![]() Artist's impression of Pioneer 12 in orbit above Venus | |
Names | Pioneer Venus 1 Pioneer 12 |
---|---|
Mission type | Venus orbiter |
Operator | NASA / Ames |
COSPAR ID | 1978-051A |
SATCAT no. | 10911 |
Website | science.nasa.gov |
Mission duration | Total: 14 years, 4 months and 18 days Science phase: 13 years, 10 months and 4 days |
Spacecraft properties | |
Bus | HS-507 |
Manufacturer | Hughes |
Launch mass | 582 kg (1,283 lb) [1] |
Dry mass | 517 kg (1,140 lb) |
Dimensions | 2.5 × 2.5 × 1.2 m (8.2 × 8.2 × 3.9 ft) |
Power | 312 watts |
Start of mission | |
Launch date | May 20, 1978, 13:13:00 UTC [1] |
Rocket | Atlas SLV-3D Centaur-D1AR (AC-50) |
Launch site | Cape Canaveral LC-36A |
End of mission | |
Disposal | Decommissioned |
Last contact | October 8, 1992, 19:22 UTC |
Decay date | October 22, 1992 [2] |
Orbital parameters | |
Reference system | Cytherocentric |
Semi-major axis | 33,405.8 km (20,757.4 mi) |
Eccentricity | 0.842 |
Pericytherion altitude | 181.6 km (112.8 mi) |
Apocytherion altitude | 66,630 km (41,400 mi) |
Inclination | 105 degrees |
Period | 24 hours |
Epoch | 22 November 1979, 11:53:20 UTC [3] |
Venus orbiter | |
Orbital insertion | December 4, 1978 |
The Pioneer Venus Orbiter, also known as Pioneer Venus 1 or Pioneer 12, was a mission to Venus conducted by NASA as part of the Pioneer Venus project. Launched in May 1978 atop an Atlas-Centaur rocket, the spacecraft was inserted into an elliptical orbit around Venus on December 4, 1978. It returned data from Venus until October 1992. [2] [4]
The spacecraft conducted radar altimetry observations allowing the first global topographic map of the Venusian surface to be constructed.
Manufactured by Hughes Aircraft Company, the Pioneer Venus Orbiter was based on the HS-507 bus. [5] The spacecraft was a flat cylinder, 2.5 meters (8.2 ft) in diameter and 1.2 meters (3.9 ft) long. All instruments and spacecraft subsystems were mounted on the forward end of the cylinder, except the magnetometer, which was at the end of a 4.7 meters (15 ft) boom. A solar array extended around the circumference of the cylinder. A 1.09 metres (3 ft 7 in) despun dish antenna provided S and X band communication with Earth. A Star 24 solid rocket motor was integrated into the spacecraft to provide the thrust to enter orbit around Venus. [5]
The Pioneer Venus Orbiter carried 17 experiments with a total mass of 45 kilograms (99 lb): [6]
The Orbiter Cloud Photopolarimeter was used to measure the vertical distribution of clouds on Venus. It was a photo-polarimeter built by the Goddard Institute for Space Studies (GISS), similar to Pioneer 10 and Pioneer 11 imaging photopolarimeter (IPP). The principal investigator was J. Hansen, later succeeded by L. Travis. The instrument had a mass of 5 kilograms and consumed 5.4 watts of power.
The Orbiter Radar Mapper Instrument was designed to determine the topography and surface characteristics of Venus. It was a radar system developed by the Massachusetts Institute of Technology (MIT), with G. Pettengill serving as the principal investigator. Weighing 9 kilograms and consuming 18 watts, the instrument operated when the spacecraft was within 4,700 kilometres (2,900 mi) of the planet. It transmitted a 20-watt S-band signal at 1.757 Gigahertz and achieved a surface mapping resolution of 23 by 7 kilometres (14.3 mi × 4.3 mi) at periapsis.
The Orbiter Infrared Radiometer was used to measure infrared emissions from Venus's atmosphere. It was constructed by the Jet Propulsion Laboratory (JPL), and the principal investigator was F. Taylor. The instrument had a mass of 5.9 kilograms and required 5.2 watts of power.
The Orbiter Ultraviolet Spectrometer measured scattered and emitted ultraviolet light from Venus. Built by the Laboratory for Atmospheric and Space Physics (LASP), its principal investigator was A.I.F. Stewart. The spectrometer weighed 3.1 kilograms and consumed 1.7 watts of power.
The Orbiter Neutral Mass Spectrometer was used to determine the composition of Venus's upper atmosphere. Manufactured by the Goddard Space Flight Center (GSFC), it was managed by principal investigator H. Neimann. The instrument had a mass of 3.8 kilograms and consumed 12 watts.
