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Hayabusa and Hayabusa2 - Challenges for Sample Return from Asteroids -
Makoto Yoshikawa (JAXA)
Cleveland, Ohio, USA October 18, 2016
14th BroadSky Workshop : Opening Up Ways to Deep Space
Lunar and Planetary Missions of Japan
Sakigake
Suisei
1985
Hiten
1990
2007
Kaguya
×Nozomi
2003
2010
1998
IKAROS
Akatsuki
Hayabusa
Hayabusa2
×LUNAR-A
2014
Comet Halley
Moon
Moon
Moon
Mars
Venus
Asteroid Itokawa Asteroid Ryugu
PROCYON
SLIM ×SELENE2
BepiColombo
Mercury
2
Starting Point 1985
Japan's Asteroid Explorations Past, Present, and Future
Hayabusa 2003-2010
Hayabusa2 2014-2020
to Trojans ? S-type
C-type D-type
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Phaethon ((Geminids))
to NEO ?
Technology of Sample Return New technology for asteroid sample return mission
Ion engine Autonomous navigation Sample collection system Re-entry capsule
Hayabusa
Impactor system Ka-band communicaiton
Hayabusa2
Many New technologies
Next: Trojan mission?
4
Science of Sample Return Origin and evolution of the solar system
Ryugu Itokawa
In addition to the science of Itokawa...
Organic matter, H2O
Solar system
Proto solar system disk
HAYABUSA
Earth
The science of Itokawa
Mineralogy, Topography, Structure, Regolith, Meteoroid
Space weathering, Impact, Cosmic ray, Solar wind
Boulder
Molecular cloud 4.6 billion years ago...
• Planetesimal formation : Accumulation and destruction • Evolution from planetesimals to asteroids • Initial material : Minerals, water, organic matters • Material circulation in the early solar system • Relation between asteroids and meteorites
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Hayabusa 1&2 will solve the "Missing Zone"
Formation of CAI*
Formation of Chondrule
Present Condensation melt and evaporation of dust
Orbital evolution
Molecular cloud core
Adhesion/mixture
Near earth asteroid
Protoplanetary disk
metamorphism and differentiation by internal heating
Formation of planetesim
al
Meteorite
Collision and growth of planetesimal
Scattered to outside Fall to center
Asteroid
Collisional destruction and re-accumulation
Heating space weathering
Formation of parent asteroid
Missing Zone
Formation environment and composition of parent asteroid
4.6 billion years ago
*CAI : Calcium-aluminium-rich inclusion
Dust (mineral, H2O, Organic mater)
Planetesimal Catastrophic disruption
Rubble pile
Differentiation
History of Asteroid
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metal core
Idea for sample return began in1985
History of Hayabusa and Hayabusa2
Year
▲ Launch
Hayabusa ▲
launch
Now
Project
Serious troubles in Hayabusa
Post Haybusa2
MUSES-C Sample Analysis
project Started in 1996 Post MUSES-C Post Hayabusa
Preparation
Hayabusa Mk2 Marco Polo
Initial proposal in 2006 Copy of Hayabusa but modified Target : C-type asteroid 1999 JU3 Launch: 2010
New proposal in 2009 Modified Hayabusa adding new challenges Target : C-type asteroid 1999 JU3 (Ryugu) Launch: 2014
7
▲ Earth return
Op. Hyabusa2
2000 01 02 03 04 05 06 07 08 09 10 11 12 13 14 15 16
Objectives : Hayabusa vs Hayabusa-2
1. Science Origin and evolution of the solar system Organic matter, H2O
2. Engineering Technology : more reliable and robust New challenge : ex) impactor
3. Exploration Extend the area that human can reach Spaceguard, Resources, Research for manned mission, etc.
Technological demonstrator Round-trip to asteroid Sample return
Engineering Ion engine Autonomous navigation Sample collection Reentry capsule
Science : Origin and evolution of the solar system Remote sensing observation Sample analysis
Hayabusa Hayabusa2
C-type Asteroid
S-type Asteroid
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Mission Scenario of Hayabusa
Launch 9 May 2003
Earth Swingby 19 May 2004 Asteroid Arrival
12 Sept. 2005
Observations, sampling
Earth Return 13 June 2010
9
Serious troubles
Engineering of Hayabusa 2003.05.09
2005.09.12
2010.06.13
2004.05.19
10
Instrument Module Container
Capsule and Sample
Capsule (June 14, 2010)
Inside the container Small grain Confirmation of Itokawa grain
11
Images of Itokawa
Eastern Side
Western Side
Head
Bottom
1122 12
Summary of Science Results by Remote Sensing
l Mass
l Shape, size, spin
l Density
l Albedo
l Material
l Structure
l etc.
