The Ch-class asteroids: Connecting a visible taxonomic class to a 3-{\mu}m band shape
Andrew S. Rivkin, Cristina A. Thomas, Ellen S. Howell, and Joshua P., Emery

TL;DR
This study links the Ch asteroid spectral class to Pallas-type 3-μm band shapes, confirming that the 0.7-μm absorption is a reliable proxy for hydrated minerals, with 88% of observed Ch asteroids showing this connection.
Contribution
First to demonstrate a strong correlation between Ch class and Pallas-type 3-μm band shapes, confirming the 0.7-μm band as an indicator of hydrated minerals in asteroids.
Findings
88% of Ch asteroids exhibit Pallas-type 3-μm bands
The 0.7-μm band is a proxy for Pallas-type hydration signatures
Weak correlation between 2.95-μm band depth and semi-major axis
Abstract
Asteroids belonging to the Ch spectral taxonomic class are defined by the presence of an absorption near 0.7 {\mu}m, which is interpreted as due to Fe-bearing phyllosilicates. Phyllosilicates also cause strong absorptions in the 3-{\mu}m region, as do other hydrated and hydroxylated minerals and H2O ice. Over the past decade, spectral observations have revealed different 3-{\mu}m band shapes the asteroid population. Although a formal taxonomy is yet to be fully established, the "Pallas-type" spectral group is most consistent with the presence of phyllosilicates. If Ch class and Pallas type are both indicative of phyllosilicates, then all Ch-class asteroids should also be Pallas-type. In order to test this hypothesis, we obtained 42 observations of 36 Ch-class asteroids in the 2- to 4-{\mu}m spectral region. We found that 88% of the spectra have 3-{\mu}m band shapes most consistent with…
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