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Fig. 9

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Modelled hemispherical emissivity εh of a regolith of grains following a power-law size distribution with p = 2.8, amax = 5 cm, and amin = 1 µm. Water ice is crystalline (Ih90) and contaminants are AmC or Th, intra-mixed with fraction f. Two estimates of the emissivity εF of the unlit B ring with the CIRS instrument on April 5, 2017, are displayed (blue dots, see text for details). Both esa (solid line) and δ-Edd (dash-dotted line) diffraction corrections are shown, assuming ξ = 0.

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