Pyroxene Olivine
Pyroxene and Olivine
Mass::(3.51 ± 0.105) x 1010 kg�� Volume = (1.84 ± 0.092) x 107 m3 Bulk Density::1.9 ± 0.13 g/cm3
Macro-porosity = 40%
Ordinary chondrite
Rubble pile
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Formation of Itokawa parental
body (>20 km)
Thermal metamorphism ((<4.562 Ba))
Catastrophic impact
Itokawa formation Rubble pile asteroid
planetesimal
Solar wind
Space weathering
Galactic cosmic ray
Micro-meteoroids
Escape rate (~10 cm/My)
Grain motion (150y~3My))
Scientific Results from Sample Initial Analysis
100 m
LL chondrite LL5/6 (~800oC) LL4 (~600oC)
Re- accumulation
14
Science Publications 2 June 2006 26 August 2011
15
- A Direct Link Between S-Type Asteroids and Ordinary Chondrites
- Oxygen Isotopic Compositions - Neutron Activation Analysis - Origin and Evolution of Itokawa Regolith - Irradiation History of Itokawa Regolith Space
-Rubble-pile structure -Near-infrared spectral results -Surface morphologies -Local topography -Shape, physical properties
The impactor collides to the surface of the asteroid.
The sample will be obtained from the newly created crater.
Launch
The spacecraft observes the asteroid, releases the small rovers and the lander, and executes multiple samplings.
Earth Return
Sample analysis
Mission Scenario of Hayabusa2
03 Dec. 2014 June-July 2018
2019
Nov.-Dec. 2020
New Experiment
Nov.-Dec. 2019 : Departure
Arrival at Ryugu 03 Dec. 2015
Earth swing-by
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X-band MGA
X-band HGA
Ka-band HGA
Star Trackers
Reentry Capsule
Sampler Horn
Solar Array Panel
Near Infrared Spectrometer (NIRS3)
LIDAR
X-band LGA Deployable Camera (DCAM3)
ONC-W2
Hayabusa2 Spacecraft
Size :: 1m×1.6m×1.25m (body) Mass:: 600kg (Wet)
Ion Engine
Small Carry-on Impactor (SCI)
MASCOT Lander
MINERVA-II Rovers
Target Markers ×5
RCS thrusters ×12
Thermal Infrared Imager (TIR)
ONC-T, ONC-W1
ONC-T LIDAR NIRS3 TIR
Science Instruments
II-1A II-1B
by DLR and CNES
MASCOT
II-2
II-2 : by Tohoku Univ. & MINERVA-II consortium
II-1 : by JAXA MINERVA-II Team
MINERVA-II
Small Lander and Rovers
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Remote Sensing Instruments of Hayabusa2
Optical Navigation Camera (ONC) filter set was changed (ONC-T : 6.35deg2, ONC-W : 65.24deg2) Light Detection and Ranging (LIDAR) adapted to low albedo of C-type (Range : 30m – 25km) Near Infrared Spectrometer (NIRS3) absorption by H2O Wave length : 1.8 – 3.2 µm Thermal Infrared Imager (TIR) Thermal radiation Wave length : 8 – 12 µm
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Sampling Operation Sequence
19
1999JU3
Artificial Crater Generation Operation
①SCI Separation
②Horizontal Escape ③Vertical Escape
④DCAM3 Separation
⑤Detonation & Impact
⑥Return to HP
Impact Observation
Detonation & Impact
1999 JU3
explosion
separation
(a) high speed debris (b) high speed ejecta (c) low speed ejecta
(a)
(b)
(c)
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Trajectory Design for the way to Ryugu
Sun
Launch (Dec. 3, 2014)
Earth swing-by (Dec. 3, 2015)
Ryugu arrival (June-July 2018)
Ryugu orbit
Hayabusa2 trajectory
Earth orbit
21
Launch and Initial Operations 2014/12/3 04:22:04 Launch 06:09:25 Separation 06:14:53 SAP deployment 06:16:31 Sun acquisition maneuver 09:06:51 Single spin established
1st, 2nd, 3rd tracking passes Three axis attitude stabilization established Sampler horn deployed Ion engine gimbal launch lock released Moon photo taken by ONC-W2, benefit for scientific calibration purpose
PAF interface
Fully deployed SMP
Moon taken at 300,000km distance.
