Original title: Termální konvekce jako klíč k pochopení vnitřního vývoje a dynamiky velkých ledových těles
Translated title: Subsolidus thermal convection as a key to understanding volatile evolution and internal dynamics of large icy bodies
Authors: Ninneman, Brendan ; Kalousová, Klára (advisor) ; Šrámek, Ondřej (referee)
Document type: Master’s theses
Year: 2020
Language: eng
Abstract: Titan is a unique moon in the solar system as it is the only one with a thick atmo- sphere, and surface lakes and seas. Observations made by the Cassini/Huygens probe showed the potential of a subsurface ocean hidden below the outer crust made of ice. This thesis analyzes the heat transfer through the crust of Titan to understand the long term evolution of the ocean. We developed a finite element model of the heat transfer through a thickening ice crust and investigated the effect of viscosity, internal heat flux, and ammonia concentration in the ocean. While other explanations cannot be ruled out, it was found high values of viscosity and possible ammonia presence could keep the ocean liquid for long periods. 1
Keywords: internal dynamics; subsolidus thermal convection; volatile evolution

Institution: Charles University Faculties (theses) (web)
Document availability information: Available in the Charles University Digital Repository.
Original record: http://hdl.handle.net/20.500.11956/119603

Permalink: http://www.nusl.cz/ntk/nusl-416090


The record appears in these collections:
Universities and colleges > Public universities > Charles University > Charles University Faculties (theses)
Academic theses (ETDs) > Master’s theses
 Record created 2020-08-02, last modified 2022-03-04


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