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Mean distacne from sun, \[{{10}^{6}}\,km\] 57.9 108 150 228 778 1430 more...
Applying the law of conservation of angular momentum at perigee and apogee \[m{{v}_{p}}{{r}_{p}}=m{{v}_{a}}{{r}_{a}}\] \[\Rightarrow \] \[\frac{{{v}_{p}}}{{{v}_{a}}}=\frac{{{r}_{a}}}{{{r}_{p}}}=\frac{a+c}{a-c}=\frac{1+e}{1-e}\]     [As \[{{r}_{p}}=a-c,\,\,\,\,\,\,\,{{r}_{a}}=a+c\] and eccentricity \[e=\frac{c}{a}\]] Applying the conservation of mechanical energy at perigee and apogee \[\frac{1}{2}m{{v}_{p}}^{2}-\frac{GMm}{{{r}_{p}}}=\frac{1}{2}m{{v}_{a}}^{2}-\frac{GMm}{{{r}_{a}}}\] \[\Rightarrow \] \[{{v}_{p}}^{2}-{{v}_{a}}^{2}=2GM\,\left[ \frac{1}{{{r}_{p}}}-\frac{1}{{{r}_{a}}} \right]\] \[\Rightarrow \] \[{{v}_{a}}^{2}\,\left[ \frac{{{r}_{a}}^{2}-{{r}_{p}}^{2}}{{{r}_{p}}^{2}} \right]\,=\,\,2\,GM\,\left[ \frac{{{r}_{a}}-{{r}_{p}}}{{{r}_{a}}{{r}_{p}}} \right]\]        [As \[{{v}_{p}}=\frac{{{v}_{a}}{{r}_{a}}}{{{r}_{p}}}\]] \[\Rightarrow \] \[{{v}_{a}}^{2}=\frac{2\,GM}{{{r}_{a}}+{{r}_{p}}}\,\,\left[ \frac{{{r}_{p}}}{{{r}_{a}}} \right]\]Þ \[{{v}_{a}}^{2}=\frac{2\,GM}{a}\,\left( \frac{a-c}{a+c} \right)\,=\,\frac{GM}{a}\,\left( \frac{1-e}{1+e} \right)\] Thus the speeds of planet at apogee and perigee are \[{{v}_{a}}=\sqrt{\frac{GM}{a}\left( \frac{1-e}{1+e} \right)}\],                       \[{{v}_{p}}=\sqrt{\frac{GM}{a}\,\left( \frac{1+e}{1-e} \right)}\] Note :
  • The gravitational force is a central force so torque on planet relative to sun is always zero, hence angular momentum of a planet or satellite is always constant irrespective of shape of orbit.

Planets are large natural bodies rotating around a star in definite orbits. The planetary system of the star sun called solar system consists of nine planets, viz., Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus, Neptune and Pluto. Out of these planets Mercury is the smallest and closest to the sun and so hottest. Jupiter is largest and has maximum moons (12). Venus is closest to Earth and brightest. Kepler after a life time study, work out three empirical laws which govern the motion of these planets and are known as Kepler?s laws of planetary motion. These are, (1) The law of Orbits : Every planet moves around the sun in an elliptical orbit with sun at one of the foci. (2) The law of Area : The line joining the sun to the planet sweeps out equal areas in equal interval of time. i.e. areal velocity is constant. According to this law planet will move slowly when it is farthest from sun and more rapidly when it is nearest to sun. It is similar to law of conservation of angular momentum. Areal velocity \[=\frac{dA}{dt}=\frac{1}{2}\,\,\frac{r(vdt)}{dt}=\frac{1}{2}rv\] \[\therefore \] \[\frac{dA}{dt}=\frac{L}{2\,m}\]                            [As \[L=mvr\]; \[rv=\frac{L}{m}\]]     (3) The law of periods : The square of period of revolution \[(T)\] of any planet around sun is directly proportional to the cube of the semi-major axis of the orbit. \[{{T}^{2}}\,\propto \,{{a}^{3}}\] or \[{{T}^{2}}\propto {{\left( \frac{{{r}_{1}}+{{r}_{2}}}{2} \right)}^{3}}\] Proof :  From the figure\[AB=AF+FB\] \[2a={{r}_{1}}+{{r}_{2}}\]   \[\therefore \]\[a=\frac{{{r}_{1}}+{{r}_{2}}}{2}\]         where  a = semi-major axis \[{{r}_{1}}=\] Shortest distance of planet from sun (perigee). \[{{r}_{2}}=\] Largest distance of planet from sun (apogee). Important data  
Planet Semi-major axis \[a({{10}^{10}}\,\text{metre})\] Period T(year) \[{{T}^{2}}/{{a}^{3}}\,({{10}^{-34}}\,\,yea{{r}^{2}}/metr{{e}^{2}})\]
Mercury 5.79 0.241 more...
