STEM 699 2014 Derivation of Kepler’s Laws from Newton’s Laws Kepler’s Laws 1. A planet orbits the sun in an elliptical path with the sun at one of the foci. 2. The area swept out by a planet radially from the sun over a fixed period of time is constant. (Hence the planets vary their speed as orbit the sun; planets travel faster when they are closer to the sun.) 3. The square of the orbital period is proportional to the cube of the semimajor axis of the orbit. Newton’s Laws 1. (Newton’s Second Law) F = ma 2. (Newton’s Law of Universal Gravitation) Suppose a point of mass M is located at the origin (0, 0) and a point of mass m is located at ( x, y ) . We assume (for time being) that the point of mass M is fixed and doesn’t move. Let r denote the vector ( x, y ) , r denote the length of this vector (i.e., r x 2 y 2 ), r̂ be the unit vector in the direction of r (so r rˆ = ). Then the gravitation force that M exerts on m is given by r Mm F G 2 rˆ r where G is a universal constant, independent of M , m , and r. Putting these two equations together we get ma = G Mm GM rˆ or equivalently a = 2 rˆ 2 r r 1 or a GM r GM 3 r 2 r r r Angular Momentum of planet about the origin is conserved Suppose a point mass M is located at the origin (0, 0) and a point mass m is located at ( x, y ) . Suppose that at all times, there is a central force acting on m (i.e., a force always in the direction of r = ( x, y ) . Note r is the position of mass m relative to M. By Newton’s law of universal gravitation, gravity is such a force. Let v = r = ( x, y) be the velocity vector of m . Define the angular momentum of m2 to be L = r × mv . Then L 0 Proof. L' = (r × mv)' = (r' × mv) (r × mv') = (v × mv) (r × ma) where a is the acceleration. The first term is 0, because v × v = 0 . As for the second term, a is in the direction of r so because r × r = 0 , it is also 0. A corollary of this result is that the motion of m2 must lie in a single plane determined by the normal vector L , {c 3 | L c 0} . Areas swept out are constant (Kepler’s Second Law) The key challenge here is to express the area swept out in a given amount of time. Define r = r (cos i sin j ) . NOTE: r and are functions of time. is relative to some (arbitrary) fixed ray. Here is an elementary way to get the formula for the area swept out in a given amount of time. y Q R r(θ + Δθ) P Δθ r(θ) θ x O 2 A 1 r ( )r ( ) sin( ) 2 So A 1 sin( ) r ( )r ( ) t 2 t So A 1 sin( ) lim r ( ) r ( ) t 0 t t 0 2 t 1 2 d r 1 2 dt lim So dA 1 2 d r dt 2 dt Another way I know is to express it in polar coordinates based at the origin. Now the area swept out by m2 from time 0 to time t is given by A (t ) r d 1 2 (0) 2 Taking the derivative with respect to time we get A 12 r 2 Now taking the derivative of r = r (cos i sin j ) , we find v = r (cos i sin j ) r ( sin i cos j ) So L = v = r × mv = r (cos i sin j ) × m r (cos i sin j ) r ( sin i cos j ) mr 2 k Hence 3 A 12 r 2 L constant 2m where L denotes the magnitude of the constant angular momentum vector. Another way of approaching this is to think about the incremental area swept out as one half of the area of the parallelogram formed by r and Δr , i.e., ΔA 12 | r r | Then A 1 r 2 r t t In the limit, dA 1 L 2 r v dt 2m Conservation of Energy Prop. For an object moving in with a central force whose magnitude varies according the inverse square law, the quantity 12 mv 2 GMm is constant. r Proof. Note the dynamical variables v and r are scalars in the expression. v || v || || r || and r || r || . We are going to differentiate, and one needs to be a little careful in doing so. d 1 mv 2 GMm d 1 m || v ||2 GMm dt 2 r dt 2 || r || d 12 m(v v ) GMm1/2 dt || r r || 1 m 2(a v ) 1 GMm3/2 2 r v 