Well it won't have a similar density will it? Planets compress and compact as they get heavier because their constituent atoms get squeezed ever harder by their own self gravity. Eventually the maximum radius is reached, beyond which the planet's radius gets smaller with increasing mass because the core is now degenerate matter.
Earth's uncompressed density is actually just 4.08 compared with its average density of 5.5148, so it's already somewhat compacted. To get a rough estimate of its maximum radius we have to make a few guesstimates about its composition - it's ~83.8% silicates and about 16.2% iron/nickel, by volume. By mass it's more like 67%:33%. If we approximate all the silicates by SiO2 and the core as just Fe-56, then we can roughly work out the relative numbers of the component atoms. So we'll assume the silicon has a Z = 14 and A = 28, the oxygen has a Z = 8, A = 16 and the iron Z = 26, A = 56. This ignores the lesser isotopes, but including them won't change much. We've also ignored a few other elements, but they're all close to Silicon or oxygen anyway.
So SiO2 has Z = (14 + 8 x 2)/3 = 10, and A = (28 + 16 x 2)/3 = 20 and there's M*(0.67/20) kilomoles of SiO2 and M*(0.33/56) kilomoles of Fe. In otherwords by number it's 85% SiO2 and 15% iron. Plug in the numbers and the maximum radius is 16,500 km or ~2.6 Earth radii. A pure SiO2 planet would max at ~3 Earth radii, more or less.
These are rough figures. More elaborate modelling using more detailed physics gives similar results.