The minimum velocity with which a body must be projected up so as to enable it to just overcome the gravitational pull, is known as escape velocity. The work done to displace a body from the surface of earth (r = R) to infinity (\[r=\infty \]) is \[g=\frac{4}{3}\pi \rho GR\]\[=-GMm\,\left[ \frac{1}{\infty }-\frac{1}{R} \right]\] \[\Rightarrow \] \[W=\frac{GMm}{R}\] This work required to project the body so as to escape the gravitational pull is performed on the body by providing an equal amount of kinetic energy to it at the surface of the earth. If \[{{v}_{e}}\] is the required escape velocity, then kinetic energy which should be given to the body is \[\frac{1}{2}mv_{e}^{2}\] \ \[h\]Þ\[h\] \[\Rightarrow \] \[{{v}_{e}}=\sqrt{2gR}\]                  [As \[=-\frac{3}{2}\frac{GMm}{R}\]]s or \[{{v}_{e}}=\sqrt{2\times \frac{4}{3}\pi \rho GR\times R}\] \[\Rightarrow \] \[{{v}_{e}}=R\sqrt{\frac{8}{3}\pi G\rho }\] [As \[g=\frac{4}{3}\pi \rho GR\]] (i) Escape velocity is independent of the mass and direction of projection of the body. (ii) Escape velocity depends on the reference body. Greater the value of \[(M/R)\] or \[v\propto \frac{1}{\sqrt{{{r}^{n}}-1}}\] for a planet, greater will be escape velocity. (iii) For the earth as \[g=9.8m/{{s}^{2}}\] and \[R=6400\,km\] \[{{v}_{escape}}=\sqrt{2}\,\,\,{{v}_{orbital}}\] (iv) A planet will have atmosphere if the velocity of molecule in its atmosphere \[\left[ {{v}_{rms}}=\sqrt{\frac{3RT}{M}} \right]\] is lesser than escape velocity. This is why earth has atmosphere (as at earth \[v=\frac{{{v}_{e}}}{\sqrt{2}}\]) while moon has no atmosphere (as at moon \[{{v}_{rms}}>{{v}_{e}}\]) (v) If a body projected with velocity lesser than escape velocity (\[v<{{v}_{e}}\]), it will reach a certain maximum height and then may either move in an orbit around the planet or may fall down back to the planet. (vi) Maximum height attained by body : Let a projection velocity of body (mass \[m\]) is \[v\], so that it attains a maximum height \[h\]. At maximum height, the velocity of particle is zero, so kinetic energy is zero. By the law of conservation of energy Total energy at surface = Total energy at height \[h\]. \[\Rightarrow \ -\frac{GMm}{R}+\frac{1}{2}m{{v}^{2}}=-\frac{GMm}{R+h}+0\] \[\Rightarrow \] \[\frac{{{v}^{2}}}{2}=GM\,\left[ \frac{1}{R}-\frac{1}{R+h} \right]\] \[=\frac{GMh}{R(R+h)}\] \[\Rightarrow \]\[\frac{2GM}{{{v}^{2}}R}=\frac{R+h}{h}\] \[=1+\frac{R}{h}\] \[\Rightarrow \]\[h=\frac{R}{\left( \frac{2GM}{{{v}^{2}}R}-1 \right)}\] \[=\frac{R}{\frac{v_{e}^{2}}{{{v}^{2}}}-1}\]\[=R\,\,\left[ \frac{{{v}^{2}}}{v_{e}^{2}-{{v}^{2}}} \right]\]                                [As \[{{v}_{e}}=\sqrt{\frac{2GM}{R}}\] \[\therefore \] \[\frac{2GM}{R}=v_{e}^{2}\]] (vii) If a body is projected with velocity greater than escape velocity \[(v>{{v}_{e}})\] then by conservation of energy. Total energy at surface = Total energy at infinite \[\frac{1}{2}m{{v}^{2}}-\frac{GMm}{R}=\frac{1}{2}m{{({v}')}^{2}}+0\] i.e., \[{{({v}')}^{2}}={{v}^{2}}-\frac{2GM}{R}\] Þ \[v{{'}^{2}}={{v}^{2}}-v_{e}^{2}\]     [As \[\frac{2GM}{R}=v_{e}^{2}\]] \[\therefore \] \[{v}'=\sqrt{{{v}^{2}}-v_{e}^{2}}\] i.e, the body will move in interplanetary or inter stellar space with velocity \[\sqrt{{{v}^{2}}-v_{e}^{2}}\]. (viii) Energy to be given to a stationary object on the surface of earth so that its total energy becomes zero, is called escape energy. Total energy at the surface of the earth \[=KE+PE=0-\frac{GMm}{R}\] \[\therefore \] Escape energy \[=\frac{GMm}{R}\] (ix) If the escape velocity of a body is equal to the velocity of light then from such bodies nothing can escape, not even light. Such bodies are called black holes. The radius of a black hole is given as \[R=\frac{2GM}{{{C}^{2}}}\] [As \[C=\sqrt{\frac{2GM}{R}}\], where \[C\] is the velocity of light]  

