Spectral characterization of analog samples in anticipation of OSIRIS-REx's arrival at Bennu: A blind test study

Icarus Elsevier 319 (2018) 701-723

Authors:

Kerri L Donaldson Hanna, DL Schrader, EA Cloutis, GD Cody, AJ King, TJ McCoy, DM Applin, JP Mann, Neil E Bowles, Brucato, HC Connolly, E Dotto, LP Keller, LF Lim, BE Clark, VE Hamilton, C Lantz, DS Lauretta, SS Russell, PF Schofield

Abstract:

We present spectral measurements of a suite of mineral mixtures and meteorites that are possible analogs for asteroid (101955) Bennu, the target asteroid for NASA's Origins, Spectral Interpretation, Resource Identification, Security, Regolith Explorer (OSIRIS-REx) mission. The sample suite, which includes anhydrous and hydrated mineral mixtures and a suite of chondritic meteorites (CM, CI, CV, CR, and L5), was chosen to characterize the spectral effects due to varying amounts of aqueous alteration and minor amounts of organic material. Our results demonstrate the utility of mineral mixtures for understanding the mixing behavior of meteoritic materials and identifying spectrally dominant species across the visible to near-infrared (VNIR) and thermal infrared (TIR) spectral ranges. Our measurements demonstrate that, even with subtle signatures in the spectra of chondritic meteorites, we can identify diagnostic features related to the minerals comprising each of the samples. Also, the complementary nature of the two spectral ranges regarding their ability to detect different mixture and meteorite components can be used to characterize analog sample compositions better. However, we observe differences in the VNIR and TIR spectra between the mineral mixtures and the meteorites. These differences likely result from (1) differences in the types and physical disposition of constituents in the mixtures versus in meteorites, (2) missing phases observed in meteorites that we did not add to the mixtures, and (3) albedo differences among the samples. In addition to the initial characterization of the analog samples, we will use these spectral measurements to test phase detection and abundance determination algorithms in anticipation of mapping Bennu's surface properties and selecting a sampling site.

MGS‐TES Spectra Suggest a Basaltic Component in the Regolith of Phobos

Journal of Geophysical Research Planets American Geophysical Union (AGU) 123:10 (2018) 2467-2484

Authors:

Timothy D Glotch, Christopher S Edwards, Mehmet Yesiltas, Katherine A Shirley, Dylan S McDougall, Alexander M Kling, Joshua L Bandfield, Christopher DK Herd

Near infrared throughput and stray light measurements of diffraction gratings for ELT-HARMONI

Proceedings of SPIE Society of Photo-optical Instrumentation Engineers 10706 (2018)

Authors:

M Rodrigues, John Capone, F Clarke, A Earle, T Foster, J Lynn, K Obrien, M Tecza, NA Thatte, I Tosh, A Hidalgo Valadez, IJ Lewis

Sensing and control of segmented mirrors with a pyramid wavefront sensor in the presence of spiders

(2018)

Authors:

Noah Schwartz, Jean-François Sauvage, Carlos Correia, Cyril Petit, Fernando Quiros-Pacheco, Thierry Fusco, Kjetil Dohlen, Kacem El Hadi, Niranjan Thatte, Fraser Clarke, Jérome Paufique, Joel Vernet

A chemical survey of exoplanets with ARIEL

Experimental Astronomy Springer 46:1 (2018) 135-209

Authors:

Giovanna Tinetti, Pierre Drossart, Paul Eccleston, Paul Hartogh, Astrid Heske, Jérémy Leconte, Giusi Micela, Marc Ollivier, Paul Eccleston, Göran Pilbratt, Ludovic Puig, Diego Turrini, Neil Bowles

Abstract:

Thousands of exoplanets have now been discovered with a huge range of masses, sizes and orbits: from rocky Earth-like planets to large gas giants grazing the surface of their host star. However, the essential nature of these exoplanets remains largely mysterious: there is no known, discernible pattern linking the presence, size, or orbital parameters of a planet to the nature of its parent star. We have little idea whether the chemistry of a planet is linked to its formation environment, or whether the type of host star drives the physics and chemistry of the planet’s birth, and evolution. The Atmospheric Remote-sensing Infrared Exoplanet Large-survey (ARIEL) has been selected by the European Space Agency as the next mediumclass science mission, M4, to address these scientific questions. ARIEL was conceived to observe a large number (~1000) of transiting planets for statistical understanding, including gas giants, Neptunes, super-Earths and Earth-size planets around a range of host star types using transit spectroscopy in the 1.25-7.8 μm spectral range and multiple narrow-band photometry in the optical. ARIEL will focus on warm and hot planets to take advantage of their well-mixed atmospheres which should show minimal condensation and sequestration of high-Z materials compared to their colder Solar System siblings. Said warm and hot atmospheres are expected to be more representative of the planetary bulk composition. Observations of these warm/hot exoplanets, and in particular of their elemental composition (especially C, O, N, S, Si), will allow the understanding of the early stages of planetary and atmospheric formation during the nebular phase and the following few million years. ARIEL will thus provide a representative picture of the chemical nature of the exoplanets and relate this directly to the type and chemical environment of the host star. ARIEL is designed as a dedicated survey mission for combined-light spectroscopy, capable of observing a large and well-defined planet sample within its 4-year mission lifetime. Transit, eclipse and phase-curve spectroscopy methods, whereby the signal from the star and planet are differentiated using knowledge of the planetary ephemerides, allow us to measure atmospheric signals from the planet at levels of 10-100 part per million (ppm) relative to the star and, given the bright nature of targets, also allows more sophisticated techniques, such as eclipse mapping, to give a deeper insight into the nature of the atmosphere. These types of observations require a stable payload and satellite platform with broad, instantaneous wavelength coverage to detect many molecular species, probe the thermal structure, identify clouds and monitor the stellar activity. The wavelength range proposed covers all the expected major atmospheric gases from e.g. H2O, CO2, CH4 NH3, HCN, H2S through to the more exotic metallic compounds, such as TiO, VO, and condensed species. Simulations of ARIEL performance in conducting exoplanet surveys have been performed – using conservative estimates of mission performance and a full model of all significant noise sources in the measurement – using a list of potential ARIEL targets that incorporates the latest available exoplanet statistics. The conclusion at the end of the Phase A study, is that ARIEL – in line with the stated mission objectives – will be able to observe about 1000 exoplanets depending on the details of the adopted survey strategy, thus confirming the feasibility of the main science objectives.