Water On Earth Brings You Here?
My Very Educated Mother Just Served
Us Nine Pies. If 2nd grade wasn’t yesterday you might have forgotten
this mnemonic device. Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus,
Neptune, (Pluto omitted)— the order of the planets moving away from the sun.
To understand how water remained on
Earth, Marcia Bjornerud pictures the three neighboring planets Venus, Earth,
and Mars. The mass of planets is generally given in yoctograms (Yg). One yoctogram is equivalent to
10^21 kilograms when mass is given relative to mass on Earth. Mars is
approximately 0.11 Yg, Earth 1 Yg, and Venus 0.88 Yg according to NASA’s
calculations. An effect of Mars being so small in mass is that it does not have
the gravitational pull to maintain an atmosphere. Venus, which is much more
similar to Earth in mass, maintains close proximity to the sun. This proximity prevents
Venus from being able to stabilize its temperature. At the beginning of
formation all three of these planets were too close to the sun to have actually
had water in the pure form, H2O. This is why scientists guess that
water resided on the planet in the form of hydrous silicate minerals we call
amphiboles.
An example of an amphibole is a form
of asbestos, Ca2Mg5Si8O22(OH)2.
General chemistry would tell you that under tremendous heat and pressure these
atoms could rearrange themselves to produce 1 molecule of water for every 8
molecules of silicon. These amphiboles are predicted to rearrange molecularly
at a depth of 60 miles beneath the surface of the Earth. This answers the
question of where Earth’s “native” water came from.
However, the answer to where water
came from does not stop at the dehydration of asbestos. Researchers conjecture
that comets supplied Earth with up to 50 percent of its water. Wherever it came
from, water is implicated in nearly EVERY geological process that takes place
on Earth above and below our surface.
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