The Voyager Program is an American scientific program that launched two unmanned space missions, the probes Voyager 1 and Voyager 2.
These were launched in 1977 to take advantage of a favorable alignment
of the planets during the late 1970s. Although they were designated
officially to study just the planetary systems of Jupiter and Saturn, the space probes were able to continue their mission.
On August 25, 2012 Voyager 1 became the first human-made object to enter the previously unexplored region of space known as interstellar space, traveling "further than anyone, or anything, in history" Voyager 2
is expected to enter interstellar space within a few years of 2016, and
its plasma spectrometer should provide the first direct measurements of
the density and temperature of the Interstellar Plasma.
As of 2013, Voyager 1 was moving with a relative velocity to the Sun of 17 kilometres per second (11 mi/s).The amount of power available to the probe has decreased over time, and
will be no longer able to power any single instrument by 2025.
Both of the Voyager missions into outer space have gathered large amounts of data about the gas giants of the solar system, and their orbiting satellites, about which little had been previously known. In addition, the trajectories of the two spacecraft have been used to place limits on the existence of any hypothetical trans-Neptunian planets.
Data and photographs collected by the Voyagers’ cameras, magnetometers, and other instruments revealed previously unknown details about each of the giant planets and their moons. Close-up images from the spacecraft charted Jupiter’s
complex cloud forms, winds, and storm systems and discovered volcanic
activity on its moon Io. Saturn’s rings were found to have enigmatic
braids, kinks, and spokes and to be accompanied by myriad of “ringlets.”
At Uranus Voyager 2 discovered a substantial magnetic field around the planet and 10 additional moons. Its flyby of Neptune uncovered three complete rings and six hitherto unknown moons as well as a planetary magnetic field and complex, widely distributed auroras.
These two space probes were built at the Jet Propulsion Laboratory in Southern California, and they were paid for by the National Aeronautics and Space Administration (NASA), which also paid for their launchings from Cape Canaveral, Florida, their tracking, and everything else concerning the space probes.
Trajectories and expected location of Pioneer and Voyager spacecraft in April 2007
Spacecraft Design
The Voyager spacecraft weighs 773 kilograms. Of this, 105 kilograms are scientific instruments.The identical Voyager spacecraft use three-axis-stabilized guidance systems that use gyroscopic and accelerometer inputs to their attitude control computers to point their high-gain antennas towards the Earth
and their scientific instruments pointed towards their targets,
sometimes with the help of a movable instrument platform for the smaller
instruments and the electronic photography system.
The diagram at the right shows the high-gain antenna (HGA) with a 3.66 meter diameter dish attached to the hollow decagonal electronics container. There is also a spherical tank that contains the hydrazine monopropellant fuel.
The Voyager Golden Record
is attached to one of the bus sides. The angled square panel to the
right is the optical calibration target and excess heat radiator. The
three radioisotope thermoelectric generators (RTGs) are mounted end-to-end on the lower boom.
The scan platform comprises: the Infrared Interferometer Spectrometer
(IRIS) (largest camera at top right); the Ultraviolet Spectrometer
(UVS) just above the UVS; the two Imaging Science Subsystem (ISS) vidicon cameras to the left of the UVS; and the Photopolarimeter System (PPS) under the ISS.
Only five investigation teams are still supported, though data is collected for two additional instruments.The Flight Data Subsystem (FDS) and a single eight-track digital tape recorder (DTR) provide the data handling functions.
The FDS configures each instrument and controls instrument
operations. It also collects engineering and science data and formats
the data for transmission. The DTR is used to record high-rate Plasma Wave Subsystem (PWS) data. The data is played back every six months.
The Imaging Science Subsystem, made up of a wide angle and a narrow angle camera, is a modified version of the slow scan vidicon
camera designs that were used in the earlier Mariner flights. The
Imaging Science Subsystem consists of two television-type cameras, each
with eight filters in a commandable Filter Wheel mounted in front of the
vidicons. One has a low resolution 200 millimeter wide-angle lens with an aperture
of f/3 (the wide angle camera), while the other uses a higher
resolution 1.500 meter narrow-angle f/8.5 lens.
Computers
Unlike the other onboard instruments, the operation of the cameras for visible light is not autonomous, but rather it is controlled by an imaging parameter table contained in one of the on-board digital computers, the Flight Data Subsystem (FDS). More recent space probes, since about 1990, usually have completely autonomous cameras.
