As the planets formed through the accretion of planetesimals, they
heated
due to the violence of the collisions. How violent were
these collisions? We can easily estimate the amount of energy
available. Suppose that I let a planetesimal accrete onto an object of
mass M and radius R.
As the object falls toward the planet, it gains speed (kinetic energy).
If the planetesimal starts to fall very far
from the
planet and is initially at rest,
by the
time it hits the planet, it will have accelerated to the
escape speed of
the object (hmmm?).
The escape speeds for the planets are roughly
2.6, 6.4, 6.9, 1.4, and 3.1
miles/second for
Mercury, Venus, Earth, the Moon, and Mars, respectively.
What happens to this energy when the planetesimal
hits the planet?
Because the surface of the planet is
hard,
the planetesimal comes to a halt and the energy is converted into
heat
and the planet heats up. In order to gauge whether the
heat
added to the planet is significant, we need to consider
whether the heat will melt the planet's
rocks.
For accretion onto the Earth, where the escape speed is 6.9 miles per
second,
and for a typical silicate rock, the answer is yes;
the heat released can
melt rocks. In fact, for every gram of material accreted there is
enough
energy to melt more than 100 grams of silicate rocks.
The amount of energy needed to melt silicate rocks at a one-to-one
rate is provided by accretion onto a planet where
v(esc) = 0.69 miles per second, that is,
all of the Terrestrial planets are capable melting
by the accretion of planetesimals.