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A comprehensive overview of gravity and gravitation, including variations in acceleration due to gravity with height and depth, gravitational field intensity, gravitational potential, and potential energy. It also covers concepts such as escape velocity, orbital velocity, and geostationary satellites. Several solved problems and exercises to reinforce understanding. It is suitable for high school students studying physics, offering a blend of theoretical explanations and practical applications to enhance their grasp of gravitational concepts. It also includes multiple choice questions.
Typology: Study notes
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Acceleration due to gravity:
The acceleration produced on a body under the influence of gravity alone is called acceleration due to gravity. It is denoted by g. The acceleration due to gravity at the surface of a planet is given by
g = 𝐺𝑀𝑅 2 , where M is mass and R is radius of the planet.
At the surface of the earth its value is found to be 9.8 m/s^2
Variation in acceleration due to gravity:
i. With height from the surface of the earth:
Consider the earth to be a sphere of mass M and radius R. The acceleration due to gravity at the surface of the earth is given by
g = 𝐺𝑀𝑅 2 ..............................(i)
Now the acceleration due to gravity at a height h from the surface of the earth is given by
g' = (^) (𝑅+ℎ)𝐺𝑀 2 ..........................(ii)
Dividing (ii) by (i), we get;
𝑔′ 𝑔 =^
𝑅^2 (𝑅+ℎ)^2
or, 𝑔
′ 𝑔 =^ (1 +^
ℎ 𝑅)
−
h
R
Expanding right hand side by using binomial theorem we get,
𝑔′ 𝑔 = 1^ –^
2ℎ 𝑅 + ... terms containing higher powers oh^
ℎ 𝑅.
For h < < R, ℎ𝑅 < < 1. So, the terms containing higher powers of (^) 𝑅ℎ can be neglected.
′ 𝑔 = 1^ –^
2ℎ 𝑅 or, ( h < < R )
This shows that the value of acceleration due to gravity goes on decreasing (g' < g) with increase in height from the surface of the earth.
ii. With depth from the surface of the earth:
Consider the earth to be a sphere of mass M and radius R. The density of the earth is given by
𝜌 = 4 𝑀 3 𝜋𝑅^3
...............................(i)
The acceleration due to gravity at the surface of the earth is given by
g = 𝐺𝑀𝑅 2 = (^) 𝑅𝐺 243 𝜋𝑅^3 𝜌
or, g = 43 𝜋𝜌𝐺𝑅 ..................................(ii)
Now the acceleration due to gravity at a depth d from the surface of the earth is only due to shaded portion of the earth of radius R-d, which is given by
g' = g (1 – 2ℎ 𝑅 )
d
R
If F be the gravitational force experienced by a mass m at any point in the gravitational field, the gravitational field intensity t that point is given by
E = (^) 𝑚𝐹 ( Its SI unit is N/kg )
Consider the earth to be a sphere of mass M and radius R. The gravitational force experienced by a mass m at a distance r from the centre of the earth is given by
F = 𝐺𝑀𝑚𝑟 2
∴ The gravitational field intensity at a distance r from the centre of the earth is given by
E = (^) 𝑚𝐹
or, E = 𝐺𝑀𝑟 2
At the surface of the earth, r = R;
∴ E = 𝐺𝑀𝑅 2
⇒ E = g
Thus gravitational field intensity is numerically equal to the acceleration due to gravity.
Gravitational Potential :
The gravitational potential at any point inside the gravitational field is defined as the amount of work done in bringing a unit mass from infinity to that point. It is a scalar quantity and denoted by V. If W be the amount of work done in bringing a mass m from infinity to any point inside the gravitational field, the gravitational potential at the point is given by
V = 𝑊𝑚 ( Its SI unit is J/kg )
m
M r
R
Expression for gravitational potential:
Consider the earth to be a sphere of mass M and radius R. Let P be a point at a distance r from the centre of the earth where the gravitational potential is to be determined. Let a unit mass is at a point at distance x from the centre of the earth. The gravitational force experienced by the unit mss t is given by
F = 𝐺𝑀𝑥 2
Now the small amount of work done in bringing the unit mass from point A to B through infinitely small distance dx is given by
dw = F dx
or dw = 𝐺𝑀𝑥 2 dx ...........................(i)
Now the total amount of work done in bringing the unit mass from infinity to point P is obtained by integrating equation (i) between the limits ∞ to r.
i.e. W = ∫∞ 𝑟𝐺𝑀𝑥 2 dx
or, W = GM∫∞ 𝑟 𝑥−2^ dx= GM [− (^1) 𝑥 ]∞𝑟^ = - GM[ (^1) 𝑟 - (^) ∞^1 ]
or, W = - 𝐺𝑀𝑟
This amount of work is called gravitational potential at P and denoted by V.
i.e. V = - 𝑮𝑴𝒓 ...............................(ii)
dx
B A P ∞
M
x
r
i.e. U = - 𝐆𝐌𝐦𝐫 ...............................(ii)
Escape Velocity:
Escape velocity is defined as the minimum velocity with which a body has to be projected vertically upward so as to escape the gravitating body.
