Literature DB >> 25774974

Methane clathrates in the solar system.

Olivier Mousis1, Eric Chassefière, Nils G Holm, Alexis Bouquet, Jack Hunter Waite, Wolf Dietrich Geppert, Sylvain Picaud, Yuri Aikawa, Mohamad Ali-Dib, Jean-Luc Charlou, Philippe Rousselot.   

Abstract

We review the reservoirs of methane clathrates that may exist in the different bodies of the Solar System. Methane was formed in the interstellar medium prior to having been embedded in the protosolar nebula gas phase. This molecule was subsequently trapped in clathrates that formed from crystalline water ice during the cooling of the disk and incorporated in this form into the building blocks of comets, icy bodies, and giant planets. Methane clathrates may play an important role in the evolution of planetary atmospheres. On Earth, the production of methane in clathrates is essentially biological, and these compounds are mostly found in permafrost regions or in the sediments of continental shelves. On Mars, methane would more likely derive from hydrothermal reactions with olivine-rich material. If they do exist, martian methane clathrates would be stable only at depth in the cryosphere and sporadically release some methane into the atmosphere via mechanisms that remain to be determined. In the case of Titan, most of its methane probably originates from the protosolar nebula, where it would have been trapped in the clathrates agglomerated by the satellite's building blocks. Methane clathrates are still believed to play an important role in the present state of Titan. Their presence is invoked in the satellite's subsurface as a means of replenishing its atmosphere with methane via outgassing episodes. The internal oceans of Enceladus and Europa also provide appropriate thermodynamic conditions that allow formation of methane clathrates. In turn, these clathrates might influence the composition of these liquid reservoirs. Finally, comets and Kuiper Belt Objects might have formed from the agglomeration of clathrates and pure ices in the nebula. The methane observed in comets would then result from the destabilization of clathrate layers in the nuclei concurrent with their approach to perihelion. Thermodynamic equilibrium calculations show that methane-rich clathrate layers may exist on Pluto as well. Key Words: Methane clathrate-Protosolar nebula-Terrestrial planets-Outer Solar System. Astrobiology 15, 308-326.

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Year:  2015        PMID: 25774974     DOI: 10.1089/ast.2014.1189

Source DB:  PubMed          Journal:  Astrobiology        ISSN: 1557-8070            Impact factor:   4.335


  5 in total

1.  Mainly on the Plane: Deep Subsurface Bacterial Proteins Bind and Alter Clathrate Structure.

Authors:  Abigail M Johnson; Dustin J E Huard; Jongchan Kim; Priyam Raut; Sheng Dai; Raquel L Lieberman; Jennifer B Glass
Journal:  Cryst Growth Des       Date:  2020-07-23       Impact factor: 4.076

2.  Salt- and gas-filled ices under planetary conditions.

Authors:  Livia E Bove; Umbertoluca Ranieri
Journal:  Philos Trans A Math Phys Eng Sci       Date:  2019-06-03       Impact factor: 4.226

3.  Methane: Fuel or Exhaust at the Emergence of Life?

Authors:  Michael J Russell; Wolfgang Nitschke
Journal:  Astrobiology       Date:  2017-09-26       Impact factor: 4.335

4.  Uptake and accommodation of water clusters by adamantane clusters in helium droplets: interplay between magic number clusters.

Authors:  Lorenz Kranabetter; Paul Martini; Norbert Gitzl; Martin Kuhn; Fatima Saleem; Bilal Rasul; Masoomeh Mahmoodi Darian; Elias Jabbour Al Maalouf; Ivan Sukuba; Alexander Kaiser; Marcelo Goulart; Diethard K Böhme; Paul Scheier
Journal:  Phys Chem Chem Phys       Date:  2018-08-22       Impact factor: 3.676

5.  Observation of methane filled hexagonal ice stable up to 150 GPa.

Authors:  Sofiane Schaack; Umbertoluca Ranieri; Philippe Depondt; Richard Gaal; Werner F Kuhs; Philippe Gillet; Fabio Finocchi; Livia E Bove
Journal:  Proc Natl Acad Sci U S A       Date:  2019-07-22       Impact factor: 11.205

  5 in total

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