If Earth's density were uniform, it would not necessarily result in a gravitational force that is half of its current value; the gravitational force at the surface is determined solely by the total mass and radius of the Earth. The discussion clarifies that variations in density, such as those found in the Earth's core versus its outer layers, do not affect surface gravity as long as the total mass remains constant. Mathematical models demonstrate that different density distributions can yield the same gravitational force if the overall mass and radius are unchanged. The article referenced does not support the claim that uniform density halves gravitational force. Ultimately, the key takeaway is that the Earth's gravitational force is primarily a function of its total mass and radius, irrespective of internal density variations.