Viking 2

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Viking 2
Viking Orbiter
Mission type Orbiter and Lander
Operator NASA
Website Viking Project Information
Mission duration

Orbiter:1050 days (1022 sol)[1]

Lander:1316 days (1281 sol)[1]
Spacecraft properties
Manufacturer Orbiter:JPL
Lander:Martin Marietta
Launch mass Orbiter:883 kg (1,947 lb)
Lander:572 kg (1,261 lb)
Power Orbiter:620 W
Lander:70 W
Start of mission
Launch date 18:39, September 9, 1975 (1975-09-09T18:39)[1][2]
Rocket Titan IIIE with Centaur upper stage
Launch site LC-41, Cape Canaveral
End of mission
Last contact April 11, 1980 (1980-04-11)
Orbital parameters
Reference system Areocentric
Mars orbiter
Spacecraft component Viking 2 Orbiter
Orbital insertion August 7, 1976[1][2]
Orbit parameters
Periareion 302 km (188 mi)
Apoareion 33,176 km (20,615 mi)
Mars lander
Spacecraft component Viking 2 Lander
Landing date September 3, 1976
22:37:50 (MSD 36500 00:34 AMT)[1]
Landing site 47°38′N 225°43′W / 47.64°N 225.71°W / 47.64; -225.71 (Viking 2 lander)[1]

The Viking 2 mission was part of the American Viking program to Mars, and consisted of an orbiter and a lander essentially identical to that of the Viking 1 mission.[1] The Viking 2 lander operated on the surface for 1316 days, or 1281 sols, and was turned off on April 11, 1980 when its batteries failed. The orbiter worked until July 25, 1978,[1] returning almost 16,000 images in 706 orbits around Mars.[3]

Mission profile[edit | hide | hide all]

The craft was launched on September 9, 1975. Following launch using a Titan/Centaur launch vehicle and a 333-day cruise to Mars, the Viking 2 Orbiter began returning global images of Mars prior to orbit insertion. The orbiter was inserted into a 1500 x 33,000 km, 24.6 h Mars orbit on August 7, 1976 and trimmed to a 27.3 h site certification orbit with a periapsis of 1499 km and an inclination of 55.2 degrees on 9 August. Imaging of candidate sites was begun and the landing site was selected based on these pictures and the images returned by the Viking 1 Orbiter.

The lander separated from the orbiter on September 3, 1976 at 22:37:50 UT and landed at Utopia Planitia. Normal operations called for the structure connecting the orbiter and lander (the bioshield) to be ejected after separation, but because of problems with the separation the bioshield was left attached to the orbiter. The orbit inclination was raised to 75 degrees on 30 September 1976.

Orbiter[edit | hide]

The orbiter primary mission ended at the beginning of solar conjunction on October 5, 1976. The extended mission commenced on 14 December 1976 after solar conjunction. On 20 December 1976 the periapsis was lowered to 778 km and the inclination raised to 80 degrees.

Operations included close approaches to Deimos in October 1977 and the periapsis was lowered to 300 km and the period changed to 24 hours on 23 October 1977. The orbiter developed a leak in its propulsion system that vented its attitude control gas. It was placed in a 302 × 33,176 km orbit and turned off on 25 July 1978 after returning almost 16,000 images in about 700–706 orbits around Mars.

Lander[edit | hide]

Model of Viking Lander

The lander and its aeroshell separated from the orbiter on 3 September 19:39:59 UT. At the time of separation, the lander was orbiting at about 4 km/s. After separation, rockets fired to begin lander deorbit. After a few hours, at about 300 km attitude, the lander was reoriented for entry. The aeroshell with its ablative heat shield slowed the craft as it plunged through the atmosphere.

The Viking 2 lander touched down about 200 km west of the crater Mie in Utopia Planitia at 48°16′08″N 225°59′24″W / 48.269°N 225.990°W / 48.269; -225.990Coordinates: 48°16′08″N 225°59′24″W / 48.269°N 225.990°W / 48.269; -225.990 at an altitude of -4.23 km relative to a reference ellipsoid with an equatorial radius of 3397.2 km and a flattening of 0.0105 (47°58′01″N 225°44′13″W / 47.967°N 225.737°W / 47.967; -225.737 (Viking 2 landing site planetographic) planetographic) at 22:58:20 UT (9:49:05 a.m. local Mars time).

