Microscopie hyperspectrale dans le proche IR pour l'analyse in situ d'échantillons (l'instrument MicrOmega à bord des missions Phobos Grunt, Hayabusa-2 et ExoMars)

L analyse de la surface par des moyens spatiaux des objets du Système Solaire permet de remonter aux processus géologiques, géochimiques et climatiques qui s y sont déroulés. La microscopie hyperspectrale dans le proche infrarouge, de par sa faculté à analyser la composition moléculaire et minéralogique d un échantillon à l échelle des grains, est une technique novatrice dans le cadre de la planétologie, amenée à compléter les mesures effectuées depuis l orbite et celles des autres instruments d'analyse in situ. Les développements techniques récents liés aux détecteurs matriciels dans le proche infrarouge, aux machines cryogéniques de dimension et masse réduites, ainsi qu aux systèmes dispersifs nous donnent désormais la capacité de développer des microscopes hyperspectraux compatibles en termes de masse, volume, puissance et télémétrie avec les contraintes fortes liées à un atterrisseur/rover. Le concept développé a ainsi donné naissance à l instrument MicrOmega, sélectionné pour faire partie de la charge utile Pasteur du rover ExoMars de l'ESA. Mon travail de thèse s'est tout d'abord fixé pour objectif d'étudier l'extension de la gamme spectrale de l'instrument vers l'infrarouge au-delà de 2.5 m afin d'identifier et de caractériser d'éventuels composés carbonés ; j'ai procédé à l'analyse des conséquences de cette extension sur la conception de l'instrument. Les résultats de ces études ont permis de faire évoluer le design et les spécifications de l'instrument MicrOmega pour ExoMars. Mon implication dans la préparation de cette mission m'ont conduit à développer des algorithmes de détection automatiques de composés spécifiques au sein d'un échantillon, de manière à coupler les mesures de MicrOmega avec celles du spectromètre RAMAN RLS et du laser à désorption de MOMA, permettant ainsi d'accroître la synergie entre les instruments de la charge utile.Au cours de ma thèse, le décalage du lancement de la mission Phobos Grunt a permis de proposer d'y adjoindre un modèle de MicrOmega ; j'ai ainsi pu participer à l'ensemble des phases de développement d'un modèle de vol de MicrOmega, de sa conception initiale à l'étalonnage final. Suite à ce développement, une autre mission d'opportunité est apparue, à laquelle j'ai également été associé : l'instrument MicrOmega a été sélectionné pour la mission Hayabusa-2, destinée à l'analyse in situ d'un astéroïde-C.The characterization of the surface of planetary objects, through space observations, gives key clues to the past and present geological, geochemical and climate processes. Near-infrared hyperspectral microscopy, through its capability to identify the molecular and mineralogical composition of a sample at its grain size, is an innovative technique that will efficiently complement both remote sensing and in situ measurements. Recent technical achievements in near-infrared detectors, space cryo-coolers and dispersive systems, has enabled us to design MicrOmega, a highly miniaturized near-infrared hyperspectral microscope, to be implemented on landers/rovers: it has been selected within the Pasteur payload of the ESA ExoMars rover, with launch scheduled for 2018.My thesis activity started with the study of the extension of the spectral range beyond 2.5 m, driven by the goal of identifying and characterizing potential organic compounds, and with the analysis of the impact on the instrument design of such an extension. The outcomes were used to set the MicrOmega / ExoMars instrument baseline. My involvement in this program included the development of algorithms enabling, in an automated way, the identification and the location, within the analyzed samples, of compounds with specific composition; it will be used both to limit the amount of information to be downloaded, and to indicate key targets for point analyzers, such as the Raman spectrometer RLS and the laser desorption spectrometer MOMA, thus increasing the synergy between the suite of ExoMars laboratory instruments. During my thesis, the shift of the launch of the Phobos Grunt mission opened the possibility to develop and deliver a flight model of MicrOmega, in less than two years; I thus have been involved in all steps of its development, from its design to its final calibration. As a follow-up, another mission of opportunity emerged, to which I have also been associated: MicrOmega has been selected as part of the Hayabusa-2 mission, which will in situ analyze a C-type asteroid.PARIS11-SCD-Bib. électronique (914719901) / SudocSudocFranceF

