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AKATSUKI’s Second Journey to Venus 7 October 2015 Chikako Hirose Japan Aerospace Exploration Agency

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Page 1: AKATSUKI’s Second Journey to Venus - Agidownloads.agi.com/u/images/gallery/events/IUC/...the Venus orbit, the heat input around perihelion is 1000 [W/m 2] higher than the one on

AKATSUKI’s Second Journey to Venus

7 October 2015 Chikako Hirose

Japan Aerospace Exploration Agency

Page 2: AKATSUKI’s Second Journey to Venus - Agidownloads.agi.com/u/images/gallery/events/IUC/...the Venus orbit, the heat input around perihelion is 1000 [W/m 2] higher than the one on

My STK usage history (2005-2009) • JAXA conjunction assessment system

– JAXA CA system was developed in 2007 and became operational in 2008. – During the transition period, SOCRATES was referred for cross-check. http://www.celestrak.com/SOCRATES/

• Assessment of how to spread space debris after kinetic engagement – By using Two Line Elements of Fengyun 1C, Chinese Anti-satellite Test, how to

spread space debris was assessed.

STK was very useful as an easy-to-use propagator for assessment.

2015 AGI International User's Conference

Page 3: AKATSUKI’s Second Journey to Venus - Agidownloads.agi.com/u/images/gallery/events/IUC/...the Venus orbit, the heat input around perihelion is 1000 [W/m 2] higher than the one on

My STK usage history (2010-) • Trajectory re-design of Japanese Venus explorer, Akatsuki

– Akatsuki was launched in May, 2010. – It reached to Venus in December, 2010, but failed in Venus Orbit Insertion. – During the VOI, the injection by main engine was stopped and Akatsuki was

transferred to Safe Hold Mode.

2015 AGI International User's Conference

Period: 96 hours

48 hours

30 hours

PlanResult

Maneuver

STK/Astrogator and Analysis Workbench played active roles in trajectory re-design.

Page 4: AKATSUKI’s Second Journey to Venus - Agidownloads.agi.com/u/images/gallery/events/IUC/...the Venus orbit, the heat input around perihelion is 1000 [W/m 2] higher than the one on

Akatsuki Fact Sheet

2015 AGI International User's Conference

Orbit Maneuvering Engine (OME): 500 N

Reaction Control System (RCS): 23 N x 4

RCS: 23 N x 4

Structures 1.04 [m] x 1.45 [m] x 1.40 [m]

Weight (dry) 321 kg (wet) 518 kg (launch) / 362 kg (now)

Instruments 1-micron Camera (IR1) 2-micron Camera (IR2) Ultraviolet Imager (UVI) Longwave Infrared Camera (LIR) Lightning and Airglow Camera (LAC)

Propulsion Orbit Maneuver Engine (OME): 500N Reaction Control System (RCS): 23N x 4 x 2 3N x 4

Telecoms X-band High Gain Antenna – T/R Middle Gain Antenna x 2 Low Gain Antenna x 2

Mission 2 years in Venus orbit

Page 5: AKATSUKI’s Second Journey to Venus - Agidownloads.agi.com/u/images/gallery/events/IUC/...the Venus orbit, the heat input around perihelion is 1000 [W/m 2] higher than the one on

Orbital Events in 2011

2015 AGI International User's Conference

Orbital Events

2010 May 20 Launch

Dec 7 Venus Orbit Insertion (VOI) - failed

2011 Sep

7 14

OME Test Maneuver (TM1) (TM2)

Sep 30 Disposal of Oxidizer Test (DOX Test)

Oct 6 12 13

Disposal of Oxidizer (DOX1) (DOX2) (DOX3) – total 65 kg

Nov 1 10 21

Trajectory correction maneuver (DV1) (DV2) (DV3) – total 240 m/s

2015 Winter Venus re-encounter

(c) TM1(d) TM2

(e) DOX Test (f)-(h) DOX1,2,3

(i) DV1

(j) DV2

(k) DV3

(b) VOI (2010)

(c)(d)

(e)(f)

(g), (h)

(i)(j)

(k)

(b)

(c)

(d)

(e)(f)(g), (h)

(i) (j)(k)

Post-DV1,2,3

Pre-DV1,2,3

x 108 km

J2000 Ecliptic coordinate

(a) Launch

(a)

(b)

(a)

Trajectory (Launch – VOI (2010))

Earth

Venus

Akatsuki

• Akatsuki was set to encounter Venus again in 2015 after several trajectory corrections in 2011.

Page 6: AKATSUKI’s Second Journey to Venus - Agidownloads.agi.com/u/images/gallery/events/IUC/...the Venus orbit, the heat input around perihelion is 1000 [W/m 2] higher than the one on

Tough Surroundings

2015 AGI International User's Conference

• Since Akatsuki is flying inside of the Venus orbit, the heat input around perihelion is 1000 [W/m2] higher than the one on Venus orbit (approx. 2,600 [W/m2]). Therefore +Z plane (HGA-T/R loaded), which is most tolerant against heat, is always facing toward the Sun.

