15th APS Topical Conference on Shock Compression of Condensed Matter
Volume 52, Number 8
Sunday–Friday, June 24–29, 2007;
Kohala Coast, Hawaii
Session B3: High Energy Density Physics / Warm Dense Matter
10:30 AM–12:30 PM,
Monday, June 25, 2007
Fairmont Orchid Hotel
Room: Plaza I
Chair: Peter Celliers, Lawrence Livermore National Laboratory
Abstract ID: BAPS.2007.SHOCK.B3.3
Abstract: B3.00003 : Simulations of Shocked Hydrogen and Helium and Implications for Giant Planet Interiors
11:00 AM–11:30 AM
Preview Abstract
Abstract
Author:
Burkhard Militzer
(Carnegie Instition of Washington)
In 1996 the NOVA laser shock wave experiments at LLNL probed the
properties
of deuterium at megabar pressure for the first time. These
measurements have
triggered a large number of theoretical and experimental studies.
Recently
the combination of static and dynamic compression techniques
allowed one to
reach even higher densities. In this talk, path integral Monte
Carlo and
density functional molecular dynamics simulations have been
applied to
predict the shock states of precompressed hydrogen and helium
samples. It
will be explained why the precompression leads to a reduction in the
compression ratio for both materials [1]. It will also be
demonstrated that
electronic excitations lead to a much higher compression ratio of
5.24 for
shocked helium compared to 4.3 that our simulations predicted for
deuterium.
Combining our equation of state (EOS) results for shock samples
with further
first-principles simulation for hydrogen-helium mixtures [2]
allowed us to
build a model for the interiors of giant planets. Included were
corrections
to the commonly used linear mixing approximation as well as the
increased
stability of hydrogen molecules that arises from the presence of
helium. Our
interior models update the suite of models that were based on the
widely
used Saumon-Chabrier-Van Horn (SCVH) EOS. Deviations from SCVH
are up to
about 5 percent depending on the pressure, and thus affect
interior models
at the same level. Unlike SCVH, the computed DFT-EOS does not
predict any
first-order thermodynamic discontinuities associated with
pressure-dissociation and metallization of hydrogen [2]. We
conclude by
discussing constraints for the size of Jupiter's rocky core and
whether the
planet was formed by core accretion.
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[1] B. Militzer, ``First Principles Calculations of Shock
Compressed Fluid Helium,'' Phys. Rev. Lett. 97 (2006) 175501.
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[2] J. Vorberger, I. Tamblyn, B. Militzer, S.A. Bonev,
``Hydrogen-Helium Mixtures in the Interiors of Giant Planets,''
Phys. Rev. B 75 (2006) 024206.
To cite this abstract, use the following reference: http://meetings.aps.org/link/BAPS.2007.SHOCK.B3.3