22
Commissioning Phase Date Event
2014 Dec. 3-6 LEOP
Dec. 7-8 XMGA pointing calibration, X-band COMM characterization/testing
Dec. 9 EPS/BAT testing
Dec. 10 NIRS3 health check
Dec. 11 TIR/DCAM3/ONC health check
Dec. 12-15 AOCS characterization/testing
Dec. 16 MINRVA-II/MASCOT health check
Dec. 17 CPSL/SCI health check
Dec. 18 XHGA pointing calibration, IES turn-on preparation
Dec. 19-22 IES baking
Dec. 23-26 IES testing (ITR-A/B/C/D, single-thruster-at-once operation)
2015 Dec. 27-Jan. 4 Precision OD, DDOR testing
Jan. 5-10 Ka-band COMM characterization/testing, KaHGA pointing calibration
Jan. 11 IES turn-on preparation
Jan. 12-15 IES testing (<A+C>,<C+D>,<A+D>,<A+C>, dual thrusters operation)
Jan. 16 IES testing (<A+C+D>, triple thrusters operation)
Jan. 19-20 IES 24hr continuous operation demonstration (<A+D>)
Jan. 23 LIDAR/LRF/FLA health check
Jan. 24-Mar. 2 IES-AOCS coordinated operation testing SRP dynamics characterization / “Solar Sail Mode” demonstration
Mar. 2 Commissioning phase completed
DSN GDS/CAN/MAD
DSN MAD
DSN MAD
DSN GDS/CAN/MAD
DSN GDS/CAN/MAD
DSN MAD
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Communication System of Hayabusa2
X-band Middle Gain Antenna (X-MGA)
X-band High Gain Antenna (X-HGA)
Ka-band High Gain Antenna (Ka-HGA)
X-band Low Gain Antenna (X-LGA-A)
X-band Low Gain Antenna (X-LGA-C)
X-band Low Gain Antenna (X-LGA-B)
X-band : Uplink : CMD, RNG (7.2GHz) Downlink : TLM, RNG (8.4GHz)
Ka-band: Downlink : TLM, RNG (32GHz)
Bit rate : 8bps〜32Kbps
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Regular Operation Phase to Earth Swing-by 2015
Mar. 3 Regular Operation Phase started
Mar. 3-21 First IES Operation in EDVEGA Phase : 409 hours Mar. 27 – May 7 Attitude control in the solar sail mode (One RW operation)
May 12-13 Three IES operation for 24hours June 2-6 Second IES Operation in EDVEGA Phase : 102 hours June 9- The solar sail mode operation Sep. 1,2 TCM by IES
- mid Sep. Precise OD
Oct.-Dec. Precise TCM by RCS
Dec. 3 Earth swingby
Dec. 2015-Apr. 2016 Post-Swingby southern hemisphere operation
25
Approach to the Earth
Earth Swing-by
Sun direction
2015/11/3 TCM1
2015/11/26 TCM2
2015/12/1 TCM3―cancel
Orbit of Moon
2015/11/10-13 TIR Obs.
2015/11/26 ONC-T, TIR, NIRS3 Obs.
2015/12/3 ONC-W2 Obs 2015/12/3
the closest point
2015/12/4 TIR and ONC-T Obs.
2015/12/22 End of Swingby Operation
Eclipse (20min)
Closest (19:08:07JST)
Sun direction
North pole
Eclipse starts (18:58JST)
Eclipse ends (19:18JST)
Orbit near the earth
(Time is in JST)
26
2015/12/19 LIDAR Experiment
The Earth images at swing-by (animation)
The images of the Earth taken by ONC-W2. The time (UTC) of each image and the distance from the Earth are shown in the photo. The images were taken from 00:00 to 09:15 (UTC) on December 3, 2015. The viewing angle is at about 60 degrees.
27
Operations of Science Instruments ONC-T TIR
NIRS3
Plants exist reasion Color image Thermal Image
Australia
LID
AR
受受信信
レレベベ
ルル (m
V)
Dec. 19, 2015 Distance 6.70 million km (= 0.045AU)
Absorption by water on the earth
1-way link from the earth to the spacecraft Earth Moon strong
weak
wav
e le
ngth
(µm
)
sign
al le
vel
data NO LI
DA
R S
igna
l Lev
el (m
V)
LIDAR
28
Optical Link Experiment by LIDAR
Mt. Stromlo station at SERC (Space Environment Research Centre Australia) in Australia transmitted laser light towards Hayabusa2. Hayabusa2 successfully received the beam using the onboard LIDAR at the distance of 6,700,000 km from Earth.
