsion Orbit: Low inclination to observe magnetic anomalies/swirls requirements are prohibitive for conventional SmallSats. that are clustered around the equator on short timescales. Mission Lifetime: 1 year (desirable), 1 lunation (minimum). Chariot to the

Planetary Science Deep Space SmallSat Studies Team Members/Institutions: PI: David Minton (Purdue) Co-Is: Briony Horgan (Purdue) David Spencer (Purdue) Philip Christensen (Arizona State University) Zachary Putnam (Univ. of Illinois at Urbana-Champaign) Austin Williams (Tyvak Inc.) Graduate Students Jacob Elliot (Purdue), Rohan Deshmukh (Purdue) Collaborators Andrew Rivkin (JHU/APL), Matija Cuk (SETI), Francesca DeMeo (MIT), Erik Asphaug (ASU)

Science Objectives: Mission Overview: 1. Determine the origin of moons of Mars, Phobos • Will piggyback on another Mars mission for launch, but and will be a free flier after separation from the upper stage 2. Evaluate the potential for resource extraction to • Cruise/aerocapture vehicle with drag modulation support human exploration on the moons trajectory control 3. Observe the effects of geologic • 12U CubeSat, 3-axis stabilized, electric propulsion processes contributing to the ongoing evolution • One Mars year mapping mission of Phobos & Deimos of the Phobos-Deimos system • Remote sensing instrument suite – Spectroscopy and visible imaging • Mission Operations Center at Purdue University • Science Operations Center at Arizona State University Aeolus A Mission to Study the Winds of Mars

Planetary Science Deep Space SmallSat Studies The Aeolus Spacecraft Team Members/Institutions: 28kkg / 24U / 117W-OAP Spacecraft

Aeolus will make the first direct Mission Overview: 6U Payload

observations of day and nighttime • Aeolus’s inclined orbit allows observations between ±75° and at all winds at all local times local times SHS • Spatial Heterodyne Spectrometers

SHS (SHS) and Mini-TES scan the Aeolus Science Objectives: atmosphere limb providing wind vectors, temperatures and 1. Produce a vertically resolved global wind speed TES aerosol/cloud densities map • SurSeP (Surface Radiometric Sensing 2. Determine the global energy balance of Mars Package) looks nadir measuring the Mini - 3. Correlate wind speeds and surface temperatures total upwelling solar and thermal radiance as well as the surface with CO2 and H2O clouds and dust column temperature and column aerosol/cloud densities density SuRSeP

SNAP Small Next-Generation Atmospheric Probe

Planetary Science Deep Space SmallSat Studies Team Members/Institutions: Kunio M. Sayanagi / Hampton University Robert A. Dillman / NASA Langley Research Center David H. Atkinson / Jet Propulsion Laboratory Amy A. Simon / NASA Goddard Space Flight Center Michael H. Wong / University of California, Berkeley Thomas R. Spilker / Independent Consultant James M. Longuski / Purdue University Sarag J. Saikia / Purdue University Jing Li / NASA Ames Research Center Drew Hope / NASA Langley Research Center

Supported by NASA Langley Research Center Engineering Design Studio

Science Objectives: Mission Overview: SNAP will examine the physical and chemical processes in the Baseline SNAP Mission Configuration atmosphere of to understand the origin and evolution of Add SNAP to Uranus Orbiter and Probe Mission the giant planets and the . Orbiter delivers Main Probe and SNAP to Uranus

Tier-1 Objectives Baseline Probe Configuration Determine spatial differences of the following atmospheric Mass: 30 kg properties from the Main Probe entry site: Aeroshell Diameter: 50 cm 1. Vertical distribution of cloud-forming molecules Probe Power: Primary Batteries 2. Thermal stratification Heatshield Material: HEEET 3. Wind speed as a function of depth Target Atmospheric Pressure: 5 bar

Tier-2 Objectives Notional Payload Augment Main Probe Science Objectives: Atmospheric Structure Instrument: Measures thermal profile 4. Measure abundances of the noble gases (He, Ne, Ar) NanoChem: Detects cloud-forming molecules 5. Measure isotopic ratios of H, C, N, and S Ultrastable Oscillator: Measures wind speeds

A SmallSat to Explore Jupiter’s Magnetospheric Boundaries JUMPER and Image its Emissions

Planetary Science Deep Space SmallSat Studies JUMPER is a Jupiter orbiting Team Members/Institutions: SmallSat mission concept to (i) understand the ’s interaction with Jupiter’s magnetosphere and (ii) quantify the contri- bution from energetic neutral atoms (ENAs) to mass loss from Jupiter’s space environment.

