Lista sztucznych obiektów na Marsie

Lista sztucznych obiektów na Marsie wymienia wysłany z Ziemi sprzęt, który dotarł na powierzchnię Marsa. Lista nie zawiera mniejszych obiektów, takich jak odrzucone osłony termiczne, spadochrony czy lądowniki łazików Mars Exploration Rover.

Mars
Viking 2 na Marsie

Lista obiektów (stan na 2022)

SondaIlustracjaPaństwoDataMasa (kg)Położenie
Mars 2 [a]
Mars3 lander vsm.jpg
ZSRR197112104º N, 47º W.
Mars 3 [b]
Mars3 lander vsm.jpg
ZSRR19711210Terra Sirenum, 45° S - 158° W
Mars 6 [a]
ZSRR1973635Margaritifer Terra, 29,90° S - 19,42° W
Viking 1
Viking lander model.jpg
USA1976657Chryse Planitia, 22,480° N - 47,967° W
Viking 2
Viking lander model.jpg
USA1976657Utopia Planitia, 48,269° N - 225,99° W
Mars Pathfinder i łazik Sojourner
Lander and rover drawing.gif
USA1997360Ares Vallis, 19,33° N - 33,55° W
Mars Climate Orbiter
Mars Climate Orbiter 2.jpg
USA1999629?
Mars Polar Lander i Deep Space 2 [a]
Mars polar lander.jpg
USA1999500Ultimi Scopuli, 76° S - 195° W
Beagle 2 [c]Wielka Brytania200369Isidis Planitia, 11,5° N - 269,6° W[1]
Spirit (MER-A)
NASA Mars Rover.jpg
USA2004185krater Gusiew, 14,5718° S - 175,4785° E
Opportunity (MER-B)
NASA Mars Rover.jpg
USA2004185Meridiani Planum, 1,9483° S - 354,4742° E
Phoenix
Pia09344.jpg
USA2008350Green Valley
Curiosity (MSL)
Curiosity - The Next Mars Rover.jpg
USA2012900Krater Gale, 4,6° S - 137,2° E
Schiaparelli EDM
Maquette EDM salon du Bourget 2013 DSC 0192.JPG
Rosja, Europejska Agencja Kosmiczna2016577Meridiani Planum, 2,05°S - 6,21°W
InSight
PIA22743-Mars-InSightLander-ArtistConcept-20181024.jpg
USA2018358Elysium Planitia, 4,5024°N - 135,6234°E
Perseverance i Ingenuity
Perseverance rover design.png
USA20211025,8Jezero, 18,445°N - 77,451°E
Tianwen-1
Mars Global Remote Sensing Orbiter and Small Rover at IAC Bremen 2018 02.jpg
Chiny20211285Utopia Planitia, 25,1°N - 109,9°E
Szacowana masa całkowita (kg)11 648,8

Zobacz też

  • Lista skał na Marsie
  • Arctowski (kamień)

Uwagi

  1. a b c Lądownik uderzył w powierzchnię Marsa, kontakt nie został przywrócony po lądowaniu.
  2. Lądownik osiągnął powierzchnię Marsa, ale kontakt został utracony po 15 sekundach.
  3. Lądownik osiągnął powierzchnię Marsa, ale nie nawiązano kontaktu, prawdopodobnie wskutek niekompletnego rozłożenia paneli słonecznych.

