Concept of Two-Body Problem:
In practice, there are several investigations which involve more than two bodies. For example, let a hypothetical satellite placed in orbit between the earth and mars. The earth, the sun and mars apply forces on satellite. Therefore, four bodies (Earth, Sun, Mars and satellite itself) are engaged. This is no longer a two-body problem. It is a four-body problem. Luckily, it is frequently allowable to split many-body problem in numerous two-body problems. This technique makes it feasible for approximate values of parameters involved to be computed with relative ease. For example, four-body problem given above can be split in 3 different two-body problems comprising of (a) two body problem involving the earth and the satellite only (b) two-body problem involving sun and the satellite only (c) a two-body problem involving mars and the satellite only.
When satellite is under main attraction of the earth, the two-body problem involving the earth and the satellite becomes about valid. Similar statement holds for each of the remaining two-body problems. Though, in carry-over region where earth and sun attract the satellite with the similar order of magnitude of force, three-body treatment becomes essential. Similar assertion also holds in carry-over region where mars and sun attract the satellite with about the same force. Luckily, these carry-over regions constitute only small fraction of total journey of satellite in its orbit. As a result, much calculation time is saved using this technique.
Solution to Two-Body Problem:
Let two bodies of masses m1 and m2 separated by the linear displacement r→. Newton's second law of motion defines that
F→ = d(mv→)/dt or F→ = md2r→/dt2 or md2r→/dt2 = ∑i=1kF→i
Force of attraction, F1→, on m1 is directed along vector r→. Force of attraction, F2, on m2 is in opposite direction.
By Newton's third law,
F1→ = -F2→
Also, by Newton's law of gravitation,
F1→ = Gm1m2/r2(r→/r)
Again
F2→ = -G(m1m2/r2)(r→/r)
Let vectors r1→ and r2→ be directed from some fixed reference point O to particles of masses m1 and m2, respectively.
Now,
F→ = m(d2r1→/dt2)
so that
F1→ = m1(d2r→1/dt2) and F2→ = m2(d2r→2/dt2)
Equation (1) can then be rewritten as
m1(d2r1→/dt2) = (Gm1m2/r2)(r→/r)
Equation (2) can also be rewritten as
m2(d2r2→/dt2) = (Gm1m2/r2)(r→/r)
By Adding, we get
m1(d2r2→/dt2) + m2((d2r2→/dt2)) = 0
by definition, the centre-of-mass C of the system of masses m1 and m2 is given by MR→ = m1r1→ + m2r2→ where M = m1 + m2 and R→ is the position vector of C Hence, by Eq.(8), you get
M(dR→/dt) = a→ Also by equation we get
MR→ = a→t + b→
These two relations show that centre of mass of the system moves with constant velocity (i.e., with constant speed in straight line).
Angular Momentum Integral:
Equations may be written as
d2r→/dt2 = Gm2(r→/r3) and d2r2→/dt2 = -Gm1(r→/r3) respectively
After solving equation gives
d2(r→1 - r2→)/dt2 = G(m1 + m2)(r→/r3) But from figure
r1→ - r2 = -r→ Hence d2r→/dt2 + μr→/r3 = 0
where μ = G(m1 + m2)
Taking the vector product of r→ with Equation you obtain
r→xd2r→/dt2 + μr→/r3 x r→ = 0
i.e.
Integrating, we have r→ x dr→/dt = h→ where h→ is constant vector.
Equation is angular momentum integral. Now, as h→ is constant, it should point in one direction or all values of t. Therefore, motion of one body about other should lie in plane defined by th direction of h.
Mathematical form of Kepler's Second Law:
If polar coordinates r and θ are taken in this plane velocity component along radius vector joining m1 to m2 is r^. Also, perpendicular component of radius vector is rθ^, where dot replaces d/dt.
By defining I→ and J→ as the unit vectors along and perpendicular to the radius vector, the resultant velocity r→^ becomes
r→^ = I→r. + J→rθ.
Therefore, using Equations we can easily verify each of the given steps:
r→ x dr→/dt = h→
r→ x r→^ = h→
r→ x(I→r. + J→rθ.) = h→
I→rx(I→r. + J→rθ.) = h→
(I→rxI→)r.+(I→r x J→)rθ. = h→
0 + (K→r)rθ. = h→
Thus K→r2θ. = h→
We may thus write:
r2θ. = h
Here constant h is twice the rate at which radius vector defines the area. This is mathematical form of Kepler's second law. For the circular orbit, rate of change of area may, of course, be evaluated as follows:
A = πr2
dA/dt = dA/dr x dr/dt
2πrdr/dt => 2πrr.
Energy Conservation Equation of System:
If scalar product of r→. with equation is now taken, we get
r→..d2r→/dt2 + μr→..r→/r3 = 0 i.e. r→..r→.. + μ/r3 r→..r→ = 0
This may be integrated to provide
1/2r→..r→.-μ/r = c
Here C is a constant v.
