A radiative transfer model of the edge-on disk d216-0939 indicates 5.4% crystalline water ice in the cold outer layers, implying outward transport of ice.
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Spatial distribution of water ice in the protoplanetary silhouette disk d216-0939
A radiative transfer model of the edge-on disk d216-0939 indicates 5.4% crystalline water ice in the cold outer layers, implying outward transport of ice.