Venus Express: from Europe to Venus

Rementeria Argote, Nagore

Elhuyar Zientziaren Komunikazioa

After the Sun and the Moon, Venus is the brightest light in the sky. Therefore, it has been known since ancient times, but that does not mean that it is well known. On the contrary, astronomers have many unanswered questions to ask about Venus. The Venus Express probe will clarify these issues.
Venus Express: From Europe to Venus
01/02/2006 | Rementeria Argote, Nagore | Elhuyar Zientzia Komunikazioa
The Venus Express probe has a meter and a half length and a weight of 1.2 tons.
ESA

Venus is back in everyone's mouth. In the years 60-70 he gave much to talk, it was the objective of several missions and - remember the Soviet ship Venera and the American Mariner, for example -. But recently space agencies have forgotten something similar.

Now, however, the European Space Agency has been interested and has sent the Venus Express probe to make Venus known.

Why have you sent a probe to Venus? For it is easier to answer this question than on the contrary, that is, it is not easy to explain why the probes have been sent to farther planets and not to Venus. In any case, the main reason for sending Venus Express is not that Venus is close to Earth, but that it has much to teach -- experts believe that what is learned there will be applicable to Earth.

Venus is said to be the sister of Earth, as they are similar in some of its characteristics: they are terrestrial planets and are believed to have a composition similar to that of the solid side, they have a similar size... In addition, when the two planets were formed, even more

they say they had more. Therefore, knowing Venus better allows us to know the creation of these planets.

(Photo: Recent searches

However, the differences between the two surprise the experts and not the similarities. Venus has several mysteries. And, of course, it is a beautiful challenge to solve these mysteries. Apparently, although they were similar in origin, they had very different evolutionary pathways. An example of this is the atmosphere.

Mission objective: Atmosphere of Venus

On the surface of Venus the temperature is very high (about 465°C on average), while on Earth the temperature is about 15°C. Venus is closer to the Sun, yes, but it is not the reason for the difference (the surface of Venus reaches less solar energy than the Earth's surface). The key is the greenhouse effect.

The greenhouse effect is violent on Venus. Its atmosphere is very compact--the surface pressure of Venus is 90 times higher than that of the Earth - and its main component is carbon dioxide. This is an extreme situation and so far this greenhouse effect has not been properly studied, since the mathematical models applied to Earth do not serve.

It is therefore a question of studying the greenhouse effect on Venus, in the hope that it will contribute to combat the Earth's.

After the Sun and the Moon (foreground in the picture), Venus is the brightest light in the sky.
(Photo: Recent searches

Another issue that is requested is superrotation. Venus, at a height of 50-65 kilometers, has clouds formed by drops of sulfuric acid. The wind speed is huge at this height (about 300 kilometers per hour), which makes the clouds move very fast. Thus, the phenomenon called superrotation occurs: Venus's atmosphere rotates much faster than the planet itself. Clouds only need four days to turn the planet, while the rotation of the planet is very slow: It takes 243 days to turn around its axis and then it has turned around the Sun. Therefore, in Venus it is said that the year is shorter than the day.

To explain these and other phenomena, Venus Express will analyze the atmosphere of Venus: composition of the atmosphere, vertical structure (i.e. characteristics of the atmosphere depending on the height), dynamics of clouds, meteorology, etc.

It will also analyze the surface of Venus. The oldest craters are only five hundred million years old. According to experts, this means that the surface of Venus is renewed from time to time. On Earth energy is constantly released from the interior of the planet, which are volcanoes, which are earthquakes... Instead, on Venus they believe that this energy accumulates within the planet. One day there is a eruption that covers the entire planet and the surface is renewed, disappearing the pre-existing craters.

The probe was launched from the Baikondo cosmodrome (Kazakhstan) on 8 November 2005.
(Photo: ESA)
According to this hypothesis, about five hundred million years ago the last global eruption would have occurred. So there is no older crater. These geological processes are very interesting to compare with those on Earth, and to understand why plate tectonics on Earth and on Venus, at least apparently, do not exist.

It seems that the surface of Venus is closely related to the atmosphere. And Venus Express will collect data to clarify this relationship.

Reuse and save

This mission was born in March 2001. The European Space Agency (ESA) requested proposals for the reuse of the Mars Express probe design. They wanted to use the same design and the same industrial equipment. However, the time was very hard: they had to prepare as soon as possible the new mission, since they had to be launched in 2005.