• The temperature of some equipment is over the design specification. However, they work properly at present. 0

50

100

150

TEM

PERA

TURE

[℃]

HGA-T HGA-R SAP-A SAP-BRCS-THV-AT1 RCS-THV-AT2 RCS-THV-AT3 RCS-THV-AT4RCS-THV-AB1 RCS-THV-AB2 RCS-THV-AB3 RCS-THV-AB4

Solar Paddles

High Gain Antenna

Thruster Valves (AT: +Z plane)

Thruster Valves (AB: -Z plane)

Fig 1.1 Temperature History since Launch

Page 7: AKATSUKI’s Second Journey to Venus - Agidownloads.agi.com/u/images/gallery/events/IUC/...the Venus orbit, the heat input around perihelion is 1000 [W/m 2] higher than the one on

Tough Conditions

2015 AGI International User's Conference

(a) Orbital Plane: close to the Venus equator (b) Orbital Direction: Retrograde (c) Umbra: less than 90 minutes (d) Incident Angle: less than 13 degrees to Akatsuki orbital plane

Polar

Propulsion: 330 m/s (RCS) = Ha: 300,000 km

It is difficult to maintain the periapsis because of the solar gravity perturbations.

Observation and System Requirements

Page 8: AKATSUKI’s Second Journey to Venus - Agidownloads.agi.com/u/images/gallery/events/IUC/...the Venus orbit, the heat input around perihelion is 1000 [W/m 2] higher than the one on

Examples

2015 AGI International User's Conference

Page 9: AKATSUKI’s Second Journey to Venus - Agidownloads.agi.com/u/images/gallery/events/IUC/...the Venus orbit, the heat input around perihelion is 1000 [W/m 2] higher than the one on

Analysis Cases

2015 AGI International User's Conference

1st Approach 2nd Approach 3rd Approach MaintainPeriapsis Altitude

System & ObservationRequirements

(1) VOI(1-1) Retrograde X -(1-2) Posigrade X -(1-3) Polar OK NG (a,b,d)

(2a) Swingby VOI θ: 170 deg (2a-1) Retrograde X - r: 16,000 km (2a-2) Posigrade OK NG (b)

(2a-3) Polar OK NG (a,b,d)

(3a) Swingby VOI(3a-1) Retrograde X -(3a-2) Posigrade OK NG (b)(3a-3) Polar OK NG (a,b,d)

(2b) Swingby VOI θ: 0 deg (2b-1) Retrograde X - r: 150,000 km (2b-2) Posigrade OK NG (b)

(2b-3) Polar OK NG (a,b,d)

(3b) Swingby VOI(3b-1) Retrograde X -(3b-2) Posigrade OK NG (b)(3b-3) Polar OK NG (a,b,d)

Solar Gravity Perturbations!!!

Page 10: AKATSUKI’s Second Journey to Venus - Agidownloads.agi.com/u/images/gallery/events/IUC/...the Venus orbit, the heat input around perihelion is 1000 [W/m 2] higher than the one on

Solar Gravity Perturbation

2015 AGI International User's Conference

Deceleration

Deceleration

(Sun-Venus Fixed Rotating Frame)

III

III IV-8

-6

-4

-2

0

2

4

6

8

-8 -6 -4 -2 0 2 4 6 8

Venus

Acceleration

Acceleration-8

-6

-4

-2

0

2

4

6

8

-8 -6 -4 -2 0 2 4 6 8

(Sun-Venus Fixed Rotating Frame)

IV

1mSun

1d

d

Deceleration

Deceleration

III

III

Acceleration

Acceleration

2d

θ

Venus

(a) Insertion to Posigrade Orbit (b) Insertion to Retrograde Orbit

Fig. 1. Acceleration and Deceleration areas caused by the SGP

θ232

1331

1 cos31, +=

−−=

ddGm

ddGm RddR 1Solar Gravity Perturbation (SGP)

Page 11: AKATSUKI’s Second Journey to Venus - Agidownloads.agi.com/u/images/gallery/events/IUC/...the Venus orbit, the heat input around perihelion is 1000 [W/m 2] higher than the one on

Geometry of Analysis Cases

2015 AGI International User's Conference

(a) Insertion to Posigrade Orbit (b) Insertion to Retrograde Orbit

Fig. 2. Geometry of Analysis Cases

-4

-3

-2

-1

0

1

2

3

4

-4 -3 -2 -1 0 1 2 3 4

Deceleration Acceleration

1st ApproachSWB1170deg+ 2nd Approach

SWB10deg+2nd Approach

(Sun-Venus Fixed Rotating Frame) x 105 [km]

