Giotto (spacecraft)

 

Originally a United States partner probe was planned that would accompany Giotto, but this fell through due to budget cuts at NASA. There were plans to have observation equipment on board a Space Shuttle in low-Earth orbit around the time of Giotto's fly-by, but they in turn fell through with the Challenger disaster.

The plan then became a cooperative armada of five space probes including Giotto, two from the Soviet Union's Vega program and two from Japan: the Sakigake and Suisei probes. The idea was for Japanese probes and the pre-existing American probe International Cometary Explorer to make long distance measurements, followed by the Soviet Vegas which would locate the nucleus, and the resulting information sent back would allow Giotto to precisely target very close to the nucleus. Because Giotto would pass so very close to the nucleus ESA was mostly convinced it would not survive the encounter due to the spacecraft colliding at very high speed with the many dust particles from the comet. The coordinated group of probes became known as the Halley Armada.

 

The cylindrical spacecraft was 1.85 m in diameter and had three internal platforms. It was derived from the GEOS research satellite built by British Aerospace in Filton, Bristol, and modified with the addition of a dust shield (Whipple shield) as proposed by Fred Whipple. The shield comprised a thin (1 mm) aluminium sheet separated by a space and a thicker (12 mm) Kevlar sheet.^[3] The later Stardust spacecraft would use a similar Whipple shield. Giotto also had a 1.51 m diameter antenna that it used to communicate with Earth.^[3] A mock-up of the spacecraft resides at the Bristol Aero Collection hangar, at Filton, Bristol, England.^{[citation needed]}

Giotto had 10 science instruments.^[4][5]

• MAG: a magnetometer
• HMC (Halley Multicolour Camera): a 16-cm telescope and camera
• DID (Dust Impactor Detector System): measured the mass of dust particles that hit the instrument
• RPA (Rème Plasma Analyser): studied solar wind and charged particles
• JPA (Johnstone Plasma Analyser): also measured solar wind and charged particles
• PIA (Particulate Impact Analyser): studied the size and chemistry of particles
• OPE (Optical Probe Experiment): examined the emissivity of gas and dust behind the spacecraft
• EPA (Energetic Particle Analyser): analyzed alpha-particles, electrons, and neutrons
• NMS (Neutral Mass Spectrometer): measured the composition of the particles around the comet
• IMS (Ion Mass Spectrometer): measured the amount of ions from the sun and the comet
• GRE (Giotto Radio Experiment): used Giotto's radio signals to study Halley's comet

The mission was given the go-ahead by ESA in 1980, and launched on an Ariane 1 rocket (flight V14) on 2 July 1985 from Kourou, French Guiana. The craft was controlled from the European Space Agency ESOC facilities in Darmstadt (then West Germany) initially in Geostationary Transfer Orbit (GTO) then in the Near Earth Phase (NEP) before the longer Cruise Phase through to the encounter. While in GTO a number of slew and spin-up manoeuvres (to 90 RPM) were carried out in preparation for the firing of the Apogee Boost Motor (ABM), although unlike orbit circularisations for geostationary orbit, the ABM for Giotto was fired at perigee. Attitude determination and control used sun pulse and IR Earth sensor data in the telemetry to determine the spacecraft orientation.

The Soviet Vega 1 started returning images of Halley on 4 March 1986, and the first ever of its nucleus, and made its flyby on 6 March, followed by Vega 2 making its flyby on 9 March. Vega 1's closest approach to Halley was 8 889 km.

Giotto passed Halley successfully on 14 March 1986 at 596 km distance, and surprisingly survived despite being hit by some small particles. One impact sent it spinning off its stabilized spin axis so that its antenna no longer always pointed at the Earth, and its dust shield no longer protected its instruments. After 32 minutes Giotto re-stabilized itself and continued gathering science data.

Another impact destroyed the Halley Multicolor Camera, but not before it took photographs of the nucleus at closest approach.

 

Giotto's trajectory was adjusted for an Earth flyby and its science instruments were turned off on 15 March 1986 at 02:00 UTC.

Giotto was commanded to wake up on 2 July 1990 when it flew by Earth in order to sling shot to its next cometary encounter.

The probe then flew by the Comet Grigg–Skjellerup on 10 July 1992 which it approached to a distance of about 200 km. Afterwards, Giotto was again switched off on 23 July 1992.

In 1999 Giotto made another Earth flyby but was not reactivated.

Images showed Halley's nucleus to be a dark peanut-shaped body, 15 km long, 7 km to 10 km wide. Only 10% of the surface was active, with at least three outgassing jets seen on the sunlit side. Analysis showed the comet formed 4.5 billion years ago from volatiles (mainly ice) that had condensed onto interstellar dust particles. It had remained practically unaltered since its formation.

Measured volume of material ejected by Halley:

• 80% water,
• 10% carbon monoxide
• 2.5% a mix of methane and ammonia.
• other hydrocarbons, iron, and sodium were detected in trace amounts.

Giotto found Halley's nucleus was dark, which suggested a thick covering of dust.^[6]

The nucleus's surface was rough and of a porous quality, with the density of the whole nucleus as low as 0.3 g/cm³.^[6] Sagdeev's team estimated a density of 0.6 g/cm³,^[7] but S. J. Peale warned that all estimates had error bars too large to be informative.^[8]

The quantity of material ejected was found to be three tonnes per second^[9] for seven jets, and these caused the comet to wobble over long time periods.^[6]

The dust ejected was mostly only the size of cigarette smoke particles, with masses ranging from 10 ag to 0.4 g. (See Orders of magnitude (mass).) The mass of the particle that impacted Giotto and sent it spinning was not measured, but from its effects—it also probably broke off a piece of Giotto^[9]—the mass has been estimated to lie between 0.1 g and 1 g.^[6]

Two kinds of dust were seen: one with carbon, hydrogen, nitrogen and oxygen; the other with calcium, iron, magnesium, silicon and sodium.^[6]

The ratio of abundances of the comet's light elements excluding nitrogen (i.e. hydrogen, carbon, oxygen) were the same as the Sun's. The implication is that the constituents of Halley are among the most primitive in the Solar System.

The plasma and ion mass spectrometer instruments showed Halley has a carbon-rich surface.

• Giotto made the closest approach to Halley's Comet and provided the best data for this comet.^[10]
• Giotto was the first spacecraft:

• to provide detailed pictures of a cometary nucleus.^[11]
• to make a close flyby of two comets. Young and active comet Halley could be compared to old comet Grigg–Skjellerup.
• to return from interplanetary space and perform an Earth swing-by.
• to be re-activated from hibernation mode.
• to use Earth for a gravity assist.^[1]

• Timeline of Solar System exploration
• Rosetta (spacecraft)
• Philae (spacecraft)

 

Wikimedia Commons has media related to Giotto (spacecraft).

• Mission website
• Interview with the mission's Deputy Project Scientist by NASA's Solar System Exploration
• Nature 1986 about Giotto mission
• Giotto di Bondone's Adoration of the Magi painting that includes his rendition of Halley's Comet
• Image of Halley in 1986 by Giotto spacecraft
• Giotto Mission Archive at the NASA Planetary Data System, Small Bodies Node
• Giotto Extended Mission Archive at the NASA Planetary Data System, Small Bodies Node