Consider a body of mass m is projected vertically upward from the surface of the earth with velocity ve so that it can go beyond the gravitational field of the earth. Let at any instant during its upward motion, the projected mass is at point P at a distance x from the centre of the earth. The gravitational force between the earth and the projected mass at P is given by
F = 𝐺𝑀𝑚𝑥 2
Now the small amount of work done in taking the mass from point P to Q through infinitely small distance dx is given by
dw = F dx
or dw = 𝐺𝑀𝑚𝑥 2 dx ...........................(i)
Now the total amount of work done in taking the mass from the surface of the earth to infinity is obtained by integrating equation (i) between the limits R to ∞.
x
∞
P
M R
dx
i.e. W = (^) ∫𝑅 ∞𝐺𝑀𝑚𝑥 2 dx
or, W = GM𝑚 ∫𝑅 ∞ 𝑥−2^ dx = GMm [− (^) 𝑥^1 ]𝑅∞^ = - GMm [ (^) ∞^1 - (^1) 𝑅 ]
or, W = 𝐺𝑀𝑚𝑅
This amount of work is done at the cost of initially supplied kinetic energy of the body.
i.e. 12 mve^2 = 𝐺𝑀𝑚𝑅
∴ ve = √2𝐺𝑀𝑅 ................................(ii)
Also using g = 𝐺𝑀𝑅 2 ⇒ GM = gR^2 we get
ve = (^) √2𝑔𝑅 .................................(ii)
Equations (i) and (ii) are the expressions for escape velocity.
For earth, g = 9.8 m/s^2 and R = 6.4 × 10^6 m,
∴ ve = √2 × 9.8 × 6.4 × 10^6 = 11 200 m/s = 11 .2 km/s
Satellites: The heavenly bodies which revolve round the planet are called satellites. Satellite may be natural or artificial. For example moon is the natural satellite of earth. Artificial satellites are used for different purposes like weather forecasting, in telecommunications, in transmitting radio TV signals etc.
Orbital velocity and time period of a satellite:
Orbital Velocity:
The velocity of a satellite in its orbit is called orbital velocity.
m
V
r
M
Using g = 𝐺𝑀𝑅 2 ⇒ GM = gR^2 , we get
3 𝑔𝑅^2
or T = 2𝜋𝑅 √𝑟
3 𝑔
or, T = 𝟐𝝅𝑹 √(𝑹+𝒉)
𝟑 𝒈 .......................(iv)
This is the expression for time period of a satellite.
Geostationary Satllites:
The satellite which appears stationary to an observer on the earth is called geostationary satellite. The orbit of a geostationary satellite is called parking orbit or geosynchronous orbit. For a satellite to be geostationary, it must satisfy the following conditions.
i. The orbit of the satellite must lie on the equatorial plane of the earth. ii. Its period and direction of revolution must be same as the period and direction of rotation of earth about its axis.
Note:
All communication satellites are geostationary satellites The minimum number of geostationary satellites needed to be placed in a geostationary orbit for worldwide communication between any two locations must be three. The period of revolution of geostationary satellite is 24 hours. The height of geostationary satellite is 36000 km and its orbital velocity is 3.1 km/s.
Total Energy of Satellite:
A satellite revolving round the earth has both kinetic and potential energy. So, the total energy of a satellite is given by the sum of its kinetic and potential energy.
𝜔
satellite earth
Fig : Geostationary Satellite
KE of a satellite:
Consider a satellite of mass m is revolving round the earth in a circular path of radius r with orbital velocity vo. The centripetal force for the satellite to revolve round the earth is provided by the gravitational force between the earth and the satellite.
i.e. Fc = Fg
or, 𝑚vo
2 𝑟 =^
𝐺𝑀𝑚 𝑟^2 , where M is mass of the earth
or, vo = √GMr ........................(i)
Now kinetic energy of the satellite is given by
KE = 12 mvo^2
∴ KE = GMm2r .........................(ii)
PE of a satellite:
The gravitational potential energy of a satellite is given by
U = - GMmr ......................(iii)
Now the total energy of a satellite is given by the sum of its KE and PE.
i.e. E = KE + PE = GMm2r + ( - GMmr )
or, E = - 𝐆𝐌𝐦𝟐𝐫 .................(iv)
Thus the total energy of a satellite is negative. This shows that the satellite is bound to the gravitational field of the earth. The total energy required to make the satellite free from the gravitational field of the earth is given by, E = GMm2r.
Global Positioning System (GPS) :
The Global Positioning System (GPS) is the Global Navigation Satellite System (GNSS) that provides location velocity and time synchronization. It uses satellites, a receiver and algorithms to synchronize location, velocity and time data for air, sea and land travel. GPS works on any weather conditions, anywhere in the world, 24 hours a day. The GPS system is created and maintained by the United States government. It is freely accessible to anyone with a GPS receiver.
Applications of GPS:
The main applications of GPS are: i. Location : It is used for determining Position. ii. Navigation : It is used to get navigation from one place to another. iii. tracking : It is used for tracking personal or object movement. iv. Maping : It is used for creating map of the world. v. Timing : It is used to make precise time measurement.
Conceptual Questions:
2 𝑟 =^
𝐺𝑀𝑚 𝑟^2 or, vo
2 𝑟 =^
𝐺𝑀 𝑟^2 ⇒ a = g Thus the acceleration (centripetal acceleration) of a satellite is equal to the acceleration due to gravity at the position of satellite and its direction is also towards the centre of the earth. This shows that a satellite orbiting the earth is in the state of free fall.
Numerical Problems:
time period of a satellite at 100 km from the surface of the earth will be (Hint : T ∝ 𝑟
3 (^2) ) a) 0.5 hrs b) 1 hr c) 1.8 hrs d) 4 hrs
other due to gravitational force only, then the distance covered by the smaller body just before collision is (Hint: 𝑆 𝑆^12 = 𝑎 𝑎^12 & S 1 + S 2 = 9R) a) 7.5 R b) 4.5 R c) 3.5 R d) 2.5 R
a) V = √𝐺𝑀2𝑅 b) (^) 2𝑅^1 √ (^) 𝐺𝑀^1 c) 𝟏𝟐 √𝑮𝑴𝑹 d) √4𝐺𝑀𝑅
a) Infinite b) 2 mg R c) 12 mg R d) mgR
a) 8 times b) 4 times c) 𝟏𝟖 times d) 14 times