Przypisy

Media użyte na tej stronie

NASA Mars Rover.jpg
An artist's concept portrays a NASA Mars Exploration Rover on the surface of Mars. Rovers Opportunity and Spirit were launched a few weeks apart in 2003 and landed in January 2004 at two sites on Mars. Each rover was built with the mobility and toolkit to function as a robotic geologist.
Curiosity - The Next Mars Rover.jpg
This artist concept features NASA's Mars Science Laboratory Curiosity rover, a mobile robot for investigating Mars' past or present ability to sustain microbial life. Curiosity is being tested in preparation for launch in the fall of 2011. In this picture, the rover examines a rock on Mars with a set of tools at the end of the rover's arm, which extends about 2 meters (7 feet). Two instruments on the arm can study rocks up close. Also, a drill can collect sample material from inside of rocks and a scoop can pick up samples of soil. The arm can sieve the samples and deliver fine powder to instruments inside the rover for thorough analysis. The mast, or rover's "head," rises to about 2.1 meters (6.9 feet) above ground level, about as tall as a basketball player. This mast supports two remote-sensing instruments: the Mast Camera, or "eyes," for stereo color viewing of surrounding terrain and material collected by the arm; and, the ChemCam instrument, which is a laser that vaporizes material from rocks up to about 9 meters (30 feet) away and determines what elements the rocks are made of.
Maquette EDM salon du Bourget 2013 DSC 0192.JPG
Autor: Pline, Licencja: CC BY-SA 3.0
Schiaparelli EDM lander concept Paris Air Show 2013
Viking lander model.jpg
Autor: Mark Pelligrino, Licencja: CC-BY-SA-3.0
Viking lander proof test article in the National Air and Space Museum, Smithsonian Institute, Washington, D.C.
Mars3 lander vsm.jpg
Mars 3 Lander model at the Memorial Museum of Cosmonautics in Russia
Mars Hubble.jpg
NASA's Hubble Space Telescope took the picture of Mars on June 26, 2001, when Mars was approximately 68 million kilometers (43 million miles) from Earth — the closest Mars has ever been to Earth since 1988. Hubble can see details as small as 16 kilometers (10 miles) across. The colors have been carefully balanced to give a realistic view of Mars' hues as they might appear through a telescope. Especially striking is the large amount of seasonal dust storm activity seen in this image. One large storm system is churning high above the northern polar cap (top of image), and a smaller dust storm cloud can be seen nearby. Another large dust storm is spilling out of the giant Hellas impact basin in the Southern Hemisphere (lower right).
Mars6.gif
Foto della sonda spaziale sovietica Mars 6 (uguale a Mars 7).
PIA22743-Mars-InSightLander-ArtistConcept-20181024.jpg
PIA22743: InSight Deploys Its Instruments

https://photojournal.jpl.nasa.gov/catalog/PIA22743

This artist's concept depicts NASA's InSight lander after it has deployed its instruments on the Martian surface.

NASA's Jet Propulsion Laboratory, a division of Caltech in Pasadena, California, manages the InSight Project for NASA's Science Mission Directorate, Washington. Lockheed Martin Space, Denver, Colorado built the spacecraft. InSight is part of NASA's Discovery Program, which is managed by NASA's Marshall Space Flight Center in Huntsville, Alabama.

For more information about the mission, go to https://mars.nasa.gov/insight.
Mars Global Remote Sensing Orbiter and Small Rover at IAC Bremen 2018 02.jpg
Autor: Pablo de León, Licencja: CC BY-SA 3.0
Mockup of the Mars Global Remote Sensing Orbiter and Small Rover at the 69th International Astronautical Congress 2018 at Bremen
Perseverance rover design.png
The Perseverance rover relies on the successful design of the Mars Science Laboratory rover, Curiosity. However, Perseverance has a new science and technology toolbox. An important difference is that this rover can sample and cache minerals. To do so, Perseverance has a new coring drill to collect samples. The samples are then sealed in tubes and placed on the surface of Mars.

In the future, another space mission could potentially pick up the samples and bring them to Earth for detailed analysis. Differences Between Perseverance and Curiosity

The large robotic arm on the front of the rover differs from Curiosity's for two main reasons:

   Perseverance will collect rock cores. It needs to collect rock core samples and save them for possible future study by scientists. Curiosity studied samples collected onsite, using the rover's onboard laboratory.
   Perseverance has a larger "hand," or turret. The rover's new functions and new science tools means it must accommodate a larger turret at the end of the robot arm. This turret has the coring drill and two science instruments, plus a color camera for close-up surface inspection and also "selfies" for engineering health checkups. 

There is an internal workspace inside the rover body that is dedicated to picking up, moving and placing drill bits and sample tubes within the Sample Caching System. New motors that drive these specialized movements were needed beyond those used on rover Curiosity. The rover motor controller electronics have been modified from the Curiosity design to accommodate these motors.

