What matters when talking about gravitational PE is the
change in PE measured from some reference point.
eurekameh said:
Gravitational Potential Energy (U) = -(GMm)/R
Note that R stands for the distance between the two masses. This formula assumes that the zero PE point is at R = infinity, when the masses are infinitely far apart.
This formula is useful near the Earth's surface. It takes the zero PE point to be wherever you set y = 0.
I need help making a connection between these two equations. For U = -(GMm)/R, it is saying that because R = radius of the Earth, an object on the surface of the Earth has a gravitational potential energy, correct?
Right. If you plug in R = Radius of Earth, it will give you the gravitational PE compared to when they were infinitely far away.
U = mgy seems to be saying otherwise because y = 0.
That formula uses y = 0 as a reference, so you can't directly compare those results.
But as I said up front, what really matters is the
change in PE. For example, if you lift the mass m from y = 0 to y = h, what's the change in gravitational PE? Using the second equation, you'll get ΔU = mgΔy = mgh.
You could use the first equation to measure that change in PE. In that case you'd need to compare the PE when the masses moved from R = Radius of Earth (Re) to R = Re + h. Like so:
ΔU = [-(GMm)/(Re + h)] - [-(GMm)/(Re)]
For values of h near the Earth's surface where h << Re, you can work it out and find that
ΔU = (GMm)/(Re)
2*h = mgh
You get the same answer either way. (If h is too big, then the value of g will vary too much, making the mgy version unusable.)