2 2 || r r || m(r v ) GMm3/2 r v || r r || GM GM 3 r r3 0 r v 4 So the quantity 12 mv 2 GMm is constant. We will denote this quantity E. r Another Proof using x, y, and z coordinates. d dt 1 2 GMm mv 2 GMm d 12 m( x2 y2 z 2 ) 2 2 2 r dt x y z 12 m 2 ( xx yy zz) 12 2 2 GMm ( xx yy zz) ( x y 2 z 2 )3/2 ( x, y, z ) mx 2 GMm x, my 2 GMm y, mz 2 GMm 2 2 3/2 2 2 3/2 ( x y z ) ( x y z ) ( x y 2 z 2 )3/2 But GM x , y 2 GM y , and z 2 GM z. 2 2 3/2 2 2 3/2 (x y z ) (x y z ) ( x y 2 z 2 )3/2 So the second vector is 0 and the derivative is zero. x 2 A Derivation of Kepler’s First Law We will use the previously derived result L mr 2 k is constant. denot the length of L , i.e., L mr 2 . As usual let use L to We also need an expression for v 2 in polar coordinates: r r cos i r sin j So v dtd (r cos )i dtd (r sin ) j So v2 = v v ( dtd (r cos )) 2 ( dtd (r sin )) 2 (r cos r sin ) 2 (r sin r cos ) 2 r 2 cos 2 2rr cos sin r 2 2 sin 2 r 2 sin 2 2rr cos sin r 2 2 cos 2 r 2 r 2 2 Substituting L mr 2 and v 2 r 2 r 2 2 into the expression E 12 mv 2 GMm . r 5 z E 12 mv 2 GMm r 12 m(r 2 r 2 2 ) GMm r 2 12 mr 2 12 mr 2 L2 4 GMm r mr 2 12 mr 2 L 2 GMm r 2mr Now solve for r : 2 r 2 2 E 2GM L2 2 m r mr Notice that if we take the square root of the previous expression we get a differential equation with time as independent variable that one could solve. However we are interested in the equation of the orbit, not the equation as a function of time. We would like d or dr . dr d L d d dt mr 2 dr dr 2 E 2GM L2 dt m r m2r 2 L mr 2 d dr 2 E 2GM L2 m r m2 r 2 This is an integral one can evaluate actually using simple, if awkward, Calculus. It doesn’t look that way at first, but it really is straightforward. Notice that if you let u 1 r the integral becomes d adu b cu du 2 for some constants a¸b, c, and d. This is an arccos integral. I have left the details of evaluating in the integral in the appendix. You get 6 1 cos( 0 ) r where L2 GMm 2 and 2EL2 1 G 2 M 2 m3 We usually take θ0 = 0 because θ0 is an arbitrary angle from which we start. Kepler’s First Law Case 1. e = 0. Then L2 r GMm 2 The orbit is a circle. Now we convert to Cartesian coordinates: r er cos x 2 y 2 ex x 2 y 2 ( ex ) 2 x 2 y 2 2 2 ex e 2 x 2 x 2 (1 e 2 ) 2 ex y 2 2 We now obtain Case 2: If e = 1, the orbit is a parabola. Now assume e 1 . Complete the square to get 7 x 2 (1 e 2 ) 2 ex y 2 2 2 ex (1 e 2 ) x 2 y2 2 2 1 e 2 ex 2e2 2 2e2 2 (1 e 2 ) x 2 y 1 e 2 (1 e 2 ) 2 1 e2 e (1 e 2 ) 2 2 e 2 2 (1 e 2 ) x y 1 e2 1 e2 2 e 2 2 (1 e ) x y 1 e2 1 e2 2 2 e x y2 1 e2 2 2 2 1 (1 e 2 ) 2 1 e2 If e > 1, then this last equation is the equation for a hyperbola. If e < 1, the equation is the equation of an ellipse. Let us assume e < 1, the ellipse case, for the rest. Let a 2 2 , b2 2 1 e2 (1 e2 )2 is c where c 2 a 2 b 2 . . Then distance from the center to the ellipse to the focus c2 a 2 b2 2 (1 e 2 ) 2 2 (1 e 2 ) 2 (1 e) 2 2 (1 e 2 ) 2 e2 2 (1 e 2 ) 2 e 1 e2 So c e 1 e2 . So (0,0) is a focus of the ellipse. Note that the eccentricity of the ellipse is e c 1 e2 e. a 1 e2 8 Kepler’s Third Law The derivative of the area is a constant L . Thus over an entire closed orbit of time T 2m L T ab 2m Therefore T 2m ab L 2 m L 1 e2 1 e2 2 m 2 L (1 e2 )3/2 But L2 or L GM m GMm2 So T 2 m 2 GM m (1 e 2 )3/2 2 3/2 2 3/2 GM (1 e ) 2 a 3/2 GM Or 4 2 3 T a GM 2 9 Newton’s Correction Newton realized that mass m will pull on M as well. A more realistic analysis goes as follows. m2 r2 − r1 r2 m1 r1 m1r1 G m1m2 (r2 r1 ) | r2 r1 |3 m2 r2 G m1m2 (r2 r1 ) | r2 r1 |3 Or r1 G m2 (r2 r1 ) | r2 r1 |3 r2 G m1 (r2 r1 ) | r2 r1 |3 Subtract the first equation from the second: r2 r1 G m1 m2 (r2 r1 ) | r2 r1 |3 10 Or (r2 r1 ) G m1 m2 (r2 r1 ) | r2 r1 |3 