Clathrate hydrates are molecules like methane, carbon dioxide, etc, trapped in well-defined cages of water molecules forming crystalline solids.
IIT
Madras scientists have created what they call 'space fuel' by
simulating interstellar conditions in the lab, a method that may be
used to convert atmospheric CO2 into a next-generation energy
source on Earth.
The
research, published in the journal Proceedings of the National
Academy of Sciences (PNAS), could help curb greenhouse gases as well
as provide a new, sustainable source of energy.
"What
we have found is that molecules like methane and ammonia in space
could exist in a completely different form than what is known to us,"
Thalappil Pradeep of Indian Institute of Technology (IIT) Madras told
PTI.
Clathrate
hydrates are molecules like methane, carbon dioxide, etc, trapped in
well-defined cages of water molecules forming crystalline solids.
They
are formed at high pressures and low temperatures at places such as
the ocean floor, hundreds of metres below the sea level. They are
also found in glaciers such as in Siberia.
Such
hydrates especially that of methane, are thought to be the future
sources of fuel. Many nations across the world including India have
programmes to explore hydrates in the ocean bed.
IIT
Madras researchers formed such hydrates in vacuum, one thousand
billion times below the atmospheric pressure called ultra-high vacuum
(UHV) and temperature close to minus 263 degree Celsius. These are
the conditions present in deep space.
This
discovery of hydrates is highly unexpected at extremely low pressures
and ultra-cold temperatures and may have several implications for the
chemistry of such atmospheres, Pradeep said.
An
experimental UHV was specially built for such studies, which housed
several spectroscopic probes. Nanometre thin layers of ice and
methane were prepared by condensing a mixture of the gases on a
specially made single crystal of ruthenium metal.
The
ruthenium metal surface was cooled to low temperatures initially
The
formation of hydrates was studied by spectroscopy. At first, when the
gases were deposited, the spectroscopic features resembled solids of
methane and water ice.
However,
as the hydrate cage formed with methane trapped in it, the molecule
became 'free' as in the gas phase. The observed changes were compared
with theoretical simulations which confirmed the hydrate formation.
The results were verified with the hydrate formed by standard
methods.
Cages
of water are not expected to form under such conditions as the water
molecules are frozen and cannot move at very low temperatures.
"Normally,
in UHV experiments, spectroscopic changes are monitored only for
minutes, may be an hour. I thought that why not wait for days and
keep observing the changes.
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