The diamond anvil press and multi-anvil press are scientific equipment
that re-create the high pressures found deep within and
at the center of the Earth and in other celestial bodies. They
provide scientists with indirect ways to study the conditions
and mineral phases present deep in the Earth. The diamond
anvil press is the smaller of the two and is only able to put
small amounts of material under about 100 GPa of pressure,
or roughly about the pressure found at the center of the
Earth. The multi-anvil press is a larger press and can accommodate
more material but can produce far less pressure
(about 11 GPa) compared to the diamond anvil press. The
diamond anvil press can experimentally produce greater
amounts of pressure, but the multi-anvil press is more widely
used because it can accommodate greater amounts of material
that can be studied after the experiment. Many of the diamond
and multi-anvil presses can also pass electric current
through the samples that reproduce higher temperatures
found inside the Earth.
Mineral physicists mainly use olivine, a silicate mineral,
to represent the upper mantle and also iron and nickel combinations
to represent the core in the high pressure experiments.
The diamond anvil press and the multi-anvil press
have allowed scientists to learn about how the core and the
mantle separated. They have also been used to study the
phases and stabilities of minerals at high pressure, earthquakes
that occur deep inside the Earth, and the properties of
other materials at high pressure and temperatures.














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