Acceleration due to gravity at a depth d
Consider earth to be a homogeneous sphere of radius R and mass M with centre at O .
Let g be the value of acceleration due to gravity at a point A on the surface of earth then
g=GMr2 ........(1)
If ρ is uniform density of material of the earth, then
M=43πR3ρ
Putting value of M in equation (1) and equating it, we get:
∴g=G×43πR3ρR2=43πGRρ .......(2)
Let g′ be the acceleration due to gravity at the point B at a depth d below the surface of earth. The distance of the point B from the centre of the earth is (R–d). The earth can be supposed to be made of a smaller sphere of radius (R–d) and a spherical shell of thickness d.
The body at B is inside the spherical shell of thickness d. The force on body of mass m at B due to spherical shell is zero.
The body at B is outside the surface of smaller sphere of radius (R–d). The force on the body of mass m at B is due to smaller sphere of earth of radius (R–d) is just as if the entire mass M′ of the smaller sphere of earth is concentrated at the centre O.
∴g′=GM′(R−d)2
and M′=43π(R−d)3ρ
∴g′=G×43π(R−d)3ρ(R−d)2=43πG(R−d)ρ ........(3)
Dividing (3) by (2), we get
g′g=43πG(R−d)ρ43πGRρ=R−dR=RR−dR
∴g′=g(1−dR)
Hence, as depth increases, value of acceleration due to gravity decreases.