JUMPER will ride to Jupiter onboard another spacecraft such as NASA’s Clipper.

Science Objectives: Spacecraft Overview:

1. Characterize the solar wind upstream of Jupiter’s magnetosphere and provide additional context for studying magnetospheric dynamics by the primary spacecraft.

2. Investigate the modes of solar wind coupling (e.g. magnetic reconnection, Kelvin-Helmholtz waves) along Jupiter’s dayside magnetopause. The spacecraft consists of an ESPA frame supporting four 3. Determine the flux, energy spectra, and spatial double-deployed solar array panels, and four science distribution of energetic neutral atoms (ENAs) instruments. A CubeSat sized electronics vault will house escaping from Jupiter’s magnetosphere. a majority of the electronics, shielding them from radiation.

A small satellite to measure noble Cupid’s Arrow gases in Venus' atmosphere

Planetary Science Deep Space SmallSat Studies Team Members/Institutions: Christophe Sotin JPL Guillaume Avice Caltech John Baker JPL Murray Darrach JPL Anthony Freeman JPL Glenn Lightsey Georgia Tech Bernard Marty Univ. Nancy Stojan Madzunkov JPL Daniel Wenkert JPL Sterling Peet Georgia Tech Terry Stevenson – graduate std. Georgia Tech Atelier team JPL

Science Objectives: Mission Overview: 1. Determine how did the form and evolve? • Several Venus-bound trajectory options to be studied: a) Free-flyer launched directly from Earth 2. Compare the primordial volatile compounds b) Drop-off on a gravity assist flyby of the Earth, Mars, and Venus? c) Drop-off from orbit 3. Determine the volcanic history of Venus • Probe (mass <30 kg; diam. 60 cm) skims through the atmosphere These objectives are achieved by measuring the • At closest approach (below the homopause), spin- stabilized probe grabs a sample of the atmosphere abundances of noble gases (Ne, Ar, Kr, Xe) and • Sample is analyzed in a compact mass spectrometer (4 their isotopic ratios in Venus’ atmosphere below kg, 31 W, 4U CubeSat form factor) the homopause (well mixed atmosphere) • Sample analysis data are relayed back to Earth

Cubesat UV Experiment: Unveil Venus’ UV Absorber with CUVE Cubesat UV Mapping Spectrometer

Planetary Science Deep Space SmallSat Studies Team Members/Institutions: Principal Investigator: Valeria Cottini (University of Maryland College Park) Co-Investigators: Shahid Aslam (NASA, GSFC) Nicolas Gorius (Catholic University of America) Tilak Hewagama (University of Maryland College Park) Giuseppe Piccioni (INAF-IAPS, Italy) Collaborators: Lori Glaze (NASA, GSFC) Nikolay Ignatiev (IKI RAN, Russia) Emiliano D’Aversa (INAF-IAPS, Italy)

Science Objectives: Mission Overview: Baseline Spacecraft Configuration • Nature of the "Unknown” UV-absorber (range 320 – 6U to 12U Cubesat (e.g. Morehead or Dellingr) 490 nm) which drives Venus’ thermal radiative • Cruise < 1.5 year, Science phase > 0.5 year balance • Propulsion: Chemical, EP, cold gas • Abundances and distributions of SO2 and SO at • Power Generation: solar arrays and above Venus’s cloud tops and their correlation • Polar orbit around Venus with the UV absorber (range 190 – 320 nm) • Nadir dayside and nightside observations

• Atmospheric dynamics at the cloud tops using wind tracking (190 – 490 nm) and structure of upper Payload includes (2U, 2kg) clouds • UV spectrometer 190 – 570 nm, 0.3 nm spectral resolution • Nightglow emissions: NO (190-300 nm), CO (205- • UV imager broadband centered at 365 nm 240 nm), O2 (400-500 nm)