Acceleration Deceleration

NA

NA

NA

(1)

(2b)

(2a)

-4

-3

-2

-1

0

1

2

3

4

-4 -3 -2 -1 0 1 2 3 4

1st Approach

SWB1170deg+2nd Approach

SWB10deg+2nd Approach

(Sun-Venus Fixed Rotating Frame) x 105 [km]

Acceleration Deceleration

Deceleration Acceleration

NA

OK

OK

(2a)(2b)

(1)

Page 12: AKATSUKI’s Second Journey to Venus - Agidownloads.agi.com/u/images/gallery/events/IUC/...the Venus orbit, the heat input around perihelion is 1000 [W/m 2] higher than the one on

Retrograde Orbit Insertion I

2015 AGI International User's Conference

Change of approach direction

-600,000

-400,000

-200,000

0

200,000

400,000

600,000

-600,000 -400,000 -200,000 0 200,000 400,000 600,000

Approach in November

Approach in December

Deceleration Effect by the Solar Gravity

Acceleration Effect by the Solar Gravity

Acceleration Effect

Deceleration Effect

Sun Venus

(Sun-Venus Fixed Rotation Frame) Fig 3. Change of approach angle

Page 13: AKATSUKI’s Second Journey to Venus - Agidownloads.agi.com/u/images/gallery/events/IUC/...the Venus orbit, the heat input around perihelion is 1000 [W/m 2] higher than the one on

Retrograde Orbit Insertion II

2015 AGI International User's Conference

Fig. 4 GBM Trajectory in Inertial frame

(Venus centered Inertial Frame)

PosigradeRetrograde

Earth @ Nov. 22Earth @ Dec. 31

Sun @ VOI(Nov. 22)

Venus

Acceleration

Acceleration Deceleration

Deceleration

3. retrograde2. posigrade

1. 4.

5.

6.

Sun

Venus

Fig. 5 GBM Trajectory in Sun-Venus fixed rotating frame

Hill radius

Make the most of the solar gravity perturbations. (Gravity Brake)

Page 14: AKATSUKI’s Second Journey to Venus - Agidownloads.agi.com/u/images/gallery/events/IUC/...the Venus orbit, the heat input around perihelion is 1000 [W/m 2] higher than the one on

Candidate Cases of Re-VOI

2015 AGI International User's Conference

maintainingaltitude

Ha [km]x 1000

(1a) VOI (approach from inside of Venus's orbit)Retrograde NA -

Direct NA -

Polar OK 300

(1b) VOI (Hohmann Transfer Method)Retrograde OK 330Direct NA -

Polar OK -

(1c) VOI (Gravity Break Method)Direct -> Retrograde OK 300

(2a) Swingby VOIθ 170° Retrograde NA -

r 16,000km Direct OK 300Polar OK 410

(2b) Swingby VOIRetrograde NA -

Direct OK -

Polar OK 410

(3a) Swingby VOIθ 0° Retrograde NA -r 150,000km Direct OK 410

Polar OK 410

(3b) Swingby VOIRetrograde NA -

3rd approach2nd approach1st approach

Venus Circular Orbit

C

A

D

Summary VOI Ha (x1000) [km]

A. Polar November 22, 2015 300

B. Posigrade July 1, 2016 300

C. Retrograde (Hohmann Transfer) December 5-13, 2015 330

D. Retrograde (Gravity Brake) November 22, 2015 300

B

Page 15: AKATSUKI’s Second Journey to Venus - Agidownloads.agi.com/u/images/gallery/events/IUC/...the Venus orbit, the heat input around perihelion is 1000 [W/m 2] higher than the one on

Orbital Events in 2015

2015 AGI International User's Conference

Orbital Events

2015 July 17 24 31

Trajectory correction maneuver (DV4-1) (DV4-2) (DV4-3)

Aug 29 9th & Last Perihelion

Dec 7 Venus Orbit Insertion (VOI-R1)

VOI-R2

2016 Phase Control (PC1, 2, ...)

Fig 2.2.1 Altitude History (Apoapsis)

VOI-R1 VOI-R2

PC1

PC2

Page 16: AKATSUKI’s Second Journey to Venus - Agidownloads.agi.com/u/images/gallery/events/IUC/...the Venus orbit, the heat input around perihelion is 1000 [W/m 2] higher than the one on

2015 AGI International User's Conference

Page 17: AKATSUKI’s Second Journey to Venus - Agidownloads.agi.com/u/images/gallery/events/IUC/...the Venus orbit, the heat input around perihelion is 1000 [W/m 2] higher than the one on

Akatsuki Official Report Covers

2015 AGI International User's Conference

Spacecraft Specification (- 2009)

Operation Result (2010)

Operation Result & Trajectory Design

(2011-2012)