Pluto's haze as a surface material

Icarus Elsevier 314 (2018) 232-245

Authors:

WM Grundy, T Bertrand, RP Binzel, MW Buie, BJ Buratti, AF Cheng, JC Cook, DP Cruikshank, SL Devins, CM Dalle Ore, AM Earle, K Ennico, F Forget, P Gao, GR Gladstone, CJA Howett, DE Jennings, JA Kammer, TR Lauer, IR Linscott, CM Lisse, AW Lunsford, WB McKinnon, CB Olkin, AH Parker, S Protopapa, E Quirico, DC Reuter, B Schmitt, KN Singer, JA Spencer, SA Stern, DF Strobel, ME Summers, HA Weaver, GE Weigle, ML Wong, EF Young, LA Young, X Zhang

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