The computer command subsystem (CCS) controls the cameras. The CCS contains fixed computer programs
such as command decoding, fault detection, and correction routines,
antenna pointing routines, and spacecraft sequencing routines. This
computer is an improved version of the one that was used in the Viking orbiter.The hardware in both custom-built CCS subsystems in the Voyagers is identical. There is only a minor software modification for one of them that has a scientific subsystem that the other lacks.
The Attitude and Articulation Control Subsystem (AACS) controls the spacecraft orientation (its attitude). It keeps the high-gain antenna pointing towards the Earth, controls attitude changes, and points the scan platform. The custom-built AACS systems on both craft are identical.
It has been erroneously reported on the Internet that the Voyager space probes were controlled by a version of the RCA 1802 , but such claims are not supported by the primary design documents. The CDP1802 microprocessor was used later in the Galileo space probe, which was designed and built years later. The digital control electronics of the Voyagers were based on RCA CD4000 radiation-hardened, silicon-on-sapphire (SOS) custom-made integrated circuit chips, combined with standard transistor-transistor logic (TTL) integrated circuits.
Communications
The uplink communications are executed via S-band microwave communications. The downlink communications are carried out by an X-band microwave
transmitter on board the spacecraft, with an S-band transmitter as a
back-up. All long-range communications to and from the two Voyagers have been carried out using their 3.67-meter high-gain antennas.
Because of the inverse-square law in radio communications, the digital data rates used in the downlinks from the Voyagers
have been continually decreasing the farther that they get from the
Earth. For example, the data rate used from Jupiter was about 115,000
bits per second. That was halved at the distance of Saturn, and it has
gone down continually since then. Some measures were taken on the ground
along the way to reduce the effects of the inverse-square law. In
between 1982 and 1985, the diameters of the three main parabolic dish antennas of the Deep Space Network was increased from 240 feet to 270 feet, dramatically increasing their areas for gathering weak microwave signals.
Then between 1986 and 1989, new techniques were brought into play to
combine the signals from multiple antennas on the ground into one, more
powerful signal, in a kind of an antenna array. This was done at Goldstone, California, Canberra, and Madrid using the additional dish antennas available there. Also, in Australia, the Parkes Radio Telescope was brought into the array in time for the fly-by of Neptune in 1989. In the United States, the Very Large Array in New Mexico
was brought into temporary use along with the antennas of the Deep
Space Network at Goldstone. Using this new technology of antenna arrays
helped to compensate for the immense radio distance from Neptune to the
Earth.
Power
Radioisotope thermoelectric generators for the Voyager program.
Electrical power is supplied by three MHW-RTG radioisotope thermoelectric generators (RTGs). They are powered by Plutonium-238 and provided approximately 470 W at 30 volts DC when the spacecraft was launched. Plutonium-238 decays with a half-life of 87.74 years,so RTGs using Pu-238 will lose a factor of 1−0.5{1/87.74} = 0.79% of their power output per year.
In 2011, 34 years after launch, such an RTG would inherently produce 470 W × 2−(34/87.74) ≈ 359 W, about 76% of its initial power. Additionally, the thermocouples that convert heat into electricity also degrade, reducing available power below this calculated level.
By 7 October 2011 the power generated by Voyager 1 and Voyager 2
had dropped to 267.9 W and 269.2 W respectively, about 57% of the power
at launch. The level of power output was better than pre-launch
predictions based on a conservative thermocouple degradation model. As
the electrical power decreases, spacecraft loads must be turned off,
eliminating some capabilities.
It is notable that the electrical utility of the two Voyager
craft would seem to average out ((470 W+268.5 W)÷2) at about 369 W or
about (369 W ÷ 773 kg) 0.4773 W/kg over a period of about 34 years for a
work record of about (0.4773 × 34 X 31,556,925.22) 512 megajoules per
kilogram. By comparison gasoline contains about 42 MJ per kg and compared to a typical gasoline engine's efficiency of 14%
Voyager has produced 87 times as much
energy per kilogram. If a spacecraft with such an efficient radioisotope
powerplant were also equipped with a high efficiency ion motor and a
convenient mass ratio of e (ca 2.71828) then it could calculably escape
from the solar system by electric propulsion from low earth orbit though
it would still not match the high velocities of the Voyagers.
Voyager Golden Record
Voyager 1 and Voyager 2 both carry with them a Golden Record that
contains pictures and sounds of Earth, along with symbolic directions
for playing the record and data detailing the location of Earth.The record is intended as a combination time capsule and interstellar message to any civilization, alien or far-future human, that may recover either of the Voyager craft. The contents of this record were selected by a committee that included Timothy Ferris and was chaired by Carl Sagan.
