Question
Question: If a particle is thrown with a speed of v at an angle theta with its orbit around the earth while re...
If a particle is thrown with a speed of v at an angle theta with its orbit around the earth while revolving around in a radius R0 R=Radius of Earth, M mass of earth M0 mass of partile , analyse its elliptical motion mathematicall

The elliptical orbit is described by the equation r(ϕ)=1+ecos(ϕ−ϕ0)a(1−e2), where a=2GM−R0v2GMR0 is the semi-major axis, e=1+(GM)2(v2−2GM/R0)R02v2cos2θ is the eccentricity, and ϕ0 is the angle of periapsis. The initial position is at r=R0 and angle ϕ=0, with initial radial velocity vr=vsinθ and tangential velocity vt=vcosθ. The eccentricity e must be between 0 and 1 for an ellipse, which requires v2<2GM/R0.
Solution
The motion of a particle under the gravitational force of the Earth is governed by the laws of central forces. The orbit of the particle is a conic section, which is an ellipse in this case. The parameters of the elliptical orbit (semi-major axis a and eccentricity e) are determined by the initial conditions: the initial position (radius R0) and the initial velocity (speed v and angle θ with the local tangent).
Let the initial position be at radius r=R0. Let the initial velocity be v with magnitude v. The angle between the initial velocity vector and the local tangent is θ. The angle between the initial velocity vector and the initial radius vector is α=90∘−θ (assuming θ is measured towards the center) or α=90∘+θ (assuming θ is measured away from the center). Let's assume the angle between the velocity vector and the radius vector is α. Then the radial component of velocity is vr=vcosα and the tangential component is vt=vsinα. The problem states the angle is θ with the orbit (tangent). So, the tangential component is vt=vcosθ and the radial component is vr=vsinθ (assuming θ is the angle between v and the tangent, and the radial component is positive outward).
The total mechanical energy E and the angular momentum L are conserved.
Initial total energy E=21M0v2−R0GMM0.
Initial angular momentum magnitude L=∣r0×M0v0∣=R0M0vt=R0M0vcosθ.
For an elliptical orbit, the total energy E must be negative:
E<0⟹21M0v2<R0GMM0⟹v2<R02GM. This means the initial speed v must be less than the escape velocity at R0.
The parameters of the ellipse are related to E and L:
Semi-major axis a=−2EGMM0=−2(21M0v2−R0GMM0)GMM0=R02GM−v2GM=2GM−R0v2GMR0.
Eccentricity e is given by L2=GMM02a(1−e2).
(R0M0vcosθ)2=GMM022GM−R0v2GMR0(1−e2)
R02v2cos2θ=2GM−R0v2(GM)2R0(1−e2)
1−e2=(GM)2R0R02v2cos2θ(2GM−R0v2)=(GM)2R0v2cos2θ(2GM−R0v2)
e2=1−(GM)2R0v2cos2θ(2GM−R0v2).
Alternatively, e2=1+(GMM0)22EL2=1+(GMM0)22(21M0v2−R0GMM0)(R0M0vcosθ)2
e2=1+G2M2M02M0(21v2−R0GM)2R02M02v2cos2θ=1+G2M2(v2−R02GM)R02v2cos2θ
e2=1+G2M2v4R02cos2θ−R02GMG2M2R02v2cos2θ=1+G2M2v4R02cos2θ−GM2R0v2cos2θ.
The equation of the elliptical orbit in polar coordinates with the Earth at the origin is:
r(ϕ)=1+ecos(ϕ−ϕ0)a(1−e2)
where ϕ is the angle from the direction of periapsis (closest approach).
Let's set the initial position at ϕ=0. So r(0)=R0.
R0=1+ecos(−ϕ0)a(1−e2)=1+ecosϕ0a(1−e2).
We also need to determine ϕ0. The radial velocity at the initial point is vr=vsinθ.
The radial velocity in polar coordinates is r˙=dtd(1+ecos(ϕ−ϕ0)a(1−e2))=a(1−e2)(1+ecos(ϕ−ϕ0))2−1(−esin(ϕ−ϕ0))ϕ˙
r˙=(1+ecos(ϕ−ϕ0))2a(1−e2)esin(ϕ−ϕ0)ϕ˙.
