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Our Moon Is No More Bone Dry
Zachary Sharp, geochemist, at the University of New Mexico and his fellow colleagues measured the moon rocks “ chlorine isotopes", or different forms of chlorine atom at a new study of Apollo moon rocks. In regard to this the chlorine is strongly attracted to hydrogen and as the magma cools and solidifies, the hydrogen and the chlorine which is present in the molten rock tends to bond from hydrogen chloride gas. It is said that on the phase of the earth , the volcanic magma contains more hydrogen than chlorine. So, which is why most of the chlorine bonds with hydrogen.
Now
because
of
nature
of
the
bond,
the
ratio
of
chlorine
isotopes
left
behind
in
the
cooling
rock
is
about
the
same
as
the
ratio
that
gets
released
as
gas.
The
moon
was
analysed
and
was
found
that
the
chlorine
isotope
values
vary
by
25
times
more
than
the
Earth's
and
the
best
way
to
explain
this
result
is
that
the
rocks,
formed
as
the
moon
cooled
4.5
billion
years
ago,
are
low
in
hydrogen.
Instead
of
becoming
mostly
hydrogen
chloride
gas,
the
chlorine
in
lunar
magma
was
free
to
bond
with
other
elements
and
form
salts
such
as
iron
chloride
and
zinc
chloride,
leading
to
a
wider
range
of
chlorine
isotopes
in
the
rock.
The study concluded that If the moon lacks hydrogen they it should lack water too.
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