Spectral Characterization of Bennu Analogs Using PASCALE: A New Experimental Set-Up for Simulating the Near-Surface Conditions of Airless Bodies
Author
Donaldson Hanna, K.L.Bowles, N.E.
Warren, T.J.
Hamilton, V.E.
Schrader, D.L.
McCoy, T.J.
Temple, J.
Clack, A.
Calcutt, S.
Lauretta, D.S.
Affiliation
Lunar and Planetary Laboratory, University of ArizonaIssue Date
2021
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Blackwell Publishing LtdCitation
Donaldson Hanna, K. L., Bowles, N. E., Warren, T. J., Hamilton, V. E., Schrader, D. L., McCoy, T. J., ... & Lauretta, D. S. (2021). Spectral characterization of Bennu analogs using PASCALE: A new experimental set‐up for simulating the near‐surface conditions of airless bodies. Journal of Geophysical Research. Planets, 126(2).Rights
Copyright © 2020. The Authors. This is an open access article under the terms of the Creative Commons Attribution License.Collection Information
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.Abstract
We describe the capabilities, radiometric stability, and calibration of a custom vacuum environment chamber capable of simulating the near-surface conditions of airless bodies. Here we demonstrate the collection of spectral measurements of a suite of fine particulate asteroid analogs made using the Planetary Analogue Surface Chamber for Asteroid and Lunar Environments (PASCALE) under conditions like those found on Earth and on airless bodies. The sample suite includes anhydrous and hydrated physical mixtures, and chondritic meteorites (CM, CI, CV, CR, and L5) previously characterized under Earth- and asteroid-like conditions. And for the first time, we measure the terrestrial and extra-terrestrial mineral end members used in the olivine- and phyllosilicate-dominated physical mixtures under the same conditions as the mixtures and meteorites allowing us better understand how minerals combine spectrally when mixed intimately. Our measurements highlight the sensitivity of thermal infrared emissivity spectra to small amounts of low albedo materials and the composition of the sample materials. As the albedo of the sample decreases, we observe smaller differences between Earth- and asteroid-like spectra, which results from a reduced thermal gradient in the upper hundreds of microns in the sample. These spectral measurements can be compared to thermal infrared emissivity spectra of asteroid (101955) Bennu's surface in regions where similarly fine particulate materials may be observed to infer surface compositions. © 2020. The Authors.Note
Open access articleISSN
2169-9097Version
Final published versionae974a485f413a2113503eed53cd6c53
10.1029/2020JE006624
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Except where otherwise noted, this item's license is described as Copyright © 2020. The Authors. This is an open access article under the terms of the Creative Commons Attribution License.