Viking program

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Viking
JPL
ApplicationsMars orbiter/lander
Specifications
Launch mass3,527 kilograms (7,776 lb)
PowerOrbiters: 620 watts (
solar array)
Lander: 70 watts (two RTG units)
RegimeAreocentric
Design lifeOrbiters: 4 years at Mars
Landers: 4–6 years at Mars
Production
StatusRetired
Built2
Launched2
RetiredViking 1 orbiter
August 17, 1980[1]
Viking 1 lander
July 20, 1976[1] (landing) to November 13, 1982[1]

Viking 2 orbiter
July 25, 1978[1]
Viking 2 lander
September 3, 1976[1] (landing) to April 11, 1980[1]
Maiden launchViking 1
August 20, 1975[1][2]
Last launchViking 2
September 9, 1975[1][3]

The Viking program consisted of a pair of identical American

orbiter designed to photograph the surface of Mars from orbit, and a lander
designed to study the planet from the surface. The orbiters also served as communication relays for the landers once they touched down.

The Viking program grew from NASA's earlier, even more ambitious, Voyager Mars program, which was not related to the successful Voyager deep space probes of the late 1970s. Viking 1 was launched on August 20, 1975, and the second craft, Viking 2, was launched on September 9, 1975, both riding atop Titan IIIE rockets with Centaur upper stages. Viking 1 entered Mars orbit on June 19, 1976, with Viking 2 following on August 7.

After orbiting Mars for more than a month and returning images used for landing site selection, the orbiters and landers detached; the landers then entered the Martian

instruments
on the surface.

The project cost was roughly US$1 billion at the time of launch,[5][6] equivalent to about $6 billion in 2023 dollars.[7] The mission was considered successful and is credited with helping to form most of the body of knowledge about Mars through the late 1990s and early 2000s.[8][9]

Science objectives

  • Obtain high-resolution images of the Martian surface
  • Characterize the structure and composition of the atmosphere and surface
  • Search for evidence of
    life on Mars

Viking orbiters

The primary objectives of the two Viking orbiters were to transport the landers to Mars, perform reconnaissance to locate and certify landing sites, act as communications relays for the landers, and to perform their own scientific investigations. Each orbiter, based on the earlier

axis
of the orbiter, the distance from tip to tip of two oppositely extended solar panels was 9.75 m (32 ft).

Propulsion

The main

change in velocity of 1,480 m/s (3,300 mph). Attitude control
was achieved by 12 small compressed-nitrogen jets.

Navigation and communication

An acquisition

accelerometers
were also on board.

Communications were accomplished through a 20 W

MHz relay radio was also available.[citation needed
]

Power

The power to the two orbiter craft was provided by eight 1.57 m × 1.23 m (62 in × 48 in)

batteries
.

The combined area of the four panels was 15 square meters (160 square feet), and they provided both regulated and unregulated direct current power; unregulated power was provided to the radio transmitter and the lander.

Two 30-amp·hour, nickel-cadmium, rechargeable batteries provided power when the spacecraft was not facing the Sun, during launch, while performing correction maneuvers and also during Mars occultation.[10]

Main findings

Mars image mosaic from the Viking 1 orbiter

By discovering many geological forms that are typically formed from large amounts of water, the images from the orbiters caused a revolution in our ideas about water on Mars. Huge river valleys were found in many areas. They showed that floods of water broke through dams, carved deep valleys, eroded grooves into bedrock, and travelled thousands of kilometers. Large areas in the southern hemisphere contained branched stream networks, suggesting that rain once fell. The flanks of some volcanoes are believed to have been exposed to rainfall because they resemble those caused on Hawaiian volcanoes. Many craters look as if the impactor fell into mud. When they were formed, ice in the soil may have melted, turned the ground into mud, then flowed across the surface. Normally, material from an impact goes up, then down. It does not flow across the surface, going around obstacles, as it does on some Martian craters.[11][12][13] Regions, called "Chaotic Terrain," seemed to have quickly lost great volumes of water, causing large channels to be formed. The amount of water involved was estimated to ten thousand times the flow of the Mississippi River.[14] Underground volcanism may have melted frozen ice; the water then flowed away and the ground collapsed to leave chaotic terrain.

