Hi janvd.
It really is negligible.
Consider the scales here. 4,5 billion (10
9) years might sound like a lot of time, but the Earth is a seriously hefty lump of rock. It weighs 6*10
24kg. It takes a lot to slow down such a juggernaut.
Let's compare the densities of Earth:
5,5 * 10
6 g/m
3 (or, five and a half tons per cubic metre)
and vacuum:
3*1,5 * 10
-24 g/m
3 (or, three hydrogen atoms per cubic metre)
The Earth travels at 30 km/s through space, so each second it hits:
(∏*36*10
12 m
2) {Earth cross-section} * (3*10
7 m) {distance traveled in 1 second} * (3*1,5 * 10
-24 g/m
3) {density of vacuum} = 0,015 grams of matter.
multiply that by Earth's age:
0,015 * 4,5*10
9 {years} * 365 {
days in a year} * 24 {hours in a day} * 3600 {seconds in an hour} = 2 * 10
12 kg
Or, the Earth managed to hit some two billion tons of hydrogen during its life so far*.
Compare that to Earth's total mass: 6 000 000 000 000 billion tons.
That's 3 trillion times more.
Quite negligible, I'd say.
*that's of course assuming there has always been the same density of dust in vacuum, which is obviously not true, but is not a terribly bad approximation for this kind of calculations.
Additionally, it's worth noting that tidal effects of the Sun have much more significant effect on Earth, transferring its rotational angular momentum into its orbital angular momentum(which translates to increasing orbit radius). So overall, the Earth is actually spiralling outwards.