A New Model of the Hydrologic Properties of the Martian Crust and Implications for the Formation of Valley Networks and Outflow Channels

Mathematics – Logic

Scientific paper

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Scientific paper

Results will be discussed from a new hydrologic model for the Martian
crust, which allows for a detailed representation of the porosity,
hydraulic conductivity, and compressibility of the crust as functions of
depth and pore pressure.

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