Ice sublimation below artificial crusts: Results from comet simulation experiments

Dust mantles or non-volatile mineral crusts most probably exist on large parts of the surface of many cometary nuclei. Even when such a layer is only a few millimetres thick and porous, its existence reduces substantially the gas emission rate of the underlying ice. In the present paper we report th...

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Veröffentlicht in:Planetary and space science 1991-03, Vol.39 (3), p.515-524
Hauptverfasser: Kömle, Norbert I., Steiner, Gerhard, Dankert, Carl, Dettleff, Georg, Hellmann, Harald, Kochan, Hermann, Baguhl, Michael, Kohl, Harald, Kölzer, Gabriele, Thiel, Klaus, Öhler, Achim
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