Findings could have implications for our understanding of distant, water-rich planets
From: University of Nevada – Las Vegas
March 18, 2022 -- UNLV
researchers have discovered a new form of ice, redefining the properties of
water at high pressures.
Solid water, or ice, is
like many other materials in that it can form different solid materials based
on variable temperature and pressure conditions, like carbon forming diamond or
graphite. However, water is exceptional in this aspect as there are at least 20
solid forms of ice known to us.
A team of scientists
working in UNLV's Nevada Extreme Conditions Lab pioneered a new method for
measuring the properties of water under high pressure. The water sample was
first squeezed between the tips of two opposite-facing diamonds -- freezing
into several jumbled ice crystals. The ice was then subjected to a
laser-heating technique that temporarily melted it before it quickly re-formed
into a powder-like collection of tiny crystals.
By incrementally
raising the pressure, and periodically blasting it with the laser beam, the
team observed the water ice make the transition from a known cubic phase,
Ice-VII, to the newly discovered intermediate, and tetragonal, phase, Ice-VIIt,
before settling into another known phase, Ice-X.
Zach Grande, a UNLV
Ph.D. student, led the work which also demonstrated that the transition to
Ice-X, when water stiffens aggressively, occurs at much lower pressures than
previously thought.
While it's unlikely
we'll find this new phase of ice anywhere on the surface of Earth, it is likely
a common ingredient within the mantle of Earth as well as in large moons and
water-rich planets outside of our solar system.
The team's findings
were reported in the March 17 issue of the journal Physical Review B.
Takeaways
The research team had
been working to understand the behavior of high-pressure water that may be
present in the interior of distant planets.
To do so, Grande and
UNLV physicist Ashkan Salamat placed a sample of water between the tips of two
round-cut diamonds known as diamond anvil cells, a standard feature in the
field of high pressure physics. Applying a little bit of force to the diamonds
enabled the researchers to recreate pressures as high as those found at the
center of the Earth.
By squeezing the water
sample between these diamonds, scientists drove the oxygen and hydrogen atoms
into a variety of different arrangements, including the newly discovered
arrangement, Ice-VIIt.
Not only did the
first-of-its-kind laser-heating technique allow scientists to observe a new
phase of water ice, but the team also found that the transition to Ice-X
occurred at pressures nearly three times lower than previously thought -- at
300,000 atmospheres instead of 1 million. This transition has been a highly
debated topic in the community for several decades.
"Zach's work has
demonstrated that this transformation to an ionic state occurs at much, much
lower pressures than ever thought before," Salamat said. "It's the
missing piece, and the most precise measurements ever on water at these
conditions."
The work also
recalibrates our understanding of the composition of exoplanets, Salamat added.
Researchers hypothesize that the Ice-VIIt phase of ice could exist in abundance
in the crust and upper mantle of expected water-rich planets outside of our
solar system, meaning they could have conditions habitable for life.
https://www.sciencedaily.com/releases/2022/03/220318170514.htm
No comments:
Post a Comment