hint: Apparently the Tsiolkovsky rocket equation does not actually say that you can launch a conventional rocket into orbit around an arbitrarily large and massive body.
I'm looking for a number based on scaling the earth radius and maintaining the same average density. Must attain LEO, which also gets faster as the planet grows. Don Pettit's Tyranny mentioned in this nice answer is fun, but does not present enough math.
On this Earth, rockets barely work. Payloads can only be a few percent of the total mass for LEO, and less than one percent for deep space.
If we define slightly heavier Earths, say Earth1.1, Earth1.2... where the radii were 1.1, 1.2, etc. times that of Earth and the masses were 1.13, 1.23, etc. times the Earth's mass (in other words same average density, same "iron/rock ratio") what happens? Is there some point where chemical rockets simply will no longer be able to put things in space, or does the payload mass simply become ridiculously tiny? If there is a cut-off, is it different for LEO and deep space?
For our purposes, let's not explore alternative or hybrid launch systems or boost systems (such as balloons, planes, laser beams, space elevators etc.). Just stick to chemical propellant rockets.
edit: here is a guide. So for a scaling factor $f$:
$$ r = f r_{earth} $$ $$ m = f^3 m_{earth} $$ $$ g = G \frac{m}{r^2} = \frac{f^3}{f^2}g_{earth} = f g_{earth} $$ $$ H = \frac{kT}{gm_{molecule}} = f^{-1}H_{earth} $$
We catch a little break here. Assuming same surface atmosphere composition, temperature and pressure (STP), the scale height H actually decreases with increasing $f$. (If we were "world builders" we should probably increase pressure to get more oxygen needed for moving in the higher gravity, but that's a different Stack Exchange.)
As far as LEO altitude is concerned (thanks @Lex for catching that) one might define it as the same number of scale heights as would be on Earth. That's not really so useful because the density profiles of the bits of the atmosphere responsible for drag (Thermosphere and Exosphere are affected by many phenomenon, including the solar wind, and don't scale at all like the lower layers. Nonetheless for historical reasons I'll leave the following, as it is not essential to the question:
$$ h_{LEO} = h_{LEOearth} \frac{H}{H_{earth}} = f^{-1} h_{LEOearth} $$ $$ v_{LEO}=fv_{LEOearth} $$
The LEO period is independent of the size of a planet, if the average density is fixed. However, the velocity of LEO does scale with radius!