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Magma Ocean, Water, and the Early Atmosphere of Venus

Salvador, Arnaud (författare)
No Arizona Univ, Dept Astron & Planetary Sci, Box 6010, Flagstaff, AZ 86011 USA.;Univ Arizona, Habitabil Atmospheres & Biosignatures Lab, Tucson, AZ USA.;Univ Arizona, Lunar & Planetary Lab, Tucson, AZ 85721 USA.
Avice, Guillaume (författare)
Univ Paris Cite, Inst Phys Globe Paris, CNRS, F-75005 Paris, France.
Breuer, Doris (författare)
Inst Planetary Res, DLR, D-12489 Berlin, Germany.
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Gillmann, Cédric (författare)
Swiss Fed Inst Technol, Dept Earth Sci, Geophys Fluid Dynam, Inst Geophys, Zurich, Switzerland.
Lammer, Helmut (författare)
Austrian Acad Sci, Space Res Inst, Graz, Austria.
Marcq, Emmanuel (författare)
UVSQ Univ Paris Saclay, Sorbonne Univ, LATMOS IPSL, CNRS, Guyancourt, France.
Raymond, Sean N. (författare)
CNRS, Lab Astrophys Bordeaux, Pessac, France.;Univ Bordeaux, Pessac, France.
Sakuraba, Haruka (författare)
Tokyo Inst Technol, Dept Earth & Planetary Sci, Meguro Ku, Ookayama, Tokyo 1528551, Japan.
Scherf, Manuel (författare)
Austrian Acad Sci, Space Res Inst, Graz, Austria.;Graz Univ, Inst Phys, Graz, Austria.;Tech Univ, Inst Geodesy, Graz, Austria.
Way, Michael J. (författare)
Uppsala universitet,Teoretisk astrofysik,NASA, Goddard Inst Space Studies, 2880 Broadway, New York, NY 10025 USA
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No Arizona Univ, Dept Astron & Planetary Sci, Box 6010, Flagstaff, AZ 86011 USA;Univ Arizona, Habitabil Atmospheres & Biosignatures Lab, Tucson, AZ USA.;Univ Arizona, Lunar & Planetary Lab, Tucson, AZ 85721 USA. Univ Paris Cite, Inst Phys Globe Paris, CNRS, F-75005 Paris, France. (creator_code:org_t)
Springer Nature, 2023
2023
Engelska.
Ingår i: Space Science Reviews. - : Springer Nature. - 0038-6308 .- 1572-9672. ; 219:7
  • Forskningsöversikt (refereegranskat)
Abstract Ämnesord
Stäng  
  • The current state and surface conditions of the Earth and its twin planet Venus are drastically different. Whether these differences are directly inherited from the earliest stages of planetary evolution, when the interior was molten, or arose later during the long-term evolution is still unclear. Yet, it is clear that water, its abundance, state, and distribution between the different planetary reservoirs, which are intimately related to the solidification and outgassing of the early magma ocean, are key components regarding past and present-day habitability, planetary evolution, and the different pathways leading to various surface conditions.In this chapter we start by reviewing the outcomes of the accretion sequence, with particular emphasis on the sources and timing of water delivery in light of available constraints, and the initial thermal state of Venus at the end of the main accretion. Then, we detail the processes at play during the early thermo-chemical evolution of molten terrestrial planets, and how they can affect the abundance and distribution of water within the different planetary reservoirs. Namely, we focus on the magma ocean cooling, solidification, and concurrent formation of the outgassed atmosphere. Accounting for the possible range of parameters for early Venus and based on the mechanisms and feedbacks described, we provide an overview of the likely evolutionary pathways leading to diverse surface conditions, from a temperate to a hellish early Venus. The implications of the resulting surface conditions and habitability are discussed in the context of the subsequent long-term interior and atmospheric evolution. Future research directions and observations are proposed to constrain the different scenarios in order to reconcile Venus' early evolution with its current state, while deciphering which path it followed.

Ämnesord

NATURVETENSKAP  -- Fysik -- Astronomi, astrofysik och kosmologi (hsv//swe)
NATURAL SCIENCES  -- Physical Sciences -- Astronomy, Astrophysics and Cosmology (hsv//eng)

Nyckelord

Venus
Interior evolution
Atmosphere
Degassing

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