The Orbiter Plasma Analyzer measured properties of the solar wind. Developed at the Ames Research Center (ARC), the instrument was led by principal investigator J. Wolfe, who was later succeeded by A. Barnes. It had a mass of 3.9 kilograms and required 5 watts of power.
The Orbiter Magnetometer was designed to characterize Venus’s magnetic field. It was built by the University of California, Los Angeles (UCLA), with C. Russell as the principal investigator. The 2-kilogram instrument consumed 2.2 watts of power and was mounted on a 4.7-meter boom to reduce spacecraft interference.
The Orbiter Electric Field Detector studied electric fields in the Venusian environment. Built by TRW and led by principal investigator F. Scarf, it had a mass of 0.8 kilograms and used only 0.7 watts of power.
The Orbiter Electron Temperature Probe investigated the thermal properties of Venus’s ionosphere. It was developed by the Goddard Space Flight Center (GSFC) under the direction of principal investigator L. Brace. The probe had a mass of 2.2 kilograms and consumed 4.8 watts.
The Orbiter Ion Mass Spectrometer was used to characterize the ion population in the ionosphere of Venus. Built by the Goddard Space Flight Center (GSFC), it was managed by principal investigator H. Taylor. The instrument had a mass of 3 kilograms and required 1.5 watts of power.
The Orbiter Retarding Potential Analyzer studied ionospheric particles. It was developed at the Lockheed Palo Alto Research Laboratory (LPARL), with W. Knudsen as the principal investigator. This instrument weighed 2.8 kilograms and consumed 2.4 watts of power.
The Orbiter Gamma-Ray Burst Detector recorded gamma-ray burst events. It was constructed by the Los Alamos Scientific Laboratory (LASL), and W. Evans served as the principal investigator. The instrument had a mass of 2.8 kilograms.
The orbiter also performed in situ radio science experiments: [6]
The OGPE utilized dual-frequency radio signals to investigate how Venus's atmosphere affects radio wave propagation. By analyzing signal attenuation and phase shifts, the experiment aimed to deduce atmospheric properties such as electron density and refractive index. This information is crucial for understanding the structure and composition of Venus's ionosphere. [7] [8] T. Croft from SRI was the principal investigator.
The OAD measured the deceleration of the spacecraft due to atmospheric drag at the fringes of Venus's atmosphere. By tracking changes in the spacecraft's velocity, the experiment provided data on atmospheric density and its variations with altitude and solar activity. G. Keating from LRC was the principal investigator.
DLBI, also known as delta-VLBI, involved simultaneous observations of the spacecraft's radio signals by widely separated Earth-based antennas. By measuring the time difference in signal arrival, the experiment achieved precise spacecraft positioning, enhancing orbit determination and navigation accuracy.
OTUR focused on detecting and analyzing turbulence in Venus's upper atmosphere and the solar wind. By examining fluctuations in radio signal properties, the experiment aimed to understand the dynamic interactions between the solar wind and Venus's ionosphere. T. Croft from SRI was the principal investigator.
The ORO experiment employed radio occultation techniques, where the spacecraft's radio signals passed through Venus's atmosphere to Earth. By analyzing changes in signal frequency and amplitude, the experiment derived vertical profiles of atmospheric temperature, pressure, and electron density. A. Kliore from JPL was the principal investigator.
OIDD aimed to map Venus's gravitational field by tracking the spacecraft's orbit perturbations. Variations in gravity indicated differences in mass distribution within the planet, providing insights into its internal structure and composition. [9] R. Phillips from JPL was the principal investigator.
