A Hydrodynamic Control of Channel Morphology in Unsaturated Regoliths on Earth and Mars

Details A Hydrodynamic Control of Channel Morphology in Unsaturated Regoliths on Earth and Mars A Hydrodynamic Control of Channel Morphology in Unsaturated Regoliths on Earth and Mars

Mar 1996

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1996lpi....27.1383w&link_type=abstract

Lunar and Planetary Science, volume 27, page 1383

Physics

Arroyo, Bernoulli Effect, Capillary Forces, Channels, Erosion

Scientific paper

Channels cut by short-lived, episodic discharge in unconsolidated,
unsaturated materials are characterized by steep-walled, flat-floored
channel morphology. Martian outflow channels and terrestrial arroyo
morphologies are attributed to the interaction of capillary forces and
the Bernoulli effect for water flow across an unsaturated regolith.

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