Think and do it. The Venus Express probe was launched on 8 November 2005 from the Baiconur cosmodrome in Kazakhstan. For the launch they used a Soyuz-Fregat, which is currently heading to Venus.

Like the Venus Express probe, Rosetta also has a VIRTIS camera, which can take photos at once at many wavelengths and receive images like this.
ESA
Therefore, this mission to Venus has a great advantage since its origin: the same technology has been used as other missions. Some parts of the Mars Express and Rosetta missions have been used, as well as infrastructures for all other parts. Thus, progress has been made in terms of design. However, there are three pieces that have had to be specially adapted for the Venus Express, including the camera called VIRTIS.

Also in Euskal Herria looking at Venus

The VIRTIS camera is the most complex tool in the probe. The data collected by this tool will be analyzed by experts from the University of the Basque Country, headed by physicist and astronomer Agustín Sanchez-Lavega.

They have studied the atmospheres of the great planets of the Solar System, Jupiter, Uranus, Saturn and Neptune, and this time they will have the opportunity to participate in the investigation of the atmosphere of Venus.

Jesús Arregi is part of this team and believes that the VIRTIS camera will bring you a lot of information. "With this data we will mainly try to analyze the structure of the atmosphere (which layers it contains), the clouds and their movement, the waves, the existence of wave movements, etc. ".

Venus Express will analyze the surface of Venus in addition to the atmosphere.
ESA
"Some 33-35 years ago the first missions were carried out. Radar maps and probes have been made that have landed in it, although they have been prolonged very little time due to the violent conditions of the same: very high temperatures, extreme pressure and, what may be worse, that the clouds are sulfuric acid (very corrosive). Now we can enrich that image we have made with what we have done so far, both in terms of composition, as well as the physics and chemistry of clouds, as well as the interaction of the atmosphere with the solar wind."

The probe enters the orbit of Venus in March. On the way the tools will be tested and for the moment the tests go well. The implementation of the tools by Venus Express will occur immediately after the consolidation of the orbit and, according to Jesús Arregi, "we will begin to collect the data for the month of May, and from there it will be a work of analysis".

The probe team is ready to work 486 days. However, if it works well, they will continue to work and groups of European physicists and astronomers will continue to collect data to help complete the image of Venus. We expect the results.

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Questions to answer for the mission:
· What characteristics does the atmosphere of Venus as a whole have?
· How does it move?
· How does the composition of the atmosphere change depending on the height?
· How do the atmosphere interact with the surface?
· How does the high atmosphere interact with the solar wind?
Bittersweet in missions to Venus
Between 1961 and 1989 more than thirty spacecraft were sent to Venus. Some came, others did not. The first successful mission was NASA's Mariner 2, which revolved around Venus and whose data showed that the surface temperature of the planet was very high. It happened in 1962.
In 1970, Venera landed 7 on the surface of Venus: a man-made instrument was the first time the Earth landed on a planet that was not the Earth. It took no more than twenty minutes, when the pressure and high temperatures caused by the strong atmosphere completely deteriorated it.
Venera 1.
(Photo: Virtual Space Museum)
Venera 9 (heirs of the previous one) sent in 1975 the first images of the surface: in the image appeared rocks of 30 to 40 centimeters, apparently not eroded.
With such a dense atmosphere, it has not been easy to map the surface of Venus. It has been done by radar. NASA's Magellan spacecraft, for example, orbited around Venus between 1990 and 1994, rotating eight times a day around the planet.
Venus Express tooling
ASPERA-4: will analyze neutral and ionized plasma. He is a descendant of the Mars Express bore-3.
MAG: is a magnetometer that measures the force and direction of the magnetic field. He is a descendant of the ROMAP of Rosetta Lander.
PFS: will vertically sound the atmosphere with infrared Fourier spectroscopy. Heir to Mars Express IRPF.
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SPICAV: spectrometer for ultraviolet and infrared radiation. He is a descendant of SPICAM from Mars Express.
VeRa: Radio survey of the atmosphere and surface. Rosetta RSI descendant.
VIRTIS: is a spectrometer that will work in the near, visible and infrared ultraviolet zone.
VMC: is a camera that receives images of ultraviolet, visible and near infrared field. He is a descendant of HRSC/SRC of Mars Express and OSIRIS of Rosetta.
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