Viking landers

Proof test article of the Viking lander
Astronomer Carl Sagan stands next to a model of a Viking lander to provide scale

Each lander comprised a six-sided aluminium base with alternate 1.09 and 0.56 m (43 and 22 in) long sides, supported on three extended legs attached to the shorter sides. The leg footpads formed the vertices of an equilateral triangle with 2.21 m (7.3 ft) sides when viewed from above, with the long sides of the base forming a straight line with the two adjoining footpads. Instrumentation was attached inside and on top of the base, elevated above the surface by the extended legs.[15]

Each lander was enclosed in an aeroshell heat shield designed to slow the lander down during the entry phase. To prevent contamination of Mars by Earth organisms, each lander, upon assembly and enclosure within the aeroshell, was enclosed in a pressurized "bioshield" and then sterilized at a temperature of 111 °C (232 °F) for 40 hours. For thermal reasons, the cap of the bioshield was jettisoned after the Centaur upper stage powered the Viking orbiter/lander combination out of Earth orbit.[16]

Astronomer Carl Sagan helped to choose landing sites for both Viking probes.[17]

Entry, Descent and Landing (EDL)

Each lander arrived at Mars attached to the orbiter. The assembly orbited Mars many times before the lander was released and separated from the orbiter for descent to the surface. Descent comprised four distinct phases, starting with a

soft landing on the surface of Mars.[18]

First "clear" image ever transmitted from the surface of Mars – shows rocks near the Viking 1 lander (July 20, 1976).

At landing (after using rocket propellant) the landers had a mass of about 600 kg.

Propulsion

Propulsion for deorbit was provided by the

change in velocity of 180 m/s (590 ft/s). These nozzles also acted as the control thrusters for translation and rotation
of the lander.

Terminal

microbes. The lander carried 85 kg (187 lb) of propellant at launch, contained in two spherical titanium tanks mounted on opposite sides of the lander beneath the RTG windscreens, giving a total launch mass of 657 kg (1,448 lb). Control was achieved through the use of an inertial reference unit, four gyros, a radar altimeter, a terminal descent and landing radar
, and the control thrusters.

Power

Power was provided by two

Ah (28,800 coulombs), 28 volt rechargeable batteries
were also on board to handle peak power loads.

Payload

Image from Mars taken by the Viking 2 lander

Communications

Communications were accomplished through a 20-watt S-band transmitter using two

word
memory for command instructions.

Instruments

The lander carried instruments to achieve the primary scientific objectives of the lander mission: to study the

payload
had a total mass of approximately 91 kg (201 lb).

Biological experiments

The Viking landers conducted

life in the Martian soil (if it existed) with experiments designed by three separate teams, under the direction of chief scientist Gerald Soffen of NASA. One experiment turned positive for the detection of metabolism (current life), but based on the results of the other two experiments that failed to reveal any organic molecules in the soil, most scientists became convinced that the positive results were likely caused by non-biological chemical reactions from highly oxidizing soil conditions.[20]

Dust dunes and a large boulder taken by the Viking 1 lander.
Trenches dug by the soil sampler of the Viking 1 lander.

Although there was a pronouncement by NASA during the mission saying that the Viking lander results did not demonstrate conclusive

Phoenix lander in the form of perchlorate salts.[21][22] It has been proposed that organic compounds could have been present in the soil analyzed by both Viking 1 and Viking 2, but remained unnoticed due to the presence of perchlorate, as detected by Phoenix in 2008.[23] Researchers found that perchlorate will destroy organics when heated and will produce chloromethane and dichloromethane, the identical chlorine compounds discovered by both Viking landers when they performed the same tests on Mars.[24]

The question of microbial life on Mars remains unresolved. Nonetheless, on April 12, 2012, an international team of scientists reported studies, based on mathematical speculation through

Labeled Release experiments of the 1976 Viking Mission, that may suggest the detection of "extant microbial life on Mars."[25][26] In addition, new findings from re-examination of the Gas Chromatograph Mass Spectrometer (GCMS) results were published in 2018.[27]

Camera/imaging system

The leader of the imaging team was Thomas A. Mutch, a geologist at Brown University in Providence, Rhode Island. The camera uses a movable mirror to illuminate 12 photodiodes. Each of the 12 silicon diodes are designed to be sensitive to different frequencies of light.

Several broad band diodes (designated BB1, BB2, BB3, and BB4) are placed to focus accurately at distances between six and 43 feet away from the lander.[28] A low resolution broad band diode was named SURVEY.[28]  There are also three narrow band low resolution diodes (named BLUE, GREEN and RED) for obtaining color images, and another three (IR1, IR2, and IR3) for infrared imagery.[28]

The cameras scanned at a rate of five vertical scan lines per second, each composed of 512 pixels. The 300 degree panorama images were composed of 9150 lines. The cameras' scan was slow enough that in a crew shot taken during development of the imaging system several members show up several times in the shot as they moved themselves as the camera scanned.[29][30]

Viking control room at the Jet Propulsion Laboratory, days before the landing of Viking 1.