Composition of Syrtis Major volcanic plateau

Syrtis Major, a low-relief volcanic shield centered near 295 degrees 10 degrees N, is an old, well-preserved and exposed volcanic region on Mars which formed at the end of the heavy bombardment period. The composition of these volcanic materials has importance for understanding the thermal and chemical history of Mars. Imaging spectrometer data of the Syrtis Major volcanic plateau are used in this analysis to identify major compositional components. First and second order even channel reflectance spectra between 0.77 and 2.55 microns from four broad classes of materials on Syrtis Major are given. For the volcanic materials, there are three primary classes characterized by albedo, slope, and shape of the 10 micron band. To emphasize the latter, straight line continua were removed from each spectral segment and replotted in another figure. Each spectrum shows a band minima near 0.96 microns and 2.15 microns indicative of pyroxene mineral absorptions. Comparison of these band minima with studies of pyroxene reflectance spectra suggests that the pyroxenes in the volcanics of Syrtis Major are high calcium pyroxene with a Ca/(Mg+Fe+Ca) ratio of 0.2 to 0.3. The most likely pyroxene is an augite

Disk-resolved spectral reflectance properties of Phobos from 0.3-3.2 micron: Preliminary integrated results from Phobos 2

The Phobos 2 mission provided multispectral observations of Phobos over a large wavelength range and with relatively high spectral resolution. Here, researchers integrate results from three multispectral detectors by determining the ultraviolet-visible near infrared spectral properties of color and brightness features recognized in VSK TV images. Researchers present evidence that there are two fundamental spectral units within the region of overlapping coverage by the detectors. They describe the units' spectral and reflectance properties and discuss the implications of these results for the composition of Phobos

Near-tropical subsurface ice on Mars

Near-surface perennial water ice on Mars has been previously inferred down to latitudes of about 45{\deg} and could result from either water vapor diffusion through the regolith under current conditions or previous ice ages precipitations. In this paper we show that at latitudes as low as 25{\deg} in the southern hemisphere buried water ice in the shallow (< 1 m) subsurface is required to explain the observed surface distribution of seasonal CO2 frost on pole facing slopes. This result shows that possible remnants of the last ice age, as well as water that will be needed for the future exploration of Mars, are accessible significantly closer to the equator than previously thought, where mild conditions for both robotic and human exploration lie

MASCOT’s in situ analysis of asteroid Ryugu in the context of regolith samples and remote sensing data returned by Hayabusa2

The Hayabusa2 mission provided a unique data set of asteroid Ryugu that covers a wide range of spatial scale from the orbiter remote sensing instruments to the returned samples. The MASCOT lander that was delivered onto the surface of Ryugu aimed to provide context for these data sets by producing in situ data collected by a camera (MasCam), a radiometer (MARA), a magnetometer (MasMag) and a spectrometer (MicrOmega). In this work, we evaluate the success of MASCOT as an integrated lander to bridge the gap between orbiter and returned sample analysis. We find that MASCOT’s measurements and derivatives thereof, including the rock morphology, colour in the visible wavelengths, possible meteorite analogue, density, and porosity of the rock at the landing site are in good agreement with those of the orbiter and the returned samples. However, it also provides information on the spatial scale (sub-millimetres to centimetres) at which some physical properties such as the thermal inertia and reflectance undergo scale-dependent changes. Some of the in situ observations such as the presence of clast/inclusions in rocks and the absence of fine particles at the landing site was uniquely identified by MASCOT. Thus, we conclude that the delivery of an in situ instrument like MASCOT provides a valuable data set that complements and provides context for remote sensing and returned sample analyses

New near-IR observations of mesospheric CO2 and H2O clouds on Mars

Carbon dioxide clouds, which are speculated by models on solar and extra-solar planets, have been recently observed near the equator of Mars. The most comprehensive identification of Martian CO2 ice clouds has been obtained by the near-IR imaging spectrometer OMEGA. CRISM, a similar instrument with a higher spatial resolution, cannot detect these clouds with the same method due to its shorter wavelength range. Here we present a new method to detect CO2 clouds using near-IR data based on the comparison of H2O and CO2 ice spectral properties. The spatial and seasonal distributions of 54 CRISM observations containing CO2 clouds are reported, in addition to 17 new OMEGA observations. CRISM CO2 clouds are characterized by grain size in the 0.5-2\mum range and optical depths lower than 0.3. The distributions of CO2 clouds inferred from OMEGA and CRISM are consistent with each other and match at first order the distribution of high altitude (>60km) clouds derived from previous studies. At second order, discrepancies are observed. We report the identification of H2O clouds extending up to 80 km altitude, which could explain part of these discrepancies: both CO2 and H2O clouds can exist at high, mesospheric altitudes. CRISM observations of afternoon CO2 clouds display morphologies resembling terrestrial cirrus, which generalizes a previous result to the whole equatorial clouds season. Finally, we show that morning OMEGA observations have been previously misinterpreted as evidence for cumuliform, and hence potentially convective, CO2 clouds.Comment: Vincendon, M., C. Pilorget, B. Gondet, S. Murchie, and J.-P. Bibring (2011), New near-IR observations of mesospheric CO2 and H2O clouds on Mars, J. Geophys. Res., 116, E00J0