If the body of mass \[m\] is moved from the surface of earth to a point at distance \[h\] above the surface of earth, then change in potential energy or work done against gravity will be \[T=2\pi \,\sqrt{\frac{{{r}^{3}}}{GM}}=2\pi \,\,\sqrt{\frac{{{r}^{3}}}{g{{R}^{2}}}}\] \[\Rightarrow \] \[W=GMm\left[ \frac{1}{R}-\frac{1}{R+h} \right]\]            [As \[{{r}_{1}}=R\] and \[v=\sqrt{\frac{GM}{r}}\]] \[\Rightarrow \] \[W=\frac{GMmh}{{{R}^{2}}\left( 1+\frac{h}{R} \right)}\]\[=\frac{mgh}{1+\frac{h}{R}}\]               [As \[\frac{GM}{{{R}^{2}}}=g\]]   (i) When the distance \[h\] is not negligible and is comparable to radius of the earth, then we will use above formula. (ii) If \[h=nR\] then \[W=mgR\left( \frac{n}{n+1} \right)\] (iii) If \[h=R\] then \[W=\frac{1}{2}mgR\] (iv) If \[h\] is very small as compared to radius of the earth then term \[h/R\] can be neglected From \[W=\frac{mgh}{1+h/R}\]\[=mgh\]                 \[\left[ \text{As }\,\,\frac{h}{R}\to 0 \right]\]  

The gravitational potential energy of a body at a point is defined as the amount of work done in bringing the body from infinity to that point against the gravitational force.              \[W=\int_{\infty }^{r}{\frac{GMm}{{{x}^{2}}}dx=-GMm\,\left[ \frac{1}{x} \right]_{\infty }^{r}}\]             \[W=-\frac{GMm}{r}\]                           This work done is stored inside the body as its gravitational potential energy             \[\therefore U=-\frac{GMm}{r}\] (i) Potential energy is a scalar quantity. (ii) Unit : Joule (iii) Dimension : \[[M{{L}^{2}}{{T}^{-2}}]\] (iv) Gravitational potential energy is always negative in the gravitational field because the force is always attractive in nature. (v) As the distance \[r\] increases, the gravitational potential energy becomes less negative i.e., it increases. (vi) If \[r=\infty \] then it becomes zero (maximum) (vii) In case of discrete distribution of masses Gravitational potential energy \[U=\sum {{u}_{i}}=-\left[ \frac{G{{m}_{1}}{{m}_{2}}}{{{r}_{12}}}+\frac{G{{m}_{2}}{{m}_{3}}}{{{r}_{23}}}+........ \right]\] (viii) If the body of mass \[m\] is moved from a point at a distance \[{{r}_{1}}\] to a point at distance \[{{r}_{2}}({{r}_{1}}>{{r}_{2}})\] then change in potential energy \[\Delta U=\int_{{{r}_{1}}}^{{{r}_{2}}}{\frac{GMm}{{{x}^{2}}}}dx=-GMm\,\left[ \frac{1}{{{r}_{2}}}-\frac{1}{{{r}_{1}}} \right]\] or \[\Delta U=GMm\,\left[ \frac{1}{{{r}_{1}}}-\frac{1}{{{r}_{2}}} \right]\] As \[{{r}_{1}}\] is greater than \[T=2\pi \,\,\sqrt{\frac{{{\left( R+h \right)}^{3}}}{g\,{{R}^{2}}}}\], the change in potential energy of the body will be negative. It means that if a body is brought closer to earth it's potential energy decreases. (ix) Relation between gravitational potential energy and potential \[U=-\frac{GMm}{r}\]\[=m\left[ \frac{-GM}{r} \right]\] \ \[=2\,\pi \,\,\sqrt{\frac{R}{g}}{{\left( 1+\frac{h}{R} \right)}^{3/2}}\] (x) Gravitational potential energy at the centre of earth relative to infinity. \[{{U}_{centre}}=m\,{{V}_{centre}}\]\[=m\left( -\frac{3}{2}\frac{GM}{R} \right)\] \[=-\frac{3}{2}\frac{GMm}{R}\] (xi) Gravitational potential energy of a body at height h from the earth surface is given by \[GM=g{{R}^{2}}\]  

