Jeans escape

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English

Template:Wikipedia

Etymology

Named after English physicist Sir Template:W (1877–1946), who is credited with calculating the rate of such atmospheric escape.

Noun

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  1. Template:Lb A type of atmospheric escape in which a light gas atom or molecule (typically a helium atom or hydrogen molecule) gains sufficient momentum through collision with other molecules to escape the atmosphere (and gravitational pull) of a planet.
    • 2014, Eugene F. Milone, William J. F. Wilson, Solar System Astrophysics, Springer, 2nd Edition, page 413,
      As will be seem in Sects. 11.7.2.3 and 11.7.3.2, Jeans escape of H atoms from Venus is negligible compared to other, nonthermal mechanisms, whereas Jeans escape dominates the loss of H from Mars. On both planets, Jeans escape of O, OA2 and COA2 is negligible.
    • 2017, Kevin Heng, Exoplanetary Atmospheres, Template:W, page 213,
      The simplest model of Jeans escape [112], a mechanism named after the Englishman James H. Jeans, assumes that the constituent particles of the atmosphere may be described by a Maxwell-Boltzmann distribution,
      fM=(aπ)3/2neav2,     (13.6)
      where am/2kBT, n is the number density of particles and v is the magnitude of the velocity.
    • 2021, Mark H. Thiemens, Mang Lin, 2: Discoveries of Mass Independent Isotope Effects in the Solar System, Ilya N. Bindeman, Andreas Pack (editors), Reviews in Mineralogy and Geochemistry, Volume 86: Triple Oxygen Isotope Geochemistry, Template:W, page 70,
      The hydrogen is lost from the system by diffusion and Jeans escapes.

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