29
Dec. 19, 2015
Operations and Experiments after Earth Swing-by 2016 Jan. - April Southern hemisphere operation
March 22 – May 21 1st long-term IES operation after Earth Swing-by : 798 h
May 24 – June 9 Mars Observation (by ONC-T, NIRS3, TIR)
June 22, 23 Experiment of uplink transfer June 29 – July 8 Experiments of Ka-band communication : Dec. – May 2017 ? 2nd long-term IES operation Nov. 2017 - June 2018 ? 3rd long-term IES operation
30
Experiment of Uplink Transfer
The experiment of uplink transfer was done by using DSN stations on June 22, 23, 2016 and it was successful. This is the first experiment for Japanese spacecraft.
Station A Station B
Station A Station A Station B Station B
Conventional :
Uplink Transfer::
Uplink stops for a while
Uplink continues
Uplink continues
31
Experiments of Ka band
June 26 – July 3, 2016 : Ka-band communication test by using Goldstone Station (NASA DSN) was successful in the distance of about 50 million km.
July 1, 2, 2016 : DDOR experiment by using Ka-band was successful. (Stations : NASA-Goldstone, ESA-Malargüe)
July 5 – 8, 2016 : Ka-band compatibility test by using Malargüe Station (ESA) was successful.
DDOR: Delta Differential One-way Range
QSO
32
Target Asteroid : 1999 JU3 = Ryugu Asteroid (162173) 1999 JU3 Discovered in May 1999 by LINEAR Team
Shape : almost spherical
Size : 900 m Rotation period: 7.6 h Pole orientation (320°, -40°) :current estimate
Albedo : 0.05 Type : Cg
(by Kim, Choi, Moon et al. A&A 550, L11, 2013)
(Data by Viras 2008, Sugita+ 2012, Abe+ 2008)
Orbit
Shape Light curve Spectrum
Wave length (µm)
Rela�ve reflec�on
rate
Tp=7.625 hr assumedModel
1.2
1.3
1.4
1.5
1.6
1.7
1.8
0 0.1 0.2 0.3 0.4 0.5 0.6 0.7 0.8 0.9 1
Diff
eren
tial M
agni
tude
Rotational phaseRota�onal phase
Diffe
ren�
al M
agnitude
(by T. Müller)
33
+3 +2 +1 0 -1 -2 -3 -4 -5 -6 -7 -8 -9 log10 L [m]
Return sample analyses
On-site remote sensing
Observations on the surface
Science for Wide Scale Range
ONC (T, W1, W2) LIDAR NIRS3 TIR MASCOT
MINERVA-II (1A, 1B, 2)
Ground based facilities
SCI DCAM3 Sampler
34
Europe
USA
Australia
NASA
DLR CNES
SLASO/DIISR DoD/AOSG AQIS/AC
International Cooperation Structure of Hayabusa2
35
(101955) Bennu
OSIRIS-REx
Solar Power Sail System for Trojan Mission
The spacecraft is supposed to be launched in early 2020s and make a world’s first trip to Trojan asteroid using Earth and Jupiter gravity assist. After arriving at Trojan asteroid, the lander is separated from solar power sail-craft to collect surface and underground samples and perform in-situ analysis. The lander delivers samples to solar power sail-craft for sample return mission (optional).
Sun
Mainbelt (~ 3AU)
Earth (1AU)
Trojan asteroid (~5.2 AU)
Jupiter (~5.2 AU)
5) Departure from Trojan asteroid 6) Jupiter swing-by 7) Return to Earth
optional
<Event> 1) Launch 2) Earth swing-by 3) Jupiter swing-by 4) Arrival at Trojan asteroid
Ion engines
50m from Osamu MORI
36
Summary Hayabusa and Hayabusa2 are challenging missions not only for science but also for space technologies. Hayabusa2, which was launched on Dec. 3, 2014, are now on the way to the target asteroid Ryugu, and the operations are ongoing smoothly. Asteroids are important in various aspects, and we would like to extend our missions to other objects.
Science Spaceguared
Resource Manned mission
Engineering Culture
Asteroids are important!
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