Missing data on Earth's magnetic field is in the oven

Dec 09, 2012 by Nancy Owano weblog
Missing data on Earth’s magnetic field is in the oven
A hand-drawn picture of an earth oven, used too by the Maori. Credit: Wikipedia

(Phys.org)—A New Zealand research team hopes to retrieve missing parts of a puzzle about the Earth's magnetic field and changes to it over time. Grabbing their attention are the stones that line Maori steam ovens. They want to learn more about how those ovens may give them missing data about the magnetic field. The idea is that the cooking process generates so much heat that the magnetic minerals in these stones will realign themselves with the current field direction. Examining the stones may explain more about the Earth's magnetic behavior. The archaeological search in New Zealand is out to find sites containing the old "hangi" ovens.

Radiocarbon analysis of the charcoal left from the firewood used to light the oven may provide the date recovered with the . Dr. Gillian Turner of Victoria University, Wellington, New Zealand, recently discussed her project at the (AGU) Fall meeting. She told BBC News, "We have very good palaeomagnetic data from across the world recording field strength and direction - especially in the ." Nonetheless, the southwest Pacific is a gap that makes the global models incomplete. That is why she and her team are out looking for "good, high-resolved data from our part of the world."

To define changing directions and intensities, mathematical models require data from many points of the Earth's surface. Scientists focusing on the do so for fundamental reasons. "We use the magnetic field to navigate and it protects us from the solar wind. We still don't understand the origin of the field, but the geological record tells us that it changes its intensity on relatively short timescales and sometimes dramatically reverses its direction," she has written.

The first settlers on New Zealand were the Maori. They used steam ovens for cooking, in the form of placing hot stones, food and layers of fern fronds soaked in water into pits in the ground, then covered with soil, for several hours of cooking. They chose the stones carefully, including andesite boulders, considered ideal because fire could not crack or shatter them. Dr. Turner said they were also ideal for research purposes because they behave better magnetically.

She said by putting thermocouples in the stones the team found that the temperature got as high as 1,100C. "At that temperature, rock-forming minerals start to become plastic if not melt." A compass on top of the cooled hangi stones established that a re-magnetization had taken place.

Her team is also looking at other potential sources of information including volcanic rocks and lake sediments. Once the project is complete, Dr Turner hopes the research will help scientists to understand how the earth's magnetic field might change in the future.

Explore further: Biology trumps chemistry in open ocean

More information: www.royalsociety.org.nz/2011/10/06/turner/

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User comments : 5

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WirelessPhil
1 / 5 (4) Dec 09, 2012
I doubt this will work. When magnets or magnetic rocks are heated, like in this fire, they lose their magnetization.
Torbjorn_Larsson_OM
1 / 5 (2) Dec 09, 2012
Turner is overreaching. The magnetic field is what protects ISS LEO astronauts from the solar wind, in our case the atmosphere seems to be the sufficient protection (compare almost field less Venus).

@ WP: They did find a resulting re-magnetization. I suspect not all grains will demagnetize, too uneven temp.
Doug_Huffman
5 / 5 (4) Dec 09, 2012
I doubt this will work. When magnets or magnetic rocks are heated, like in this fire, they lose their magnetization.
That may be true, Phil. While they are hot the magnetic domains realign with what ever field is present, losing their previous alignment. In this case it is the Earth's field that is frozen into the rocks when they cool. Precisely the data sought.
Torbjorn_Larsson_OM
5 / 5 (2) Dec 09, 2012
Ah yes, thanks Doug!
Caliban
1 / 5 (2) Dec 09, 2012
Still, useless for assessing paleomagnetism further back than one to two thousand years, if that much. Probably no further back than the last time the firepit was used --say, Superbowl XLVI?

Probably have better luck using the sedimentary record.

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