Organic molecules never previously observed in comets, a relatively varied structure on the surface but a fairly homogeneous interior, organic compounds forming agglomerates rather than being dispersed in the ice: these are just some of first results provided by Philae on the surface of comet Churi. This work, carried out as part of ESA’s Rosetta mission, involved researchers from the CNRS, Aix-Marseille Université, Université Joseph Fourier, Université Nice Sophia Antipolis, UPEC, UPMC, Université Paris-Sud, Université Toulouse III — Paul Sabatier and UVSQ, with support from CNES. They are published on July 31, 2015 as part of a set of eight articles in the journalScience. These in situ findings, which contain a wealth of completely new information, reveal several differences in comparison with previous observations of comets and current models.
The landing of the Philae module provided the cometary rendezvous mission Rosetta with an exceptional opportunity: that of studying in situ a cometary nucleus (from its surface to its internal structure), 67P/Churyumov-Gerasimenko (aka Churi). This is likely to shed light on these small celestial bodies that date back to the origins of the Solar System. The data collected by the lander’s ten instruments on November 12-14, 2014 (during the 63 hours that followed Philae’s separation from Rosetta) added to the observations carried out by the Rosetta orbiter1, while its bouncing touchdown on the comet was actually a source of extra information.
Previously unreported organic compounds
Twenty-five minutes after Philae’s initial contact with the cometary nucleus, COSAC (Cometary Sampling and Composition experiment) carried out a first chemical analysis in sniffing mode, that is, by examining particles that passively enter the instrument. These particles probably came from the cloud of dust raised by Philae’s first contact with the ground. Sixteen compounds were identified, divided into six classes of organic molecules (alcohols, carbonyls, amines, nitriles, amides and isocyanates). Of these, four were detected for the first time on a comet (methyl isocyanate, acetone, propionaldehyde and acetamide).
These particles are precursors of molecules important for life (sugars, amino acids, DNA bases, etc). However, the possible presence of these more complex compounds was not unambiguously confirmed in this first analysis. In addition, almost all the compounds detected are potential precursors, products, combinations or by-products of each other, which provides a glimpse of the chemical processes at work in a cometary nucleus, and even in the collapsing solar nebula in the very early Solar System.
Agglomerates of pristine organic matter
The cameras of the CIVA experiment (Comet Infrared and Visible Analyser) reveal that the terrain in the vicinity of Philae’s final landing site is dominated by dark clumps that are probably large grains made up of organic compounds. Since cometary material has hardly been altered since its origins, this means that, early in the Solar System’s history, organic compounds had already clumped together in the form of grains, and not just as small molecules trapped in the ice as was previously thought. The introduction of such grains into planetary oceans could have led to the emergence of life.
Varied terrains concealing a fairly homogeneous interior
COSAC identified a large number of nitrogen compounds but no sulfur compounds, contrary to what the ROSINA instrument on board Rosetta had observed. This suggests that the chemical composition varies depending on the area sampled.
In addition, it was possible to infer the mechanical properties of the surface from Philae’s bouncing touchdown. The lander first touched down on the surface at a site dubbed Agilkia, and then bounced several times before reaching Abydos, the final landing site. Philae’s trajectory and the data recorded by its instruments show that Agilkia is made up of granular materials at least twenty centimeters deep, whereas Abydos has a hard surface.
On the other hand, the comet’s interior appears to be more homogeneous than predicted by models. The radar experiment CONSERT (Comet Nucleus Sounding Experiment by Radio wave Transmission) provides, for the first time, an opportunity to investigate the internal structure of a cometary nucleus. The propagation time and amplitude of the signals that traveled through the upper part of the ‘head’ (the smaller of Churi’s two lobes) show that this part of the nucleus is broadly homogeneous on a scale of tens of meters. The data also confirms that porosity is high (75 à 85%) and shows that the electrical properties of the dust are comparable to those of carbonaceous chondrites.
A rugged surface
The CIVA-P (P for panorama) experiment, made up of seven microcameras, took a panoramic (360°) image of Philae’s final landing site. It shows that fractures already observed on large scales by Rosetta are also present right down to millimeter scales. The fractures are caused by thermal stress, due to the large temperature differences on the comet as it travels around the Sun.
Information about Philae’s location and orientation
The panoramic image, in which a foot or an antenna can be seen in places, also revealed Philae’s position. It rests in a hole about its own size, lying on its side (with only two feet out of three in contact with the ground), and surrounded by cliff walls that hinder its solar energy intake and its communications with Rosetta.
With three periods of observation in conditions of direct visibility between the Rosetta orbiter and Philae, the CONSERT instrument was able to determine the area (150 meters by 15 meters) where Philae is located. This made it easier to reconstruct the robot’s trajectory from the first touchdown site, Agilkia, to the final landing site, Abydos. Then, by using the signals that traveled through the comet’s interior, CONSERT reduced the uncertainty surrounding Philae’s location (on the edge of the region named Hatmehit) to a strip measuring 21 meters by 34 meters.
References: J.- P. Bibring, Y. Langevin, J. Carter, P. Eng, B. Gondet, L. Jorda, S. Le Mouelic, S. Mottola, C. Pilorget, F. Poulet, M. Vincendon.67P/Churyumov-Gerasimenko surface properties as derived from CIVA panoramic images. Science, 2015; 349 (6247): aab0671 DOI:10.1126/science.aab0671 // W. Kofman, A. Herique, Y. Barbin, J.-P. Barriot, V. Ciarletti, S. Clifford, P. Edenhofer, C. Elachi, C. Eyraud, J.-P. Goutail, E. Heggy, L. Jorda, J. Lasue, A.-C. Levasseur-Regourd, E. Nielsen, P. Pasquero, F. Preusker, P. Puget, D. Plettemeier, Y. Rogez, H. Sierks, C. Statz, H. Svedhem, I. Williams, S. Zine, J. Van Zyl. Properties of the 67P/Churyumov-Gerasimenko interior revealed by CONSERT radar. Science, 2015; 349 (6247): aab0639 DOI: 10.1126/science.aab0639 // F. Goesmann, H. Rosenbauer, J. H. Bredehoft, M. Cabane, P. Ehrenfreund, T. Gautier, C. Giri, H. Kruger, L. Le Roy, A. J. MacDermott, S. McKenna-Lawlor, U. J. Meierhenrich, G. M. M. Caro, F. Raulin, R. Roll, A. Steele, H. Steininger, R. Sternberg, C. Szopa, W. Thiemann, S. Ulamec.Organic compounds on comet 67P/Churyumov-Gerasimenko revealed by COSAC mass spectrometry. Science, 2015; 349 (6247): aab0689 DOI: 10.1126/science.aab0689 // J. Biele, S. Ulamec, M. Maibaum, R. Roll, L. Witte, E. Jurado, P. Munoz, W. Arnold, H.-U. Auster, C. Casas, C. Faber, C. Fantinati, F. Finke, H.-H. Fischer, K. Geurts, C. Guttler, P. Heinisch, A. Herique, S. Hviid, G. Kargl, M. Knapmeyer, J. Knollenberg, W. Kofman, N. Komle, E. Kuhrt, V. Lommatsch, S. Mottola, R. Pardo de Santayana, E. Remetean, F. Scholten, K. J. Seidensticker, H. Sierks, T. Spohn. The landing(s) of Philae and inferences about comet surface mechanical properties.Science, 2015; 349 (6247): aaa9816 DOI: 10.1126/science.aaa9816