Chang'e-3

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Chang'e-3
NSSDC ID 2013-070A
Mission goal Earth moon
Client CNSA
Launcher CZ-3B
Course of the mission
Start date December 1, 2013, 17:30 UTC
launch pad Xichang Cosmodrome
 
December 1st, 2013 begin
 
2nd December 2013 Transfer orbit
 
December 6, 2013 Reaching a lunar orbit
 
December 14, 2013 Landing on the moon
 
January 25, 2014 Rover drive failure
 
February 13, 2014 Rover sends data
 
3rd August 2016 Failure of the rover
 
circa 2040 End of planned life of the lander's radioisotope battery.

Chang'e-3 ( Chinese  嫦娥 三號  /  嫦娥 三号 , Pinyin Cháng'é Sānhào ) is the third lunar probe of the China National Space Administration (CNSA) as part of the lunar program of the People's Republic of China . The two predecessor probes Chang'e-1 and Chang'e-2 were orbiters , Chang'e-3 landed successfully on the moon and set down the moon rover Jadehase (Yutu, 玉兔 ). The Chang'e 3 lander is still active and providing data.

The names refer to the Chinese moon goddess and her companion .

Mission history

On December 1, 2013, aboard Chang'e-3 launched a missile of the type Long March 3B from the Xichang Satellite Launch Center in Earth orbit. 20 minutes after the launch, the probe separated from the rocket. The probe swiveled out of orbit into a transfer orbit. The swing into a lunar orbit on December 6th was prepared with three corrective maneuvers, after a braking maneuver a circular orbit around the moon with an altitude of 100 km was reached. After lowering the periselenum to 15 km, the landing was initiated by another braking maneuver. During the last 12 minutes of the descent, the probe then acted completely autonomously and independently looked for a suitable landing site.

Chang'e-3 (moon)
Chang'e-3
Chang'e-3
Landing position of Chang'e-3 on the lunar surface
Galileo image with the landing position of Chang'e-3
LRO image with the landing site on the border between darker and lighter basalt soil
LRO picture from December 25th 2013 with the lander (big arrow) and the rover (small arrow)
Zi Wei crater, the eastern edge of which has been studied

The soft landing took place on December 14 at 13:11:18 UTC, one orbit earlier than originally planned and thus 250 km east of the Sinus Iridum in the Mare Imbrium at 44.115 ° N 19.515 ° W. Live images of the descent were transmitted. Six hours later the rover (mass 140 kg) left the lander via a ramp. To generate energy on lunar nights, Chang'e-3 has a radioisotope generator on board, which is supported on lunar day by energy from the two solar panels. The moon rover Jadehase only has solar panels and does not work during the moonlit nights. He has a radionuclide heating element on board to protect against the cold at night .

To support the probe, China worked with ESA , which provided the ESTRACK antenna network for receiving the radio signals and for the flight phase . The ESA also helped to determine the position during the landing. China now has enough of its own facilities to operate the probe.

On December 25, 2013, the APX spectrometer (Active Particle-induced X-ray Spectrometer) of the moon rover Yutu was used for the first time to determine the chemical composition of the moon's surface. It is an X-ray spectrometer that determined the percentage chemical composition of rocks and lunar regolith using X -ray fluorescence spectroscopy and particle-induced X-ray emission ( PIXE ).

Between January 27 and February 13, 2014, media reports appeared about malfunctions of the rover Yutu and problems with reactivating it after the second lunar night. However, it was possible to re-establish contact with the device. On March 10, 2014, after the third lunar night, Yutu reported again from his permanent position.

On August 3, 2016 it was announced that the Jade Bunny finally wishes "good night". Although Yutu was designed for only three months, the rover explored the moon for 31 months.

The Luna-based Ultraviolet Telescope (LUT) of the National Astronomical Observatories of the Chinese Academy of Sciences on the lander, however, is still active (as of June 2020). Since it is built into a chamber to protect against the electrostatically charged lunar dust, the hatch of which is closed at sunrise and sunset - lunar dust rises increasingly at light-dark borders - so far there have been no dust deposits on the mirrors of the Ritchey-Chrétien-Cassegrain Telescope . The 238 Pu in the lander's radionuclide battery should last for about 30 years, and unless unforeseen incidents occur, astronomers could make their observations in the near-ultraviolet range (400-300 nm) during this entire time .

For the Chang'e 3 mission, the TT&C system of the lunar program was expanded in the years 2009–2012 so that the military deep-space stations at Kashgar and Giyamusi - only the People's Liberation Army is authorized and able to send control signals to Chinese spacecraft to send - address two different targets with a wave packet, so you can control the lander and rover at the same time. The viewing angle of the ultraviolet telescope can be changed by a flat mirror that is mounted at a certain distance in front of its light incidence opening and freely pivotable via a cardanic suspension . When the astronomers want to examine a certain object in space, they inform the deep-space stations via the Xi'an satellite control center , which then issue the appropriate control commands. The AIMO CCD sensor manufactured by the British e2v (formerly English Electric Valve Company , since 2017 Teledyne e2v ) sends the recorded images whenever there is visual contact with China to the civilian ground stations in Miyun and Kunming , which are assigned during the lunar missions receive the downlink traffic of the scientific payloads.

