
Computer simulations strongly support new theory of Earth's core
Date: Saturday, February 09, 2008 @ 13:38:41 UTC Topic: Science
Swedish researchers present in today’s Web edition of the journal Science
evidence that their theory about the core of the earth is correct.
Among other applications, the findings may be of significance for our
understanding of the cooling down of the earth, and of the stability of
the earth’s magnetic field.
It has long been known that the inner core of
the earth, a sphere consisting of a solid mass with a radius of about
1,200 km, is mainly made up of iron. However, seismic observations have
shown that elastic waves pass more rapidly through this core in
directions that are parallel to the earth’s axis of rotation than in
directions parallel to the equator-a phenomenon that has not been
previously explained. At the high temperatures that prevail in the core
of the earth, these waves should pass at the same speed regardless of
their direction.
In the present study, scientists from Uppsala
University and KTH present an explanation for this puzzling
characteristic. The publication is part of a series of articles
published by the same research team in Nature and Science. Initially,
in 2003, they published strong theoretical proof that the earth’s core
assumes the so-called body-centered cubic crystal structure at high
temperatures-a structure that despite its high degree of symmetry
evinces a surprisingly high level of elastic anisotropy, that is, its
elastic properties are contingent on direction. This theory about the
crystal structure directly contradicted the then prevailing view, but
since then the theory has found both experimental and theoretical
support.
In this new study the researchers present
simulations of how seismic waves are reproduced in iron under the
conditions that prevail in the core of the earth, showing a difference
of about 12 percent depending on their direction-which suffices as an
explanation for the puzzling observations. First the trajectories of
movement were calculated for several million atoms in strong
interaction with each other. On this basis, the scientists were then
able to determine that the progress of the sound waves was actually
accurately described in the computer-generated model for iron under the
conditions prevailing in the core of the earth.
“We found that the body-centered cubic structure of iron is the
only structure that could correspond to the experimental observations,”
says Börje Johansson, professor of condensed-matter theory at Uppsala
University.
The earth’s heat balance, like its magnetic field, is dependent on
the amount of heat that is stored in the inner core of the earth. These
conditions, in turn, are dependent on the crystal structure of the iron
in the inner core. Previously these estimates were based on models
deriving from the hexagonal structure of iron in the inner core. The
Swedish scientists’ discovery will now entail a critical revaluation of
the cooling off of the earth and of the stability of its magnetic
field.
“This study opens new perspectives for our understanding of the
earth’s past, present, and future,” says Natalia Skorodumova, a
researcher at the Department of Physics and Materials Science.
In their studies these researchers have used models based on the
so-called density-functional theory for which Walter Kohn was awarded
the 1999 Nobel Prize. The calculations were carried out using the most
powerful parallel supercomputers in existence, in Stockholm and
Linköping.
The body-centered cubic crystal structure forms a cube with atoms
in each corner and a further atom in the middle of this cube. It is
oriented in such a way that its great diagonal is directed along the
earth’s axis of rotation, which makes it possible for the iron to
evince sound propagations with the velocities observed.
Source: Uppsala University Via: http://www.physorg.com/news121692398.html
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