The magnetic history of ice
The findings could help us understand the history of other bodies in our
solar system

Date:
June 29, 2020
Source:
Weizmann Institute of Science
Summary:
The history of our planet has been written, among other things,
in the periodic reversal of its magnetic poles. Scientists propose
a new means of reading this historic record: in ice. Their findings
could lead to a refined probing ice cores and, in the future, might
be applied to understanding the magnetic history of other bodies
in our solar system, including Mars and Jupiter's moon Europa.



FULL STORY ==========================================================================
The history of our planet has been written, among other things, in the
periodic reversal of its magnetic poles. Scientists at the Weizmann
Institute of Science propose a new means of reading this historic
record: in ice. Their findings, which were recently reported in Earth and Planetary Science Letters, could lead to a refined probing ice cores and,
in the future, might be applied to understanding the magnetic history
of other bodies in our solar system, including Mars and Jupiter's
moon Europa.


==========================================================================
The idea for investigating a possible connection between ice and
Earth's magnetic history arose far from the source of the planet's
ice -- on the sunny isle of Corsica, where Prof. Oded Aharonson of the Institute's Earth and Planetary Sciences Department, was attending a
conference on magnetism. More specifically, the researchers there were discussing the field known as paleo- magnetism, which is mostly studied
through flakes magnetic minerals that have been trapped either in rocks
or cores drilled through ocean sediments. Such particles get aligned
with the Earth's magnetic field at the time they are trapped in place,
and even millions of years later, researchers can test their magnetic north-south alignment and understand the position of the Earth's magnetic
poles at that distant time. The latter is what gave Aharonson the idea: If small amounts of magnetic materials could be sensed in ocean sediments,
maybe they could also be found trapped in ice and measured. Some of
the ice frozen in the glaciers in places like Greenland or Alaska is
many millennia old and is layered like tree rings. Ice cores drilled
through these are investigated for signs of such things as planetary
warming or ice ages. Why not reversals in the magnetic field as well?
The first question that Aharonson and his student Yuval Grossman who
led the project had to ask was whether it was possible that the process
in which ice forms in regions near the poles could contain a detectable
record of magnetic pole reversals. These randomly-spaced reversals have occurred throughout our planet's history, fueled by the chaotic motion
of the liquid iron dynamo deep in the planet's core. In banded rock
formations and layered sediments, researchers measure the magnetic moment
-- the magnetic north-south orientations -- of the magnetic materials in
these to reveal the magnetic moment of the Earth's magnetic field at that
time. The scientists thought such magnetic particles could be found in the
dust that gets trapped, along with water ice, in glaciers and ice sheets.

The research team built an experimental setup to simulate ice formation
such as that in polar glaciers, where dust particles in the atmosphere
may even provide the nuclei around which snowflakes form. The researchers created artificial snowfall by finely grinding ice made from purified
water, adding a bit of magnetic dust, and letting it fall though a very
cold column that was exposed to a magnetic field, the latter having
an orientation controlled by the scientists. By maintaining very cold temperatures -- around 30 degrees Celsius below zero, they found they
could generate miniature "ice cores" in which the snow and dust froze
solidly into hard ice.

"If the dust is not affected by an external magnetic field, it
will settle in random directions which will cancel each other out,"
says Aharonson. "But if a portion of it gets oriented in a particular
direction right before the particles freeze in place, the net magnetic
moment will be detectible." To measure the magnetism of the "ice
cores" they had created in the lab, the Weizmann scientists took them
to Hebrew University in Jerusalem, to the lab of Prof. Ron Shaar, where
a sensitive magnetometer installed there is able to measure the very
slightest of magnetic moments. The team found a small, but definitely detectible magnetic moment that matched the magnetic fields applied to
their ice samples.

"The Earth's paleo-magnetic history has been studied from the rocky
record; reading it in ice cores could reveal additional dimensions, or
help assign accurate dates to the other findings in those cores," says Aharonson. "And we know that the surfaces of Mars and large icy moons
like Europa have been exposed to magnetic fields. It would be exciting to
look for magnetic field reversals in ice sampled from other bodies in our
solar system." "We've proved it is possible," he adds. Aharonson has even proposed a research project for a future space mission involving ice core sampling on Mars, and he hopes that this demonstration of the feasibility
of measuring such a core will advance the appeal of this proposal.


========================================================================== Story Source: Materials provided by Weizmann_Institute_of_Science. Note: Content may be edited for style and length.


========================================================================== Journal Reference:
1. Yuval Grossman, Oded Aharonson, Ron Shaar, Gunther Kletetschka.

Experimental determination of remanent magnetism of dusty ice
deposits.

Earth and Planetary Science Letters, 2020; 545: 116408 DOI:
10.1016/ j.epsl.2020.116408 ==========================================================================

Link to news story: https://www.sciencedaily.com/releases/2020/06/200629120238.htm

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