View of the Venus gas envelope with infrared sensors
The flyby of Venus and the Earth-moon-flyby that took place in spring 2020 are spaceflight maneuvers used to test the functionality of some of the experiments on board both orbiters and to calibrate the sensors and signal chains with the data obtained. "Scientific measurements will also be carried out during approach and departure and at the closest approach to Venus," say the two people primarily responsible for the MERTIS instrument, Jörn Helbert from the DLR Institute of Planetary Research and Harald Hiesinger from the Institute of Planetology at the University of Münster. "Our imaging spectrometer MERTIS, which we built together with industry and international partners, will be used again to make these measurements," says Helbert.
MERTIS was primarily developed to measure spectra of rock-forming minerals on Mercury's atmosphere-free surface. But with its infrared sensors, it can also look into the dense gas envelope of Venus down to a certain depth. "We are already expecting some very interesting findings, with more to follow in 2021, when we will be much closer to Venus," adds Hiesinger.
MERTIS is an imaging infrared spectrometer and radiometer with two uncooled radiation sensors that are sensitive to wavelengths of 7 to 14, and 7 to 40 micrometers, respectively. During two series of measurements, the first of which begins today, MERTIS will capture almost 100,000 individual images. The first series will begin as the spacecraft approaches from a distance of approximately 1.4 million kilometers from Venus up to a distance of 670,000 kilometers. After a pause to check the instrument, the second series will start at a distance of 300,000 kilometers, 11 hours before the Venus flyby, and will continue until BepiColombo is almost 120,000 kilometers from Venus four hours before the closest approach of the flyby.
Venus as the focus of planetary research
Venus is almost as large as Earth, but has developed in a completely different way. Its atmosphere is much denser, consisting almost entirely of carbon dioxide, and thus the planet experiences a very strong greenhouse effect. This results in a permanent surface temperature of around 470 degrees Celsius. There is no water and therefore it is thought that no life could survive on the surface.
It is quite possible that volcanoes are still active on Venus. "These would be detected, for example, through the sulfur dioxide that they emit," says Helbert. "Following the first measurements made in the 1960s and 1970s, about 10 years ago, ESA's Venus Express mission recorded a massive reduction, by more than half, of sulfur dioxide concentrations. Venus literally 'smells' of active volcanoes. MERTIS could now provide us with new information." The experiments will be complemented by simultaneous observations from the Japanese Venusian orbiter Akatsuki and from a dozen professional telescopes as well as information from amateur astronomers on Earth.
Venus only recently came under the spotlight of science and the media when a group of astronomers used telescopes in Hawaii and Chile to prove beyond doubt the presence of the trace gas phosphine (or monophosphane, chemical formula PH3) on Venus. Phosphine is industrially manufactured on Earth for use in pest control, but is also produced by biological processes in sapropel or in the digestive tracts of vertebrates. Phosphine is a very short-lived molecule, so there must be a current source of the molecule on Venus or in its atmosphere.
Previous modeling of natural phosphine sources such as volcanism, chemical reactions following meteorite impacts or lightning discharges cannot explain the measured concentrations. This is why the possibility that the phosphine is produced by microorganisms high up in Venus's atmosphere is debated by planetary researchers. This finding could suggest that life exists in the temperate 'flying carpets' of sulphuric acid clouds that exist at altitudes of 40 to 60 kilometers. The authors of the study themselves question this idea, however, and indicate the need for further measurements in the future. In the future, Venus will be the target of ESA and NASA missions.
Venus, an exoplanet on our doorstep
MERTIS and the other five activated instruments on board the Mercury Planetary Orbiter will not be able to detect any phosphine molecules from the distance of the flyby. Nevertheless, the flyby is scientifically interesting, as the spacecraft can be used to study Venus as if it were a distant, Earth-like extrasolar planet with a solid surface and dense atmosphere.
"During the Earth flyby, we studied the moon, characterizing MERTIS in flight for the first time under real experimental conditions. We achieved good results," says Gisbert Peter, MERTIS project manager at the DLR Institute of Optical Sensor Systems, which was responsible for the design and construction of MERTIS. "Now, we are pointing MERTIS toward a planet for the first time. This will allow us to make comparisons with measurements taken prior to the launch of BepiColombo, to optimize operation and data processing, and to gain experience for the design of future experiments."
All experiments will focus on measuring the composition, structure and dynamics of the atmosphere of Venus, the ionosphere of the planet and—using the instruments on the Japanese MMO (Mercury Magnetospheric Orbiter) – the induced magnetosphere of Venus.
Saving fuel with planetary flybys
Following BepiColombo's first flyby of Earth on 10 April 2020, its flyby of Venus is designed to continue to slow the spacecraft down without using any fuel. This is necessary in order to compress the spacecraft's orbital ellipse toward a circular orbit that is ultimately almost geometrically identical to the orbit of Mercury. The spacecraft 'falls' toward Venus on its spiraled orbit through the inner solar system at various speeds depending on its distance from the sun. At Venus, BepiColombo will reduce its heliocentric speed by 37 kilometers per second (133,500 km/h). The flyby will take place at a distance of 116 million kilometers from Earth. Venus is currently ahead of Earth in its orbit and is visible in the eastern sky just before dawn.
Due to the sun's strong gravitational pull, planetary missions to the inner solar system can only be achieved with very complex trajectories. With the maneuver on Thursday, the spacecraft's relative speed compared to Mercury will be reduced to 1.84 kilometers per second. At the end of its spiraled flight between the orbits of Earth and Mercury, BepiColombo will orbit the sun at almost the same speed as Mercury. It will then easily be captured by the gravity of the smallest planet in the solar system on 5 December 2025 and will maneuver itself into a polar orbit. BepiColombo was launched on 20 October 2018 on board an Ariane 5 launch vehicle from the European spaceport in Kourou.
The use of flyby maneuvers was first implemented during NASA's Mariner 10 mission, enabling the spacecraft to make two additional close flybys of Mercury after it had already traveled past the planet once. The calculations were made by Italian engineer and mathematician Giuseppe 'Bepi' Colombo, a professor at the University of Padua. Colombo was invited to a conference in preparation for the Mariner 10 mission at NASA's Jet Propulsion Laboratory in Pasadena, California, in 1970. After seeing the original mission plan, he realized that a highly precise first flyby could allow for two additional flybys of Mercury. The current European-Japanese Mercury mission was named in his honor.