Therefore, taking into account that the larger mass is also affected by the smaller mass, we see that the distance between bodies actually satisfies the same equation as above with M replaced by m1 m2 . This describes the motion of one body relative to the other. The corrected analysis for the relative motion r2 r1 is therefore essentially identical as the one above with M replaced by m1 m2 , so Kepler’s Third Law becomes T2 4 2 a3 G (m1 m2 ) Aside: The equation (r2 r1 ) G m1 m2 (r2 r1 ) | r2 r1 |3 can be written as m1m2 m1m2 (r2 r1 ) G (r2 r1 ) m1 m2 | r2 r1 |3 m1m2 is known as the “reduced mass” and is typically denoted by μ. So m1 m2 mm the relative motion can be described a force of magnitude G 1 2 3 (r2 r1 ) on orbiting | r2 r1 | object of mass μ, the reduced mass, i.e., The quantity (r2 r1 ) G m1m2 (r2 r1 ) | r2 r1 |3 11 Further analysis (which follows) shows for an outside observer both m1 and m1 orbit the center of mass of the system in ellipses with equal periods. The center of mass is defined to be rc m 1r1 m 2 r2 . m1 m2 By adding the two equations m1r1 G m1m2 (r2 r1 ) | r2 r1 |3 m2 r2 G m1m2 (r2 r1 ) | r2 r1 |3 we see that rc ″= 0. This means that the center of mass moves in a straight line at a constant speed. It is an inertial reference system. Now let us change coordinates so that the origin is at rc . So let r1c r1 rc and r2c r2 rc . The goal is to find the equations that r1c and r2c satisfy. First notice that r2 r1 r2c r1c , so r2c r1c satisfies exactly the same equation as r2 r1 , m m2 (r2 r1 ) namely (r2 r1 ) G 1 | r2 r1 |3 . Next notice that m1r1c m2 r2 c m1 (r1 rc ) m2 (r2 rc ) m1r1 m1rc m2 r2 m2 rc m1r m2 r2 (m1 m2 )rc m1r m2 r2 (m1 m2 ) m 1r1 m 2 r2 m1 m2 0 Also notice r1c r1 rc r1 r1 r2 m 1r1 m 2 r2 m 2 r1 m 2 r2 m2 (r1 r2 ) and so m1 m2 m1 m2 m1 m2 m1 m2 r1c . m2 12 Also r2 c r2 rc r2 m 1r1 m 2 r2 m 1r2 m 1r1 m1 (r2 r1 ) and so m1 m2 m1 m2 m1 m2 m1 m2 r2 c m1 r2 r1 So r1c'' (r1 rc )'' r'' 1 r'' c = r'' 1 =G m2 (r2 r1 ) | r2 r1 |3 G m2 m1 m2 r1c m2 G 3 m1 m2 r1c m2 m 32 r 3 1c (m1 m2 ) 2 r1c and r2 c'' (r2 rc )'' r2'' r'' c = r2'' = G G G m1 (r2 r1 ) | r2 r1 |3 m1 m1 m2 r2 c m1 3 m1 m2 r1c m 1 m 13 (m1 m2 ) 2 r2 c 3 r2 c Notice that the original set of coupled differential equations are decoupled in this reference system. 13 The conclusion is that the center of mass moves in a straight line at a constant speed and the first object moves with respect to the center of mass as if a fictitious object of mass m 32 were located at the center of mass and the second object moves with respect to (m1 m2 )2 m 13 were located at the center (m1 m2 )2 of mass. Notice that in practice you really only need to solve one equation because m1r1c m2 r2c 0 . the center of mass as if a fictitious object of mass See excellent animations at http://commons.wikimedia.org/wiki/File:Orbit1.gif 14 Appendix: Details of evaluating the integral 1 2 r d dr m 2 E 2GM L2 L m r m2 r 2 1 r2 dr 2mE 2GMm2 1 L2 L2 r r2 Complete square in the denominator 1 2 r d 2mE G 2 M 2 m 4 1 GMm 2 r L2 L4 L2 2 dr Let L2 GMm 2 d 1 r2 2mE 1 1 1 L2 2 r 2 dr Finally let 2mE 1 2 L2 2 2 so the integral becomes d 1 r2 2 1 1 2 r 2 dr Note for future reference, that 15 2mE 1 2 L2 2mE L4 1 2 2 2 2 4 L G M m 2 EL2 1 2 G 2 M 2 m3 2 EL2 1 G 2 M 2 m3 Going back to the integral: 1 2 r d dr 2 2 11 2 r 1 r2 d dr 2 1 1 1 r Let u 11 r so du 12 dr r The integral becomes: d du 1 u2 So 0 arccos(u) Or cos( 0 ) u cos( 0 ) 1 1 r cos( 0 ) 1 r 16 1 cos( 0 ) r which is the polar equation for a conic with eccentricity ε It turns out that as mentioned above, 2 1 a 2 L 2 GMm 2E 1 GMm 2 EL2 2 2 3 G M m so E GMm 2a i.e., the total energy of an object in orbit is a function only of its semi-major axis. 17