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Rosetta
Rosetta: Europe’s comet hunter
How did our solar system originate? Where does the water on Earth come from? To find out, a long journey into the past is required. To a place that is very old and very primordial – to a comet.
© ESA
The comet mission Rosetta of the European Space Agency ESA is one of the most fascinating and challenging undertakings of European space flight. It consists of an orbiter and the lander Philae.
The DLR had a significant stake in building the lander and operates the lander control centre that prepared and supported the difficult and hitherto never ventured landing on the comet.
After its launch in 2004, the probe started its ten-year journey to the comet 67P/Churyumov-Gerasimenko at a distance of 400 million kilometres. On its way to the comet, it performed several complex flight manoeuvres (three times passing the Earth and one time passing Mars) to gather momentum for the long way – which meant a detour of 100 million kilometres, however, one that was extremely fuel-saving.
Moreover, it passed the asteroids Steins (September 2008) and Lutetia (July 2010), took images of them and performed extensive physical measurements. In May 2014, Rosetta first entered a trajectory around the comet to perform first measurements in order to map the comet and search for a suitable landing site. On November 12, 2014, the lander Philae – the size of a fridge – separated from the mother ship to touch down on the comet.
It was planned that Philae should immediately anchor its harpoons in the ice. In fact, the lander bounced off after the first touch-down and only came to a rest after several skips. The initially foreseen landing site was missed. Philae performed continuous scientific measurements on the comet’s surface over a period of 56 hours and went to sleeping mode on November 15. On June 13, Philae had gained enough energy to transmit data again. Both, the lander on the comets surface and the orbiter Rosetta are now accompanying the comet on its way to its point nearest to the Sun which will take it several months.
An orbiter and a lander: what is it – and what is on board?
Eleven instruments on board the Rosetta orbiter and ten on board the Philae lander are examining the composition of the comet’s core and it’s getting active on its way to the point nearest to the Sun. The questions whether the comet’s surface is really showing a primal estate and whether comets brought prebiotic molecules and water to the Earth, thus playing a role in the evolution of life, are to be answered with the help of the Rosetta mission.
© ESA
Rosetta: probe and transporter all in one
© ESA
Normally, a probe is launched to space in order to explore a celestial body. A probe is flying by the celestial body or orbiting it and – to put it simple – takes images. Rosetta is a bit different though, since the probe is a transporter for the lander Philae at the same time. Since there are no maps of the target, the comet, the “courier vehicle” had to establish a map using the means available on board and sent it to Earth. Rosetta also has to be capable of controlling itself, for orders from Earth need a transmission time of 30 minutes. What is more: Rosetta is also the communication satellite for Philae. And all that together weighs only 2,900 kilogrammes – with half of the total weight being fuel.
Aboard Rosetta:
ALICE (ultraviolet spectrometer): Searches for noble gases. Their distribution tells us something about the ambient temperature during the evolution 4.5 billion years ago.
OSIRIS (Optical, Spectroscopic and Infrared Remote Imaging System): Two 4-megapixel cameras for orientation, searching for a landing site and taking images, in particular of the particle cloud and the surface of the comet.
VIRTIS (Visible and Infrared Thermal Imaging Spectrometer): For images of the comet’s core from which conclusions can be drawn as to the distribution of detected elements.
MIRO (Microwave Spectrometer for the Rosetta Orbiter): For measuring the degassing rate of molecules from the comet’s core.
ROSINA (Rosetta Orbiter Spectrometer for Ion and Neutral Analysis): A DFMS (Double Focusing Mass Spectrometer) and an RTOF (Flight Time Mass Spectrometer) to detect neutral gas particles.
COSIMA (Cometary Secondary Ion Mass Spectrometer): For examining the comet dust by a mass spectrometer.
MIDAS (Micro-Imaging Dust Analysis System): a scanning probe microscope can depict the fine structure of individual dust particles
RPC (Rosetta Plasma Consortium): ion and electron detectors plus magnetometer to measure the physical properties of the core, among other things.
CONSERT (Comet Nucleus Sounding Experiment by Radio wave Transmission): explores the structure of the comet core by radio waves
GIADA (Grain Impact Analyser): examines the coma and determines number, size, and speed of the dust particles contained therein
RSI (Radio Science Investigation): uses the communication system to measure the gravitational field of the comet core to determine mass and mass distribution.
Philae: the lander and its ten instruments
© ESA
The lander of the Rosetta mission named Philae – a 100-kilogramme lightweight high-tech cube with an edge length of about one metre – is equipped with ten scientific instruments. Its main task is to analyse the comet material on the spot, the presumably most primordial and oldest material existing in our solar system. In particular, element and isotope distribution, organic molecules as well as minerals and ices are to be examined.
The lander is coated with solar cells on almost every side that are capable of producing about eight watts of electric energy on average for the scientific experiments. Since the solar energy available in this aphelion area is only about one tenth of that near the Earth, the energy that can be produced on a comet is scarce and valuable goods. How valuable – that could be experienced during landing on a shadowy landing site: the sun exposure was not sufficient for continuous operation, so the recharging of the storage batteries took months.
APX (Alpha-Particle-X-Ray-Spectrometer): spectrometer for exploring the element composition of the matter directly on the comet’s surface.
CIVA (Comet Infrared and Visible Analyzer): panorama camera system for exploring the landing site, equipped with microscopes for depiction and spectroscopy of material samples from the comet’s surface obtained through the drill SD2.
CONSERT (Comet Nucleus Sounding Experiment by Radio wave Transmission): radio wave probe for tomography (fluoroscopy) of the comet’s core in interplay with the orbiter.
COSAC (Cometary Sampling and Composition): mass spectrometer and gas chromatograph for determining the elementary, isotopic and chemical composition of the freezed components of the comet’s surface up to a depth of about 30 centimetres (including amino acids, if any).
MUPUS (Multi-Purpose Sensors for Surface and Subsurface Science): measuring the surface temperature, near-surface temperature profiles, thermal conductivity of the surface material as well as the solidity of cometary matter. Insight: -170 degrees Celsius.
PTOLEMY: mass spectrometer with upstream gas chromatograph for examining the isotopic composition of the drill tests.
ROLIS (Rosetta Lander Imaging System): camera system with miniaturised CCD camera. Taking images of the landing site on the comet during the descent from the orbiter.
ROMAP (Rosetta Lander Magnetometer and Plasmamonitor): detects the magnetic field of the comet and its plasma environment.
SD2 (Sample, Drill and Distribution): drilling mechanism for acquiring samples from a depth up to 30 centimetres: Insight: 10–20-centimetre dust layer, underneath very, very hard ice – “baked together” in the course of millions of years.
SESAME (Surface Electric Sounding and Acoustic Monitoring Experiment): sensors for measuring the acoustic and dielectric properties of the comet core and its near-surface structure as well as a particle impact monitor. SESAME consists of the instruments CASSE, DIM, and PP.
CASSE (Cometary Acoustic Surface Sounding Experiment): examination of the material structure underneath the comet surface through acoustic methods (comparable to a seismometer and a sonar).
DIM (Dust Impact Monitor): registers the signals that are generated by the impact of cometary dust and ice particles on a sensor cube.
PP (Permittivity Probe): determines the water ice content in the cometary surface layer and its change over time.