10
March 2023 ESRFnews
ID15B tastes Jovian salty ices
Jupiter’s moons Europa and
Ganymede, as well as Saturn’s moons
Enceladus and Titan, are believed to
contain oceans of water under a crust
of ice. Quite how the water remains
liquid at such low temperatures
has been a mystery, however, as
spectroscopic signatures of the most
obvious antifreeze – common salt,
or sodium chloride – are absent from
the surface. Now a collaboration led
by the University of Washington in
Seattle, US, and the ESRF thinks it
has the answer, in newly discovered
salt hydrates that exist at extreme
conditions
Baptiste Journaux at the University
of Washington and colleagues
exposed salt water at low temperatures
and high pressures of 25 GPa to
Xrays at the ID15B beamline Here
Xray diffraction revealed two
previously unknown salt hydrates
that is salt crystals that trap water
within their crystalline structures
The first SC13 has one sodium
chloride molecule for every 13 water
molecules while the second SC85
which has two sodium chlorides for
every 17 water molecules, is predicted
by the researchers to be stable in the
conditions of the icy moons (PNAS
120 e2217125120). Until now,
scientists had known of only one
hydrate of sodium chloride, and it
contains much less water.
“[SC8.5] has the structure that
planetary scientists have been waiting
for to explain the mysterious surface
spectra of icy moons,” says Journaux.
“This will permit us to identify where
the best places on their surface are to
explore and eventually land and dig
to look for signs of life
Over the next two years two
missions are being launched to
study icy moons the European
Space Agencys JUpiter ICy moon
Explorer JUICE and NASAs
Europa clipper The team led by the
University of Washington and the
ESRF is planning to study other salt
species and to measure their spectral
properties in the hope that they will
be detected when these missions enter
Jupiters orbit early next decade
Thermoelectrics probed
Thermoelectrics have long been used
in specialist applications to convert
waste heat into usable electricity, but
the exact mechanism of their operation
has been unclear. Now researchers
at Université Bourgogne-Franche-
Comté in France, Oak Ridge National
Laboratory (ORNL) in Tennessee, US,
Columbia University and Brookhaven
National Laboratory in New York,
US, and the ESRF have uncovered
a detailed mechanism for one
thermoelectric, germanium telluride
(GeTe).
The team used the brilliant, high-
energy X-rays of the ESRF’s ID15A
beamline to investigate GeTe at
common operating temperatures
of around 550 °C, using the X-ray
technique known as the pair
distribution function. They
observed local structural deviations
that at first glance appeared to
represent static disorder, but turned
out, after complementary neutron
studies at ORNL, to be dynamic.
Simulations on ORNL supercomputers
confirmed the possibility of
picosecond atomic vibrations, which
disrupt heat flow and help to provide
the thermoelectric effect.
The X-ray data also revealed that
the crystal structure of GeTe is much
more rigid in some directions than
others. Theorists in the team believe
this is because the local structural
deviations reinforce chemical bonding
in those directions, favouring electrical
conductivity. They also believe that
their model is general enough to be
applied to many other thermoelectric
materials (Nat. Mater. 22 311).
“The high-energy X-rays available
at ID15 were crucial for this study, as
they allowed us to chart the real-space
atomic displacements relevant to
thermoelectricity in exquisite detail,”
says Simon Kimber, who was an ESRF
postdoc at the time of the experiments.
S K I M B E R
Above a fragment of the disordered
GeTe structure required to fit the data
The Ge sites purple must be displaced
and split from their positions
This salt
hydrate has
the structure
that planetary
scientists have
been waiting for
to explain the
mysterious
surface spectra
of icy moons
N A S A/J P L-C A L T E C H/S E T I I N S T I T U T E
Despite its very
cold temperatures,
Jupiter’s moon
Europa harbours
liquid water under
a crust of ice.