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Early Habitability and Crustal Decarbonation of a Stagnant-Lid Venus

Honing, Dennis (författare)
Origins Ctr, Groningen, Netherlands.;Vrije Univ Amsterdam, Dept Earth & Life Sci, Amsterdam, Netherlands.
Baumeister, Philipp (författare)
Inst Planetary Res, German Aerosp Ctr DLR, Berlin, Germany.;Berlin Inst Technol, Dept Astron & Astrophys, Berlin, Germany.
Grenfell, John Lee (författare)
Inst Planetary Res, German Aerosp Ctr DLR, Berlin, Germany.
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Tosi, Nicola (författare)
Inst Planetary Res, German Aerosp Ctr DLR, Berlin, Germany.
Way, Michael J. (författare)
Uppsala universitet,Teoretisk astrofysik,NASA, Goddard Inst Space Studies, New York, NY 10025 USA.;GSFC Sellers Exoplanet Environm Collaborat, Greenbelt, MD USA.
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Origins Ctr, Groningen, Netherlands;Vrije Univ Amsterdam, Dept Earth & Life Sci, Amsterdam, Netherlands. Inst Planetary Res, German Aerosp Ctr DLR, Berlin, Germany.;Berlin Inst Technol, Dept Astron & Astrophys, Berlin, Germany. (creator_code:org_t)
American Geophysical Union (AGU), 2021
2021
Engelska.
Ingår i: Journal of Geophysical Research - Planets. - : American Geophysical Union (AGU). - 2169-9097 .- 2169-9100. ; 126:10
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • Little is known about the early evolution of Venus and a potential habitable period during the first 1 billion years. In particular, it remains unclear whether or not plate tectonics and an active carbonate-silicate cycle were present. In the presence of liquid water but without plate tectonics, weathering would have been limited to freshly produced basaltic crust, with an early carbon cycle restricted to the crust and atmosphere. With the evaporation of surface water, weathering would cease. With ongoing volcanism, carbonate sediments would be buried and sink downwards. Thereby, carbonates would heat up until they become unstable and the crust would become depleted in carbonates. With CO2 supply to the atmosphere the surface temperature rises further, the depth below which decarbonation occurs decreases, causing the release of even more CO2. We assess the habitable period of an early stagnant-lid Venus by employing a coupled interior-atmosphere evolution model accounting for CO2 degassing, weathering, carbonate burial, and crustal decarbonation. We find that if initial surface conditions allow for liquid water, weathering can keep the planet habitable for up to 900 Myr, followed by evaporation of water and rapid crustal carbonate depletion. For the atmospheric CO2 of stagnant-lid exoplanets, we predict a bimodal distribution, depending on whether or not these planets experienced a runaway greenhouse in their history. Planets with high atmospheric CO2 could be associated with crustal carbonate depletion as a consequence of a runaway greenhouse, whereas planets with low atmospheric CO2 would indicate active silicate weathering and thereby a habitable climate.

Ämnesord

NATURVETENSKAP  -- Fysik -- Astronomi, astrofysik och kosmologi (hsv//swe)
NATURAL SCIENCES  -- Physical Sciences -- Astronomy, Astrophysics and Cosmology (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geofysik (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geophysics (hsv//eng)

Nyckelord

carbon cycle
exoplanets
habitability
planetary evolution
stagnant-lid
Venus

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