SETI public: On the Ionisation Fraction in Protoplanetary Disks I and II

From: LARRY KLAES (ljk4_at_msn.com)
Date: Tue Sep 20 2005 - 20:12:17 UTC

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    Paper: astro-ph/0509550
    Date: Mon, 19 Sep 2005 15:54:39 GMT (230kb)

    Title: On the Ionisation Fraction in Protoplanetary Disks I: Comparing
    Different Reaction Networks

    Authors: Martin Ilgner and Richard P. Nelson

    Categories: astro-ph

    Comments: 21 pages, 23 figures, accepted for publication in A & A
    \\
    We calculate the ionisation fraction in protostellar disk models using a
    number of different chemical reaction networks, including gas-phase and
    gas-grain reaction schemes. The disk models we consider are conventional
    alpha-disks, which include viscous heating and radiative cooling. The
    primary
    source of ionisation is assumed to be X-ray irradiation from the central
    star.
    We consider a number of gas-phase chemical networks. In general we find that
    the simple models predict higher fractional ionisation levels and more
    extensive active zones than the more complex models. When heavy metal atoms
    are
    included the simple models predict that the disk is magnetically active
    throughout. The complex models predict that extensive regions of the disk
    remain magnetically uncoupled even with a fractional abundance of magnesium
    of
    10(-8). The addition of submicron sized grains with a concentration of
    10(-12)
    causes the size of the dead zone to increase dramatically for all kinetic
    models considered. We find that the simple and complex gas-grain reaction
    schemes agree on the size and structure of the resulting dead zone. We
    examine
    the effects of depleting the concentration of small grains as a crude means
    of
    modeling the growth of grains during planet formation. We find that a
    depletion
    factor of 10(-4) causes the gas-grain chemistry to converge to the gas-phase
    chemistry when heavy metals are absent. 10(-8) is required when magnesium is
    included. This suggests that efficient grain growth and settling will be
    required in protoplanetary disks, before a substantial fraction of the disk
    mass in the planet forming zone between 1 - 10 AU becomes magnetically
    active
    and turbulent.

    \\ ( http://arXiv.org/abs/astro-ph/0509550 , 230kb)

    Paper: astro-ph/0509553
    Date: Mon, 19 Sep 2005 16:37:52 GMT (72kb)

    Title: On the Ionisation Fraction in Protoplanetary Disks II: The Effect of
    Turbulent Mixing on Gas--phase Chemistry

    Authors: Martin Ilgner and Richard P. Nelson

    Categories: astro-ph

    Comments: 11 pages, 7 figures; accepted for publication in A & A
    \\
    We calculate the ionisation fraction in protostellar disk models using two
    different gas-phase chemical networks, and examine the effect of turbulent
    mixing by modelling the diffusion of chemical species vertically through the
    disk. The aim is to determine in which regions of the disk gas can couple to
    a
    magnetic field and sustain MHD turbulence. We find that the effect of
    diffusion
    depends crucially on the elemental abundance of heavy metals (magnesium)
    included in the chemical model. In the absence of heavy metals, diffusion
    has
    essentially no effect on the ionisation structure of the disks, as the
    recombination time scale is much shorter than the turbulent diffusion time
    scale. When metals are included with an elemental abundance above a
    threshold
    value, the diffusion can dramatically reduce the size of the magnetically
    decoupled region, or even remove it altogther. For a complex chemistry the
    elemental abundance of magnesium required to remove the dead zone is 10(-10)
    -
    10(-8). We also find that diffusion can modify the reaction pathways, giving
    rise to dominant species when diffusion is switched on that are minor
    species
    when diffusion is absent. This suggests that there may be chemical
    signatures
    of diffusive mixing that could be used to indirectly detect turbulent
    activity
    in protoplanetary disks. We find examples of models in which the dead zone
    in
    the outer disk region is rendered deeper when diffusion is switched on.
    Overall
    these results suggest that global MHD turbulence in protoplanetary disks may
    be
    self-sustaining under favourable circumstances, as turbulent mixing can help
    maintain the ionisation fraction above that necessary to ensure good
    coupling
    between the gas and magnetic field.

    \\ ( http://arXiv.org/abs/astro-ph/0509553 , 72kb)


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