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Consider the spot where you’re sitting.
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Travel backwards in time
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and it might’ve been submerged at
the bottom of a shallow sea,
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buried under miles of rock,
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or floating through a molten,
infernal landscape.
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But go back far enough—
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about 4.6 billion years,
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and you’d be in the middle of an enormous
cloud of dust and gas
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orbiting a newborn star.
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This is the setting for some of the
biggest, smallest mysteries of physics:
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the mysteries of cosmic dust bunnies.
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Seemingly empty regions
of space between stars
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actually contain clouds of gas and dust,
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usually blown there by supernovas.
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When a dense cloud reaches a certain
threshold called the Jeans mass,
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it collapses in on itself.
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The shrinking cloud rotates faster
and faster, and heats up,
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eventually becoming hot enough to burn
hydrogen in its core.
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At this point a star is born.
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As fusion begins in the new star,
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it sends out jets of gas that blow
off the top and bottom of the cloud,
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leaving behind an orbiting ring of gas
and dust called a protoplanetary disk.’
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This is a surprisingly windy place;
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eddies of gas carry particles apart,
and send them smashing into each other.
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The dust consists of tiny metal fragments,
bits of rock, and, further out, ices.
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We’ve observed thousands of these disks
in the sky,
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at various stages of development
as dust clumps together
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into larger and larger masses.
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Dust grains 100 times smaller than the
width of a human hair stick to each other
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through what’s called
the van der Waals force.
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That’s where a cloud of electrons
shifts to one side of a molecule,
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creating a negative charge on one end,
and on positive charge on the other.
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Opposites attract, but van der Waals can
only hold tiny things together.
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And there’s a problem: once dust
clusters grow to a certain size,
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the windy atmosphere of a disk should
constantly break them up
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as they crash into each other.
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The question of how they continue to grow
is the first mystery of dust bunnies.
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One theory looks to electrostatic charge
to answer this.
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Energetic gamma rays, x-rays,
and UV photons
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knock electrons off of gas
atoms within the disk,
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creating positive ions
and negative electrons.
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Electrons run into and stick to dust,
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making it negatively charged.
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Now, when the wind pushes
clusters together,
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like repels like and slows them down
as they collide.
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With gentle collisions
they won’t fragment,
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but if the repulsion is too strong,
they’ll never grow.
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One theory suggests that high energy
particles
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can knock more electrons off of some
dust clumps,
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leaving them positively charged.
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Opposites again attract,
and clusters grow rapidly.
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But before long we reach
another set of mysteries.
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We know from evidence found in meteorites
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that these fluffy dust bunnies
eventually get heated, melted
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and then cooled into solid
pellets called chondrules.
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And we have no idea how
or why that happens.
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Furthermore, once those pellets do form,
how do they stick together?
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The electrostatic forces from before
are too weak,
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and small rocks can’t be held together
by gravity either.
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Gravity increases proportionally to the
mass of the objects involved.
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That’s why you could effortlessly escape
an asteroid the size of a small mountain
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using just the force generated
by your legs.
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So if not gravity, then what?
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Perhaps it’s dust.
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A fluffy dust rim collected around the
outside of the pellets
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could act like Velcro.
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There’s evidence for this in meteors,
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where we find many chondrules surrounded
by a thin rim of very fine material–
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possibly condensed dust.
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Eventually the chondrule pellets get
cemented together inside larger rocks,
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which at about 1 kilometer across
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are finally large enough to hold
themselves together through gravity.
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They continue to collide and grow
into larger and larger bodies,
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including the planets we know today.
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Ultimately, the seeds of
everything familiar–
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the size of our planet, its position
within the solar system,
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and its elemental composition–
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were determined by an uncountably large
series of random collisions.
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Change the dust cloud just a bit,
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and perhaps the conditions wouldn’t
have been right
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for the formation of life on our planet.