Control systems

The Viking landers used a Guidance, Control and Sequencing Computer (GCSC) consisting of two

plated-wire memory, while the Viking orbiters used a Command Computer Subsystem (CCS) using two custom-designed 18-bit serial processors.[31][32][33]

Financial cost of the Viking program

The two orbiters cost US$217 million at the time, which is about $1 billion in 2023 dollars.[34][35] The most expensive single part of the program was the lander's life-detection unit, which cost about $60 million then or $400 million in 2023 dollars.[34][35] Development of the Viking lander design cost $357 million.[34] This was decades before NASA's "faster, better, cheaper" approach, and Viking needed to pioneer unprecedented technologies under national pressure brought on by the Cold War and the aftermath of the Space Race, all under the prospect of possibly discovering extraterrestrial life for the first time.[34] The experiments had to adhere to a special 1971 directive that mandated that no single failure shall stop the return of more than one experiment—a difficult and expensive task for a device with over 40,000 parts.[34]

The Viking camera system cost $27.3 million to develop, or about $200 million in 2023 dollars.[34][35] When the Imaging system design was completed, it was difficult to find anyone who could manufacture its advanced design.[34] The program managers were later praised for fending off pressure to go with a simpler, less advanced imaging system, especially when the views rolled in.[34] The program did however save some money by cutting out a third lander and reducing the number of experiments on the lander.[34]

Overall NASA says that $1 billion in 1970s dollars was spent on the program,[5][6] which when inflation-adjusted to 2023 dollars is about $6 billion.[35]

Mission end

The craft all eventually failed, one by one, as follows:[1]

Craft Arrival date Shut-off date Operational lifetime Cause of failure
Viking 2 orbiter August 7, 1976 July 25, 1978 1 year, 11 months, 18 days Shut down after fuel leak in propulsion system.
Viking 2 lander September 3, 1976 April 11, 1980 3 years, 7 months, 8 days Shut down after battery failure.
Viking 1 orbiter June 19, 1976 August 17, 1980 4 years, 1-month, 19 days Shut down after depletion of attitude control fuel.
Viking 1 lander July 20, 1976 November 13, 1982 6 years, 3 months, 22 days Shut down after human error during software update caused the lander's antenna to go down, terminating power and communication.

The Viking program ended on May 21, 1983. To prevent an imminent impact with Mars the orbit of Viking 1 orbiter was raised on August 7, 1980, before it was shut down 10 days later. Impact and potential contamination on the planet's surface is possible from 2019 onwards.[5]

The Viking 1 lander was found to be about 6 kilometers from its planned landing site by the Mars Reconnaissance Orbiter in December 2006.[36]

Message artifact

Each Viking lander carried a tiny dot of microfilm containing the names of several thousand people who had worked on the mission.[37] Several earlier space probes had carried message artifacts, such as the Pioneer plaque and the Voyager Golden Record. Later probes also carried memorials or lists of names, such as the Perseverance rover which recognizes the almost 11 million people who signed up to include their names on the mission.

Viking lander locations

Map of Mars
global topography of Mars, overlaid with the position of Martian rovers and landers. Coloring of the base map indicates relative elevations of Martian surface.
Clickable image: Clicking on the labels will open a new article.
Legend:   Active (white lined, ※)  Inactive  Planned (dash lined, ⁂) )
Bradbury Landing
Deep Space 2
Mars Polar Lander
Perseverance
Schiaparelli EDM
Spirit
Viking 1