Results

Through the spectrographic recordings of the lunar surface taken in 1994 by NASA's Clementine probe , in 1998/99 by Lunar Prospector (also NASA), in 2008/2009 by Chandrayaan-1 of the Indian Space Research Organization and above all by Chang'e-1 and Chang'e-2 , one had a pretty good idea of ​​the mineralogical composition of the upper layers of the moon. The landing site of Chang'e-3 was carefully chosen on the edge of a small, only 27-80 million year old (i.e. relatively fresh) crater with a diameter of about 450 m, where the meteorite impact at the time came to the surface from a depth of 40-50 m had hurled. On the east side of this crater, officially called Zǐwēi (紫微, literally “Purple Forbidden Area”, meaning “Area of ​​the Imperial Palace”) since October 5, 2015 , the Rover Yutu covered a total of 114 meters. During its journey, the Jade Hare approached the crater rim on a more or less J-shaped course, stopping 8 times, in addition to the occasional photo-stop, to take measurements. After the first evaluations of the data he provided, his ground penetrating radar measured a two to three meter thick regolith layer , followed by a 41 to 46 meter thick basalt layer with a striking amount of titanium oxide. Beneath this, within the measuring range of 140 meters depth, lies a second basalt layer with a different composition.

Particularly interesting are the results of the spectrographic recordings that the rover made at four points from with the help of its infrared spectrometer ( Visible and Near-infrared Imaging Spectrometer or VNIS) and its alpha particle X-ray spectrometer ( Active Particle-induced X-ray Spectrometer or APXS) the lunar surface made. The main elements iron , titanium , magnesium , aluminum , silicon , potassium and calcium as well as some trace substances were detected. The percentage composition of the soil in terms of ferrous oxide (extremely high), calcium oxide (high), titanium dioxide (medium), aluminum oxide (little) and silicon dioxide (very little) was in stark contrast to the soil samples obtained by The Apollo astronauts were brought back to Earth, but corresponded to what the researchers around Ling Zongcheng (凌宗成) from the Institute for Space Science at Shandong University expected after the images made by the previous probes from the lunar orbit for this place. This showed the usefulness of area-wide long-range reconnaissance using orbital probes and proved their reliability.

The landing site was officially named Guǎnghán Gōng ( 廣寒宮  /  广寒宫  - “Palace of the Wide Cold”) on October 5, 2015 , after the moon palace in Chinese mythology, where Chang'e and Yutu lived.

The determination of the hydroxyl radical density in the very thin atmosphere or exosphere of the moon brought a rather unpleasant result . Wang Jing (王 竞) from the Xinglong Station of the National Astronomical Observatories of the Chinese Academy of Sciences , together with several colleagues, analyzed the spectrum of the background in 498 images taken by the Luna-based Ultraviolet Telescope (LUT) during the lunar days of bright stars as Thuban , Kochab etc. had recorded. The spectral line of the OH radical, which is created by the impact of ultraviolet radiation on water molecules generated by the solar wind, is at 308.7 nm, i.e. in the observation range of the CCD sensor in the 15 cm telescope. After processing the data and eliminating sources of error, Wang Jing's group came to the conclusion that there are fewer than 10,000 hydroxyl radicals per cubic centimeter in the exosphere of the moon, i.e. 2 orders of magnitude less than the 1,000,000 radicals that are found at Remote observations with the Hubble Space Telescope found, and 6 orders of magnitude less than what the Indian Chandrayaan-1 moon orbiter found. This means that there is, at least in the Palace of the Wide Cold, significantly less water on the moon than previously assumed.

With a quartz crystal microbalance mounted on the lander developed by Yao Rijian (姚 日 剑), Wang Yi (王 鹢) and others in 2009 at the Research Institute 510 (Physics) of the Chinese Academy of Space Technology in Lanzhou , the amount of Moondust deposited on the probe was measured, funded by the National Foundation for Natural Sciences and, from 2016, by the Weapons Development Department of the Central Military Commission . After a thorough analysis and consideration of the special features of the lander, the scientists of the moondust research group at Institute 510 (510 所 月 尘 测量 技术 研究 团队) published their results in the Journal of Geophysical Research  : Planets on August 2, 2019 . At a height of 190 cm above the lunar surface in the northern Mare Imbrium , 0.0065 mg of lunar dust per square centimeter was deposited on the immobile lander during twelve lunar days (that is, “blown up” by the solar wind), which corresponds to an annual deposition rate of around 21.4 μg / cm². This was the first time that such long-term measurements were carried out directly on the lunar surface (and not from orbit). The data obtained will now be incorporated into the dust protection measures for future lunar probes at the Chinese Academy for Space Technology.

By January 2016, 35 gigabytes of image material that had been recorded with the cameras of Lander and Rover had been published.

See also

literature

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Web links

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