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CNR: Alamanacco della Scienza

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N. 8 - 15 mag 2013
ISSN 2037-4801

International info   a cura di Cecilia Migali

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Earth‘s center? Hotter than we thought

Scientists have determined the temperature near the Earth's centre to be 6.000 degrees Celsius, 1.000 degrees hotter than in a previous experiment run 20 years ago. These measurements confirm geophysical models that the temperature difference between the solid core and the mantle above, must be at least 1.500 degrees to explain why the Earth has a magnetic field. The scientists were even able to establish why the earlier experiment had produced a lower temperature figure. The results are published in 'Science'.

The research team was led by Agnès Dewaele from the French national technological research organization Cea, alongside members of the French National Center for Scientific Research Cnrs and the European Synchrotron Radiation Facility Esrf in Grenoble (France).

To generate an accurate picture of the temperature profile within the Earth's centre, scientists can look at the melting point of iron at different pressures in the laboratory, using a diamond anvil cell to compress speck-sized samples to pressures of several million atmospheres, and powerful laser beams to heat them to 4.000 or even 5.000 degrees Celsius.

"In practice, many experimental challenges have to be met as the iron sample has to be insulated thermally and also must not be allowed to chemically react with its environment", explains Agnès Dewaele from Cea. "Even if a sample reaches the extreme temperatures and pressures at the centre of the Earth, it will only do so for a matter of seconds. In this short timeframe it is extremely difficult to determine whether it has started to melt or is still solid".

This is where X-rays come into play. "We have developed a new technique where an intense beam of X-rays from the synchrotron can probe a sample and deduce whether it is solid, liquid or partially molten within as little as a second, using a process known diffraction", says Mohamed Mezouar from the Esrf, "and this is short enough to keep temperature and pressure constant, and at the same time avoid any chemical reactions".

The scientists determined experimentally the melting point of iron up to 4.800 degrees Celsius and 2.2 million atmospheres pressure, and then used an extrapolation method to determine that at 3.3 million atmospheres, the pressure at the border between liquid and solid core, the temperature would be 6.000 +/- 500 degrees. This extrapolated value could slightly change if iron undergoes an unknown phase transition between the measured and the extrapolated values.

When the scientists scanned across the area of pressures and temperatures, they observed why Reinhard Boehler, then at the Mpi for Chemistry in Mainz (Germany), had in 1993 published values about 1.000 degrees lower. Starting at 2.400 degrees, recrystallization effects appear on the surface of the iron samples, leading to dynamic changes of the solid iron's crystalline structure. The experiment 20 years ago used an optical technique to determine whether the samples were solid or molten, and it is highly probable that the observation of recrystallization at the surface was interpreted as melting.

"We are of course very satisfied that our experiment validated today's best theories on heat transfer from the Earth's core and the generation of the Earth's magnetic field. I am hopeful that in the not-so-distant future, we can reproduce in our laboratories, and investigate with synchrotron X-rays, every state of matter inside the Earth," concludes Agnès Dewaele.

Per saperne di più: - eurekalert.org/pub_releases/2013-04/esrf-tec042213.php