(1) Potential due to uniform ring                  
At a point on its axis At the centre
\[V=-\frac{GM}{\sqrt{{{a}^{2}}+{{r}^{2}}}}\]   \[{{T}^{2}}\propto {{r}^{3}}\]
    (2) Potential due to spherical shell                    
Outside the surface r > R On the surface r = R Inside the surface r < R
\[V=\frac{-GM}{r}\] \[V=\frac{-GM}{R}\] \[V=\frac{-GM}{R}\]
    (3) Potential due to uniform solid sphere  
Outside the surface r > R On the surface r = R Inside the surface r < R
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At a point in a gravitational field potential \[V\] is defined as negative of work done per unit mass in shifting a test mass from some reference point (usually at infinity) to the given point i.e., \[V=-\frac{W}{m}\]\[=-\int{\frac{\overrightarrow{F}.d\overrightarrow{r\,}}{m}}\] \[=-\int{\overrightarrow{I\,}.d\overrightarrow{r\,}}\]              [As \[\frac{F}{m}=I\]] \[\therefore \] \[h=0\]      i.e., negative gradient of potential gives intensity of field or potential is a scalar function of position whose space derivative gives intensity. Negative sign indicates that the direction of intensity is in the direction where the potential decreases. (i) It is a scalar quantity because it is defined as work done per unit mass. (ii) Unit : Joule/kg or \[{{m}^{2}}/{{\sec }^{2}}\] (iii) Dimension : \[[{{M}^{0}}{{L}^{2}}{{T}^{-2}}]\] (iv) If the field is produced by a point mass then \[V=-\int_{{}}^{{}}{I\ dr}\]\[T=2\pi \sqrt{\frac{{{r}^{3}}}{GM}}=2\pi \sqrt{\frac{{{R}^{3}}}{g{{R}^{2}}}}=2\pi \sqrt{\frac{R}{g}}\]                    [As \[I=-\frac{GM}{{{r}^{2}}}\]] \[\therefore \] \[V=-\frac{GM}{r}+c\] [Here c = constant of integration] Assuming reference point at \[\infty \] and potential to be zero there we get \[0=-\frac{GM}{\infty }+c\,\Rightarrow c=0\] \[\therefore \]  Gravitational potential \[V=-\frac{GM}{r}\] (v) Gravitational potential difference : It is defined as the work done to move a unit mass from one point to the other in the gravitational field. The gravitational potential difference in bringing unit test mass m from point A to point B under the gravitational influence of source mass M is (vi) Potential due to large numbers of particle is given by scalar addition of all the potentials. \[V={{V}_{1}}+{{V}_{2}}+{{V}_{3}}+..........\]                   \[=-\frac{GM}{{{r}_{1}}}-\frac{GM}{{{r}_{2}}}-\frac{GM}{{{r}_{3}}}........\] \[=-G\sum\limits_{i=1}^{i=n}{\frac{{{M}_{i}}}{{{r}_{i}}}}\]  

(1) Intensity due to uniform solid sphere    
Outside the surface r > R On the surface r = R Inside the surface r < R
\[I=\frac{GM}{{{r}^{2}}}\] \[I=\frac{GM}{{{R}^{2}}}\] \[I=\frac{GMr}{{{R}^{3}}}\]
  (2) Intensity due to spherical shell    
Outside the surface r > R On the surface r = R Inside the surface r < R
\[I=\frac{GM}{{{r}^{2}}}\] \[I=\frac{GM}{{{R}^{2}}}\] I = 0
  (3) Intensity due to uniform circular ring                
At a point on its axis At the centre of the ring
\[I=\frac{GMr}{{{({{a}^{2}}+{{r}^{2}})}^{3/2}}}\] more...