New Software to Operate the Rover Perseverance will operate very differently than Curiosity. The new rover will gather 20 sealed samples of Martian rocks and soil. The samples will be set aside in a "cache" on Mars. The team is building new software to run the rover. The software will be updated with improvements throughout the mission.

Besides just managing the new sampling operations, the Mars 2020 rover manages all of its daily activities more efficiently to balance its on-site science measurements while also collecting samples for potential future analysis. To do that, the rover's driving software - the "brains" for moving around -- was changed to give Mars 2020 greater independence than Curiosity ever had.

This allows Perseverance to cover more ground without consulting controllers on Earth so frequently. Also, engineers have added a "simple planner" to the flight software. This allows more effective and autonomous use of electrical power and other rover resources. It allows the rover to shift the time of some activities to take advantage of openings in the daily operations schedule.

New Wheels for Perseverance Engineers redesigned the Mars 2020 Perseverance rover's wheels to be more robust due to the wear and tear the Curiosity rover wheels endured while driving over sharp, pointy rocks. Perseverance's wheels are narrower than Curiosity's, but bigger in diameter and made of thicker aluminum. The combination of the larger instrument suite, new Sampling and Caching System, and modified wheels makes Perseverance heavier than its predecessor, Curiosity.

Credits: NASA/JPL-Caltech.
Mars Viking 22e169.png

Original Caption Released with NASA Image:

Photo from Viking Lander 2 shows late-winter frost on the ground on Mars around the lander. The view is southeast over the top of Lander 2, and shows patches of frost around dark rocks. The surface is reddish-brown; the dark rocks vary in size from 10 centimeters (four inches) to 76 centimeters (30 inches) in diameter. This picture was obtained September 25, 1977. The frost deposits were detected for the first time 12 Martian days (sols) earlier in a black-and-white image. Color differences between the white frost and the reddish soil confirm that we are observing frost. The Lander Imaging Team is trying to determine if frost deposits routinely form due to cold night temperatures, then disappear during the warmer daytime. Preliminary analysis, however, indicates the frost was on the ground for some time and is disappearing over many days. That suggests to scientists that the frost is not frozen carbon dioxide (dry ice) but is more likely a carbon dioxide clathrate (six parts water to one part carbon dioxide). Detailed studies of the frost formation and disappearance, in conjunction with temperature measurements from the lander’s meteorology experiment, should be able to confirm or deny that hypothesis, scientists say.
Pia09344.jpg
NASA's Phoenix Mars Lander monitors the atmosphere overhead and reaches out to the soil below in this artist's depiction of the spacecraft fully deployed on the surface of Mars. Phoenix has been assembled and tested for launch in August 2007 from Cape Canaveral Air Force Station, Fla., and for landing in May or June 2008 on an arctic plain of far-northern Mars. The mission responds to evidence returned from NASA's Mars Odyssey orbiter in 2002 indicating that most high-latitude areas on Mars have frozen water mixed with soil within arm's reach of the surface. Phoenix will use a robotic arm to dig down to the expected icy layer. It will analyze scooped-up samples of the soil and ice for factors that will help scientists evaluate whether the subsurface environment at the site ever was, or may still be, a favorable habitat for microbial life. The instruments on Phoenix will also gather information to advance understanding about the history of the water in the icy layer. A weather station on the lander will conduct the first study Martian arctic weather from ground level. The vertical green line in this illustration shows how the weather station on Phoenix will use a laser beam from a lidar instrument to monitor dust and clouds in the atmosphere. The dark "wings" to either side of the lander's main body are solar panels for providing electric power. The Phoenix mission is led by Principal Investigator Peter H. Smith of the University of Arizona, Tucson, with project management at NASA's Jet Propulsion Laboratory and development partnership with Lockheed Martin Space Systems, Denver. International contributions for Phoenix are provided by the Canadian Space Agency, the University of Neuchatel (Switzerland), the University of Copenhagen (Denmark), the Max Planck Institute (Germany) and the Finnish Meteorological institute. JPL is a division of the California Institute of Technology in Pasadena.
Mars Climate Orbiter 2.jpg
Artist's rendering of the Mars Climate Orbiter
Mars polar lander.jpg
Front illustration of Mars Polar Lander