The OCM focused on precise measurements of the spacecraft's trajectory to study Venus's gravitational field and test aspects of celestial mechanics. Data from this experiment contributed to refining models of planetary motion and gravitational interactions. I. Shapiro from MIT was the principal investigator
Name | Complete | Studied | Instrument Type | Manufacturer | Responsible scientist | Mass | Electrical consumption |
---|---|---|---|---|---|---|---|
OCPP | Orbiter Cloud Photopolarimeter | Clouds | Photo polarimeter | GISS | J. Hansen (later L. Travis) | 5 kg (11 lb) | 5.4 W |
ORAD | Orbiter Radar Mapper Instrument | Surface and interior | Radar | MIT | G. Pettengill | 9 kg (20 lb) | 18 W |
OIR | Orbiter Infrared Radiometer | Thermal balance | Infrared radiometer | JPL | F. Taylor | 5.9 kg (13 lb) | 5.2 W |
OUVS | Orbiter Ultraviolet Spectrometer | Composition and structure of the atmosphere | Ultraviolet spectrometer | LASP | A.I.F. Stewart | 3.1 kg (6.8 lb) | 1.7 W |
ONMS | Orbiter Neutral Mass Spectrometer | Composition and structure of the atmosphere | Neutral mass spectrometer | GSFC | H. Neimann | 3.8 kg (8.4 lb) | 12 W |
OPA | Orbiter Plasma Analyzer | Solar wind and ionosphere | Analzer plasma | ARC | J. Wolfe (later A. Barnes) | 3.9 kg (8.6 lb) | 5 W |
OMAG | Orbiter Magnetometer | Solar wind and ionosphere | Magnetometer | UCLA | C. Russell | 2 kg (4.4 lb) | 2.2 W |
OEFD | Orbiter Electric Field Detector | Solar wind and ionosphere | Measure the electric fields of Venus | TRW | Frederick L. Scarf | 0.8 kg (1.8 lb) | 0.7 W |
OETP | Orbiter Electron Temperature Probe | Solar wind and ionosphere | Electron temperature gauge | GSFC | L. Brace | 2.2 kg (4.9 lb) | 4.8 W |
OIMS | Orbiter Ion Mass Spectrometer | Solar wind and ionosphere | Ion mass spectrometer | GSFC | H. Taylor | 3 kg (6.6 lb) | 1.5 W |
ORPA | Orbiter Retarding Potential Analyzer | Solar wind and ionosphere | Ion charge meter | LPARL | W. Knudsen | 2.8 kg (6.2 lb) | 2.4 W |
OGBD | Orbiter Gamma-Ray Burst Detector | High-energy astronomy | Gamma-ray burst detector | LASL | W. Evans | 2.8 kg (6.2 lb) | 1.3 W |
ORO | Orbiter Dual-Frequency Occultation | Solar wind and ionosphere | Radio science experiments | - | A. Kliore (JPL) | – | - |
OGPE | Orbiter Dual-Frequency Experiments | Composition and structure of the atmosphere | - | T. Croft (SRI) | |||
OTUR | Atmospheric and Solar Wind Turbulence Experiment | Dynamics | - | T. Croft (JPL) | |||
OAD | Orbiter Atmospheric Drag Experiment | Composition and structure of the atmosphere | - | G. Keating (LRC) | |||
OIDD | Orbiter Internal Density Distribution Experiment | Surface and interior | - | R. Phillips (JPL) | |||
OCM | Orbiter Celestial Mechanics Experiment | Surface and interior | - | I. Shapiro (MIT) |
Note: LASP: Laboratory for Atmospheric and Space Physics (University of Boulder, Colorado); UCLA: University of California in Los Angeles; JPL: Jet Propulsion Laboratory; MIT: Massachusetts Institute of Technology; GSFC: Goddard Space Flight Center GISS: Goddard Institute for Space Studies; LRC: Langley Research Center; ARC: Ames Research Center; LASL: Los Alamos National Laboratory; SRI: Stanford Research Institute
The Pioneer Venus Orbiter was launched by an Atlas SLV-3D Centaur-D1AR rocket, which flew from Launch Complex 36A at the Cape Canaveral Air Force Station. The launch occurred at 13:13:00 (8:13 a.m. local time) on May 20, 1978, and deployed the Orbiter into heliocentric orbit for its coast to Venus. Venus orbit insertion occurred on December 4, 1978.
From Venus orbit insertion to July 1980, periapsis was held between 142 and 253 kilometres (88 and 157 mi) (at 17 degrees north latitude) to facilitate radar and ionospheric measurements. The spacecraft was in a 24-hour orbit with an apoapsis of 66,900 kilometers (41,600 mi). Thereafter, the periapsis was allowed to rise to a maximum of 2,290 kilometres (1,420 mi) and then fall, to conserve fuel.
In 1991, the Radar Mapper was reactivated to investigate previously inaccessible southern portions of the planet, in conjunction with the recently arrived Magellan spacecraft. In May 1992, the probe began the final phase of its mission, in which the periapsis was held between 150 and 250 kilometres (93 and 155 mi), until the spacecraft's propellant was exhausted, after which the orbit decayed naturally. The spacecraft continued to return data until 8 October 1992, with the last signals being received at 19:22 UTC. [4] The Pioneer Venus Orbiter disintegrated upon entering the atmosphere of Venus on October 22, 1992. [2]
From its orbit of Venus, the Pioneer Venus Orbiter was able to observe Halley's Comet when it was unobservable from Earth due to its proximity to the sun during February 1986. UV spectrometer observations monitored the loss of water from the comet's nucleus at perihelion on February 9. [11]
The extended mission allowed the spacecraft controllers to make several comet observations that were never part of the original mission objectives. The tilt of the spacecraft was altered during these comet observations so that the Ultraviolet Spectrometer (OUVS) could view the comets rather than Venus. Comets Encke (April 13–16, 1984), Giacobini-Zinner (September 8–15, 1985), Halley (December 27, 1985 - March 9, 1986), Wilson (March 13 - May 2, 1987), NTT (April 8, 1987), and McNaught (November 19–24, 1987) were all observed in this way. [10]