Approximately 22 kg (49 lb) of propellants were left at landing. Due to radar misidentification of a rock or highly reflective surface, the thrusters fired an extra time 0.4 second before landing, cracking the surface and raising dust. The lander settled down with one leg on a rock, tilted at 8.2 degrees. The cameras began taking images immediately after landing.

The Viking 2 lander was powered by radioisotope generators and operated on the surface until April 11, 1980, when its batteries failed.

Results from the Viking 2 mission[edit | hide]

Landing site soil analysis[edit | hide]

The soil resembled those produced from the weathering of basaltic lavas. The tested soil contained abundant silicon and iron, along with significant amounts of magnesium, aluminum, sulfur, calcium, and titanium. Trace elements, strontium and yttrium, were detected.

The amount of potassium was one fifth of the average for the Earth's crust. Some chemicals in the soil contained sulfur and chlorine that were like those remaining after the evaporation of sea water. Sulfur was more concentrated in the crust on top of the soil than in the bulk soil beneath.

The Sulfur may be present as sulfates of sodium, magnesium, calcium, or iron. A sulfide of iron is also possible.[4] The Spirit rover and the Opportunity rover both found sulfates on Mars.[5]

The Opportunity rover (landed in 2004 with advanced instruments) found magnesium sulfate and calcium sulfate at Meridiani Planum.[6] Using results from the chemical measurements, mineral models suggest that the soil could be a mixture of about 80% iron-rich clay, about 10% magnesium sulfate (kieserite?), about 5% carbonate (calcite), and about 5% iron oxides (hematite, magnetite, goethite?).

These minerals are typical weathering products of mafic igneous rocks.[7] All samples heated in the gas chromatograph-mass spectrometer (GCMS) gave off water.

However, the way the samples were handled prohibited an exact measurement of the amount of water. But, it was around 1%.[8] Studies with magnets aboard the landers indicated that the soil is between 3 and 7 percent magnetic materials by weight. The magnetic chemicals could be magnetite and maghemite, which could come from the weathering of basalt rock.[9][10] Subsequent experiments carried out by the Mars Spirit rover (landed in 2004) suggest that magnetite could explain the magnetic nature of the dust and soil on Mars.[11]

Viking 2 lander image of Utopia Planitia.

Search for life[edit | hide]

Viking 2 carried a biology experiment whose purpose was to look for life. The Viking 2 biology experiment weighed 15.5 kg (34 lb) and consisted of three subsystems: the Pyrolytic Release experiment (PR), the Labeled Release experiment (LR), and the Gas Exchange experiment (GEX). In addition, independent of the biology experiments, Viking 2 carried a Gas Chromatograph/Mass Spectrometer (GCMS) that could measure the composition and abundance of organic compounds in the Martian soil.[12]

The results were surprising and interesting: the GCMS gave a negative result; the PR gave a positive result, the GEX gave a negative result, and the LR gave a positive result.[13] Viking scientist Patricia Straat recently stated, "Our (LR) experiment was a definite positive response for life, but a lot of people have claimed that it was a false positive for a variety of reasons."[14]

Most scientists now believe that the data were due to inorganic chemical reactions of the soil; however, this view may be changing after the recent discovery of near-surface ice near the Viking landing zone.[citation needed] Some scientists still believe the results were due to living reactions. No organic chemicals were found in the soil.[citation needed]

Mars has almost no ozone layer, unlike the Earth, so UV light sterilizes the surface and produces highly reactive chemicals such as peroxides that would oxidize any organic chemicals.[15] The Phoenix Lander discovered the chemical perchlorate in the Martian soil. Perchlorate is a strong oxidant, so it may have destroyed any organic matter on the surface.[16] Perchlorate is now considered widespread on Mars, making it hard to detect any organic compounds on the Martian surface.[17]

Viking 2 lander image gallery[edit | hide]

Viking 2 lander Camera 1 NOON HIGH RESOLUTION MOSAIC (With Low Resolution Color).
Viking 2 Lander Camera 2 FROST (Low Resolution Color) Sol 1028, 1030 and 1050 between 11:34 and 12:40.

Orbiter results[edit | hide]

Viking program[edit | hide]

The Viking 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 carved deep valleys, eroded grooves into bedrock, and traveled thousands of kilometers. Areas of branched streams, in the southern hemisphere, suggested that rain once fell.[18][19][20]

The images below, some of the best from the Viking Orbiters, are mosaics of many small, high resolution images. Click on the images for more detail. Some of the pictures are labeled with place names.