Using r=1+ecos(ϕ−ϕ0)a(1−e2)⟹(1+ecos(ϕ−ϕ0))=ra(1−e2).
r˙=a(1−e2)r2esin(ϕ−ϕ0)ϕ˙.
Using conservation of angular momentum, r2ϕ˙=h=L/M0=R0vcosθ.
r˙=a(1−e2)hesin(ϕ−ϕ0).
At the initial point (ϕ=0,r=R0,r˙0=vsinθ):
vsinθ=a(1−e2)R0vcosθesin(−ϕ0)=−a(1−e2)R0vcosθesinϕ0.
R0vcosθvsinθa(1−e2)=−esinϕ0
R0tanθa(1−e2)=−esinϕ0.
From R0=1+ecosϕ0a(1−e2), we have 1+ecosϕ0=R0a(1−e2).
ecosϕ0=R0a(1−e2)−1.
We have two equations for e and ϕ0:
ecosϕ0=R0a(1−e2)−1
esinϕ0=−R0a(1−e2)tanθ
Squaring and adding gives e2=(R0a(1−e2)−1)2+(R0a(1−e2))2tan2θ.
This is consistent with the earlier expression for e2 derived from E and L.
The mathematical analysis involves calculating the parameters of the ellipse (a,e,ϕ0) from the initial conditions (R0,v,θ) using the conservation of energy and angular momentum. The equation of the orbit in polar coordinates describes the path of the particle. The position and velocity of the particle at any point on the orbit can be derived from the orbit equation.
The semi-major axis a=2GM−R0v2GMR0.
The eccentricity e=1+(GMv2−R02)1R02v2cos2θ. (Using e2=1+(GM)22Eh2 where h=L/M0)
h=R0vcosθ. E/M0=21v2−R0GM.
e2=1+(GM)22(21v2−R0GM)(R0vcosθ)2=1+(GM)2(v2−R02GM)R02v2cos2θ.
The angle of periapsis ϕ0 can be found from tanϕ0=ecosϕ0esinϕ0=R0a(1−e2)−1−R0a(1−e2)tanθ=1−a(1−e2)R0−tanθ.
We know R0=1+ecosϕ0a(1−e2), so a(1−e2)R0=1+ecosϕ01.
tanϕ0=1−1+ecosϕ01−tanθ=1+ecosϕ01+ecosϕ0−1−tanθ=ecosϕ0−tanθ(1+ecosϕ0).
This doesn't simplify nicely. Let's use the initial velocity components.
Initial radial velocity r˙0=vsinθ. Initial tangential velocity vt0=R0ϕ˙0=vcosθ.
The equation of the orbit is r(ϕ).
dϕdr=dtdrdϕdt=ϕ˙r˙.
At the initial point ϕ=0: (dϕdr)ϕ=0=ϕ˙0r˙0=vcosθ/R0vsinθ=R0tanθ.
From r(ϕ)=1+ecos(ϕ−ϕ0)C, where C=a(1−e2).
dϕdr=C(1+ecos(ϕ−ϕ0))2−1(−esin(ϕ−ϕ0))=(1+ecos(ϕ−ϕ0))2Cesin(ϕ−ϕ0).
At ϕ=0: (dϕdr)ϕ=0=(1+ecos(−ϕ0))2Cesin(−ϕ0)=(1+ecosϕ0)2−Cesinϕ0.
We know R0=1+ecosϕ0C, so 1+ecosϕ0=C/R0.
(dϕdr)ϕ=0=(C/R0)2−Cesinϕ0=C2−Cesinϕ0R02=−Cesinϕ0R02.
So, R0tanθ=−a(1−e2)esinϕ0R02.
tanθ=−a(1−e2)esinϕ0R0.
We also have R0=1+ecosϕ0a(1−e2), so a(1−e2)R0=1+ecosϕ01.
tanθ=−esinϕ01+ecosϕ01.
esinϕ0=−tanθ(1+ecosϕ0).
This is the same as the previous equation for esinϕ0.
The state of the elliptical orbit is fully described by the parameters a and e, and the orientation ϕ0. These are calculated from the initial conditions.