The space surrounding a material body in which gravitational force of attraction can be experienced is called its gravitational field. Gravitational field intensity : The intensity of the gravitational field of a material body at any point in its field is defined as the force experienced by a unit mass (test mass) placed at that point, provided the unit mass (test mass) itself does not produce any change in the field of the body. So if a test mass \[m\] at a point in a gravitational field experiences a force \[\overrightarrow{F}\] then \[\overrightarrow{I\,}=\frac{\overrightarrow{F}}{m}\]   (i) It is a vector quantity and is always directed towards the centre of gravity of body whose gravitational field is considered. (ii) Units : Newton/kg or \[m{{s}^{2}}\] (iii) Dimension : \[[{{M}^{0}}L{{T}^{-2}}]\] (iv) If the field is produced by a point mass \[T\propto {{r}^{\frac{n+1}{2}}}\] and the test mass \[m\] is at a distance \[r\] from it then by Newton's law of gravitation \[F=\frac{GMm}{{{r}^{2}}}\], then intensity of gravitational field \[I=\frac{F}{m}=\frac{GMm/{{r}^{2}}}{m}\] \[\therefore \] \[F\propto \frac{1}{{{r}^{n}}}\] (v) As the distance \[(r)\] of test mass from the point mass \[(M)\], increases, intensity of gravitational field decreases             \[I=\frac{GM}{{{r}^{2}}}\];              \[\therefore \] \[I\propto \frac{1}{{{r}^{2}}}\]   (vi) Intensity of gravitational field \[=\frac{2\pi {{\left( {{R}^{3}} \right)}^{1/2}}}{{{\left[ G.\frac{4}{3}\pi {{R}^{3}}\rho  \right]}^{1/2}}}=\sqrt{\frac{3\pi }{G\rho }}\], when \[r=\infty \]. (vii) Intensity at a given point (P) due to the combined effect of different point masses can be calculated by vector sum of different intensities \[\overrightarrow{{{I}_{net}}}=\overrightarrow{{{I}_{1}}}+\overrightarrow{{{I}_{2}}}+\overrightarrow{{{I}_{3}}}+........\] (viii) Point of zero intensity : If two bodies A and B of different masses \[T=2\pi \sqrt{\frac{{{r}^{3}}}{GM}}=2\pi \sqrt{\frac{{{R}^{3}}}{GM}}\] and \[{{m}_{2}}\] are \[T=84.6\,\text{minute}\ \approx 1.4\ hr\] distance apart. Let \[P\] be the point of zero intensity i.e., the intensity at this point is equal and opposite due to two bodies \[A\] and \[B\] and if any test mass placed at this point it will not experience any force.               For point P, \[\overrightarrow{{{I}_{1}}}+\overrightarrow{{{I}_{2}}}=0\]   \[\Rightarrow \] \[g=9.8m/{{s}^{2}}\] By solving   \[x=\frac{\sqrt{{{m}_{1}}}\,d}{\sqrt{{{m}_{1}}}+\sqrt{{{m}_{2}}}}\] and \[(d-x)=\frac{\sqrt{{{m}_{2}}}\,\,d}{\sqrt{{{m}_{1}}}+\sqrt{{{m}_{2}}}}\] (ix) Gravitational field line is a line, straight or curved such that a unit mass placed in the field of another mass would always move along this line. Field lines for an isolated mass \[m\] are radially inwards.                (x) As \[R=6400km\] and also \[g=\frac{GM}{{{R}^{2}}}\] \[\therefore \ \ \ I=g\]        Thus the intensity of gravitational field at a point in the field is equal to acceleration of test mass placed at that point.  


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