Viking 2 lander in space art[edit | hide]

NASA Space art showing astronauts in Mars space suits approach the Viking 2 Mars lander

See also[edit | hide]

References[edit | hide]

  1. 1.0 1.1 1.2 1.3 1.4 1.5 1.6 1.7 Williams, David R. Dr. (December 18, 2006). "Viking Mission to Mars". NASA. Retrieved February 2, 2014. 
  2. 2.0 2.1 Nelson, Jon. "Viking 2". NASA. Retrieved February 2, 2014. 
  3. [1]
  4. Clark, B. et al. 1976. Inorganic Analysis of Martian Samples at the Viking Landing Sites. Science: 194. 1283–1288.
  5. Mars Exploration Rover Mission: Press Release Images: Opportunity
  6. Christensen, P. et al. 2004. Mineralogy at Meridiani Planum from the Mini-TES Experiment on the Opportunity Rover. Science: 306. 1733–1739
  7. Baird, A. et al. 1976. Mineralogic and Petrologic Implications of Viking Geochemical Results From Mars: Interim Report. Science: 194. 1288–1293.
  8. Arvidson, R et al. 1989. The Martian surface as Imaged, Sampled, and Analyzed by the Viking Landers. Review of Geophysics:27. 39-60.
  9. Hargraves, R. et al. 1976. Viking Magnetic Properties Investigation: Further Results. Science: 194. 1303–1309.
  10. Arvidson, R, A. Binder, and K. Jones. The Surface of Mars. Scientific American
  11. Bertelsen, P. et al. 2004. Magnetic Properties Experiments on the Mars Exploration rover Spirit at Gusev Crater. Science: 305. 827–829.
  12. Life on Mars Archived October 20, 2014, at the Wayback Machine.
  13. Viking Data May Hide New Evidence For Life. Barry E. DiGregorio, July 16, 2000.
  14. Viking 2 Likely Came Close to Finding H2O. Archived September 30, 2009, at the Wayback Machine.
  15. Hartmann, W. 2003. A Traveler's Guide to Mars. Workman Publishing. NY NY.
  16. Alien Rumors Quelled as NASA Announces Phoenix Perchlorate Discovery. Archived September 4, 2010, at the Wayback Machine. A.J.S. Rayl, August 6, 2008.
  17. Chang, Kenneth (1 October 2013). "Hitting Pay Dirt on Mars". New York Times. Retrieved 10 October 2013. 
  18. ISBN 0-8165-1257-4
  19. Raeburn, P. 1998. Uncovering the Secrets of the Red Planet Mars. National Geographic Society. Washington D.C.
  20. Moore, P. et al. 1990. The Atlas of the Solar System. Mitchell Beazley Publishers NY, NY.

External links[edit | hide]

Map of Marswikipedia:Acidalia Planitiawikipedia:Acidalia Planitiawikipedia:Alba Monswikipedia:Amazonis PlanitiaAonia Terrawikipedia:Arabia Terrawikipedia:Arcadia Planitiawikipedia:Arcadia Planitiawikipedia:Argyre Planitiawikipedia:Elysium Monswikipedia:Elysium Planitiawikipedia:Hellas Planitiawikipedia:Hesperia Planumwikipedia:Isidis PlanitiaWikipedia:Lucas PlanumWikipedia:Lyot Craterwikipedia:Noachis Terrawikipedia:Olympus Monswikipedia:Promethei TerraWikipedia:Rudaux Craterwikipedia:Solis Planumwikipedia:Tempe Terrawikipedia:Terra Cimmeriawikipedia:Terra Sabaeawikipedia:Terra Sirenumwikipedia:Tharsis Monteswikipedia:Utopia Planitiawikipedia:Valles Marineriswikipedia:Vastitas Borealiswikipedia:Vastitas Borealis
The image above contains clickable linksInteractive imagemap of the global topography of Mars, overlain with locations of Mars landers and rovers
Red label = Rover; Blue label = Lander; bold text = currently active. Click on label to go to the page. Hover your mouse to see the names of prominent geographic features, and click on map to go to its page in Wikipedia.
Reds and pinks are higher elevation (+3 km to +8 km); yellow is 0 km; greens and blues are lower elevation (down to −8 km). Whites (>+12 km) and browns (>+8 km) are the highest elevations.Coloring of the base map indicates relative elevations, based on data from the Mars Orbiter Laser Altimeter on NASA's Mars Global Surveyor. Axes are latitude and longitude; Poles are not shown.
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This article uses material from Viking 2 on Wikipedia (view authors). License under CC BY-SA 3.0. Wikipedia logo
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