Characterization of phyllosilicates observed in the central Mawrth Vallis region, Mars, their potential formational processes, and implications for past climate

Mawrth Vallis contains one of the largest exposures of phyllosilicates on Mars. Nontronite, montmorillonite, kaolinite, and hydrated silica have been identified throughout the region using data from the Compact Reconnaissance Imaging Spectrometer for Mars (CRISM). In addition, saponite has been identified in one observation within a crater. These individual minerals are identified and distinguished by features at 1.38–1.42, ∼1.91, and 2.17–2.41 μm. There are two main phyllosilicate units in the Mawrth Vallis region. The lowermost unit is nontronite bearing, unconformably overlain by an Al-phyllosilicate unit containing montmorillonite plus hydrated silica, with a thin layer of kaolinite plus hydrated silica at the top of the unit. These two units are draped by a spectrally unremarkable capping unit. Smectites generally form in neutral to alkaline environments, while kaolinite and hydrated silica typically form in slightly acidic conditions; thus, the observed phyllosilicates may reflect a change in aqueous chemistry. Spectra retrieved near the boundary between the nontronite and Al-phyllosilicate units exhibit a strong positive slope from 1 to 2 μm, likely from a ferrous component within the rock. This ferrous component indicates either rapid deposition in an oxidizing environment or reducing conditions. Formation of each of the phyllosilicate minerals identified requires liquid water, thus indicating a regional wet period in the Noachian when these units formed. The two main phyllosilicate units may be extensive layers of altered volcanic ash. Other potential formational processes include sediment deposition into a marine or lacustrine basin or pedogenesis

Mars Express science highlights and future plans

21st EGU General Assembly, EGU2019, proceedings from the conference held 7-12 April, 2019 in Vienna, Austria, id.11100After 15 years in orbit Mars Express remains one of ESA's most scientifically productive Solar System missions whose publication record now exceeds 1200 papers. Characterization of the geological processes on a local-to-regional scale by HRSC, OMEGA and partner experiments on NASA spacecraft has allowed constraining land-forming processes in space and time. Recent results suggest episodic geological activity as well as the presence of large bodies of liquid water in several provinces (e.g. Eridania Planum, Terra Chimeria) in the early and middle Amazonian epoch and formation of vast sedimentary plains north of the Hellas basin. Mars Express observations and experimental teams provided essential contribution to the selection of the Mars-2020 landing sites. Recent discovery of subglacial liquid water underneath the Southern polar cap has proven that the mission science potential is still not exhausted. More than a decade-long record of the atmospheric parameters such as temperature, dust loading, water vapor and ozone abundance, water ice and CO2 clouds distribution, collected by SPICAM, PFS, OMEGA, HRSC and VMC together with subsequent modeling have provided key contributions to our understanding of the martian climate. Recent spectroscopic monitoring of the 2018 dust storm revealed dust properties, their spatial and temporal variations and atmospheric circulation. More than 10,000 crossings of the bow shock by Mars Express allowed ASPERA-3 to characterize complex behavior of the magnetic boundary topology as function of the solar EUV flux. Observations of the ion escape during complete solar cycle revealed important dependencies of the atmospheric erosion rate on parameters of the solar wind and EUV flux and established global energy balance between the solar wind and escaping ion flow. The observations showed that ion escape can be responsible for removal of about 10 mbar over the Mars history that implies existence of other more effective escape channels. The structure of the ionosphere sounded by the MARSIS radar and the MaRS radio science experiment was found to be significantly affected by the solar activity, the crustal magnetic field, as well as by the influx of meteorite and cometary dust. MARSIS and ASPERA-3 observations suggest that the sunlit ionosphere over the regions with strong crustal fields is denser and extends to higher altitudes as compared to the regions with no crustal anomalies. Several models of the upper atmosphere and plasma environment are being developed based on and in support of the collected experimental data. The models aim at creating user-friendly data base of plasma parameters similar to the Mars Climate Database that would be of great service to the planetary community. A significant recent achievement was the flawless transition to the >gyroless> attitude control and operations mode on the spacecraft, that would allow mitigating the onboard gyros aging and extending the mission lifetime. In November 2018 ESA's Science Programme Committee (SPC) confirmed the mission operations till the end of 2020 and notionally approved its extension till the end of 2022. The talk will give the Mars Express status, review the recent science highlights, and outline future plans focusing on synergistic science with TGO