See also

References

  1. ^ a b c d e f g h i j Williams, David R. Dr. (December 18, 2006). "Viking Mission to Mars". NASA. Archived from the original on December 6, 2023. Retrieved February 2, 2014.
  2. from the original on October 24, 2023. Retrieved February 2, 2014.
  3. from the original on October 8, 2023. Retrieved February 2, 2014.
  4. ^ Soffen, G. A. (July–August 1978). "Mars and the Remarkable Viking Results." Journal of Spacecraft and Rockets. 15 (4): 193-200.
  5. ^ a b c "Viking 1 Orbiter spacecraft details". NASA Space Science Data Coordinated Archive. NASA. March 20, 2019. Retrieved July 10, 2019.
  6. ^ a b Howell, Elizabeth (October 26, 2012). "Viking 1: First U.S. Lander on Mars". Space.com. Archived from the original on September 6, 2023. Retrieved December 13, 2016.
  7. Gross Domestic Product deflator
    figures follow the MeasuringWorth series.
  8. ^ "The Viking Program". The Center for Planetary Science. Archived from the original on November 20, 2023. Retrieved April 13, 2018.
  9. ^ "Viking Lander". California Science Center. July 3, 2014. Archived from the original on May 27, 2023. Retrieved April 13, 2018.
  10. ^ "Viking Fact Sheet" (PDF). Jet Propulsion Laboratory. Archived from the original (PDF) on March 10, 2012. Retrieved March 27, 2012.
  11. LCCN 92010951
    . Retrieved March 7, 2011.
  12. .
  13. .
  14. .
  15. ^ Hearst Magazines (June 1976). "Amazing Search for Life On Mars". Popular Mechanics. Hearst Magazines. pp. 61–63.
  16. from the original on February 11, 2023. Retrieved December 21, 2023.
  17. ^ Kragh, Helge. "Carl Sagan". Encyclopædia Britannica. Archived from the original on November 8, 2023. Retrieved August 9, 2022.
  18. ^ "Viking". astro.if.ufrgs.br. Archived from the original on August 13, 2023.
  19. ^ "SNAP-19 Radioisotope Thermoelectric Generator Fact Sheet by Energy Research & Development Administration (ERDA) Diagram 2 - The Energy Research and Development Administration". Google Arts & Culture. Retrieved August 9, 2022.
  20. PMID 17723090
    .
  21. ^ Johnson, John (August 6, 2008). "Perchlorate found in Martian soil". Los Angeles Times. Archived from the original on April 19, 2023.
  22. ^ "Martian Life Or Not? NASA's Phoenix Team Analyzes Results". Science Daily. August 6, 2008. Archived from the original on November 18, 2023.
  23. ^ Navarro–Gonzáles, Rafael; Edgar Vargas; José de la Rosa; Alejandro C. Raga; Christopher P. McKay (December 15, 2010). "Reanalysis of the Viking results suggests perchlorate and organics at midlatitudes on Mars". Journal of Geophysical Research: Planets. Vol. 115, no. E12010. Archived from the original on January 9, 2011. Retrieved January 7, 2011.
  24. ^ Than, Ker (April 15, 2012). "Life on Mars Found by NASA's Viking Mission". National Geographic. Archived from the original on April 15, 2012. Retrieved April 13, 2018.
  25. .
  26. ^ Klotz, Irene (April 12, 2012). "Mars Viking Robots 'Found Life'". DiscoveryNews. Retrieved April 16, 2012.
  27. (PDF) from the original on November 3, 2020.
  28. ^ a b c "PDS: Instrument Information". pds.nasa.gov. Retrieved March 28, 2023.
  29. ^ The Viking Lander Imaging Team (1978). "Chapter 8: Cameras Without Pictures". The Martian Landscape. NASA. p. 22.
  30. ^ McElheny, Victor K. (July 21, 1976). "Viking Cameras Light in Weight, Use Little Power, Work Slowly". The New York Times. Archived from the original on February 22, 2021. Retrieved September 28, 2013.
  31. ^ Tomayko, James (March 1988). Computers in Spaceflight: The NASA Experience (Technical report). NASA. CR-182505. Archived from the original on May 6, 2023. Retrieved February 6, 2010.
  32. ^ Holmberg, Neil A.; Robert P. Faust; H. Milton Holt (November 1980). "NASA Reference Publication 1027: Viking '75 spacecraft design and test summary. Volume 1 – Lander design" (PDF). NASA. Retrieved February 6, 2010.
  33. ^ Holmberg, Neil A.; Robert P. Faust; H. Milton Holt (November 1980). "NASA Reference Publication 1027: Viking '75 spacecraft design and test summary. Volume 2 – Orbiter design" (PDF). NASA. Retrieved February 6, 2010.
  34. ^ .
  35. ^
    Nominal Gross Domestic Product
    per capita is used for the inflation-adjusting calculation.
  36. ^ Chandler, David (December 5, 2006). "Probe's powerful camera spots Vikings on Mars". New Scientist. Retrieved October 8, 2013.
  37. ^ "Visions of Mars: Then and Now". The Planetary Society.

Further reading

External links