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Question: At what depth from the surface of the earth (in terms of radius of earth) the acceleration due to gr...

At what depth from the surface of the earth (in terms of radius of earth) the acceleration due to gravity will be 2g5\dfrac{2g}{5} ?
A. 25R\dfrac{2}{5}R
B. 35R\dfrac{3}{5}R
C. 425R\dfrac{4}{25}R
D. 925R\dfrac{9}{25}R

Explanation

Solution

Acceleration due to gravity or g does not remain constant above and below the surface of Earth instead it changes.
As the depth dd increases, the Earth can be thought of as being composed of a smaller sphere of radius (REd)\left( {{R}_{E}}-d \right) with a spherical shell of thickness dd and since Mass of a sphere is proportional to the cube of its Radius, so consequently, mass of the Earth decreases.
Thus the Force on the point mass decreases and so does the acceleration due to gravity at depth dd which can be formulated as g(d)=g(1dRE)g\left( d \right)=g\left( 1-\dfrac{d}{{{R}_{E}}} \right) where RE{{R}_{E}} is the Radius of Earth.
Hence, the acceleration due to gravity at depth dd can be said to decrease by a factor of (1dRE)\left( 1-\dfrac{d}{{{R}_{E}}} \right) .

Complete step-by-step answer:
Let the depth from the surface of Earth at which the acceleration due to gravity is 2g5\dfrac{2g}{5} be dd .
We know, acceleration due to gravity at depth dd ,
g(d)=g(1dRE)g\left( d \right)=g\left( 1-\dfrac{d}{{{R}_{E}}} \right)
Putting the value of g(d)=2g5g\left( d \right)=\dfrac{2g}{5} , we get
25=(1dRE)\Rightarrow \dfrac{2}{5}=\left( 1-\dfrac{d}{{{R}_{E}}} \right)
dRE=(125)\Rightarrow \dfrac{d}{{{R}_{E}}}=\left( 1-\dfrac{2}{5} \right)
dRE=35\Rightarrow \dfrac{d}{{{R}_{E}}}=\dfrac{3}{5}
d=35RE\Rightarrow d=\dfrac{3}{5}{{R}_{E}}
Therefore, the depth dd at which the acceleration due to gravity is 2g5\dfrac{2g}{5} is equal to35RE\dfrac{3}{5}{{R}_{E}}.
Hence, the correct option would be (B) 35R\dfrac{3}{5}{{R}_{{}}}

So, the correct answer is “Option B”.

Note: One is advised to must remember that just like the acceleration due to gravity decreases by a factor of (1dRE)\left( 1-\dfrac{d}{{{R}_{E}}} \right) at depth dd , it also decreases by a factor of (12hRE)\left( 1-\dfrac{2h}{{{R}_{E}}} \right) at a height h above the Surface of Earth and these changes are only subjected to Earth and not any other planet. And at the surface of Earth, gg has a stable value of 9.8ms29.8m{{s}^{-2}} .