I.e., 1/2v2 - μ/r = c
Here v is velocity.
Equation is energy conservation equation of the system. Quantity C isn't the total energy of system. Though, quantity 1/2v2 is associated to kinetic energy whereas quantity -μ/r is associated to potential energy of the system.
Satellite Obits in Two-Body System:
The components of acceleration along and perpendicular to radius vector are
r.. - rθ.2 and 1/2(d/dt)(r2θ.) respectively. Equation can be written as:
I→(r.. - rθ.2) + J→[(1/r)(d/dt)(r2θ.)] + (μ/r3)(I→r) = 0
Equating coefficients of vectors, we get:
r.. - rθ.2 = -μ/r2 and (1/r)(d/dt)(rθ.2) = 0
Integration of equation provides angular momentum integral
Substituting u = 1/r and eliminating time t between equations we get:
d2u/dt2 + u = μ/h2
General solution of equation is as follows:
u = μ/h2 + Acos(θ-ω)
Here A and ω are two constants of integration. Reintroducing r in equation it becomes:
1/r = μ/h2 + Acos(θ-ω) or
r = [1/(μ/h2 + Acos(θ-ω))] or
r = [(h2/μ)/1-(Ah2/μ)cos(θ-ω)]
But, generally, polar equation of the conic section may be written as:
r = P/(1 + ecos(θ-ω)) so that p = h2/μ and e = Ah2/μ
Therefore, solution of two-body problem is a conic section. It comprises Kepler's first law as special case. Particularly, orbit of a satellite about earth is categorized by value of eccentricity e. Four cases to be remembered are:
i) For 0 < e < 1, orbit is ellipse.
ii) For e = 1, orbit is parabola.
iii) For e >1, orbit is hyperbola.
iv) For e = 0, orbit is circle
Tutorsglobe: A way to secure high grade in your curriculum (Online Tutoring)
Expand your confidence, grow study skills and improve your grades.
Since 2009, Tutorsglobe has proactively helped millions of students to get better grades in school, college or university and score well in competitive tests with live, one-on-one online tutoring.
Using an advanced developed tutoring system providing little or no wait time, the students are connected on-demand with a tutor at www.tutorsglobe.com. Students work one-on-one, in real-time with a tutor, communicating and studying using a virtual whiteboard technology. Scientific and mathematical notation, symbols, geometric figures, graphing and freehand drawing can be rendered quickly and easily in the advanced whiteboard.
Free to know our price and packages for online physics tutoring. Chat with us or submit request at [email protected]
wondering where to get the finest britain after 1688 assignment help service at low prices? get it from our qualified tutors!
Complete your assignments with PhD Number Theory Assignment Help experts and score top grades with 24x7 support at reasonable prices.
Artificial Satellite and Remote Sensing tutorial all along with the key concepts of orbit of the Earth, Satellites in Circular Orbits, Relationship between Radius and Orbital Speed, Period of Satellite, Orbital Radius of Synchronous Satellites, Remote Sensing, Preliminary Remarks, Data Collection, Processing of Remote Sensing Data
www.tutorsglobe.com offers development of software design model homework help, assignment help, case study, writing homework help, online tutoring assistance by computer science tutors.
www.tutorsglobe.com offers answering questions to theories of international trade, the principle of absolute advantage, economics assignment help - homework help by online tutors.
tutorsglobe.com mendels interpretation and explanation assignment help-homework help by online monohybrid cross tutors
the working of fan is which they do not in fact decrease the temperature of the room but because of the circulation and wind motion they result in surface cooling and provide a breezy feeling.
Direct-Current Resistivity Methods tutorial all along with the key concepts of Direct Current Resistivity Methods, Metal electrodes, Non-polarizing electrodes, Cables, Generators and transmitters, Receivers
Introduction to Bound States tutorial all along with the key concepts of Particle in an infinite potential well and the Finite Potential Well
tutorsglobe.com standard entropy assignment help-homework help by online entropy tutors
windless picture, ringing. mirror image, horizontalsync. loss, horizontal line only; sound ok, insufficient height; sound ok, vertically non linear picture; sound ok, vertical keystone effect, vertical jitter; sound ok, picture upside down; sound ok, picture rolling from top to bottom or bottom to top sound ok
Get the un-matched Electromagnetism Physics Assignment Help service from PhD experts that you need today for top grades.
a satellite telephone or also termed as sat phone is a type of mobile which connects to orbiting satellites in place of terrestrial cell sites.
tutorsglobe.com scanning electron microscope assignment help-homework help by online light and electron microscope tutors
tutorsglobe.com advantages of capitalist economy assignment help-homework help by online capitalist economy tutors
1957313
Questions Asked
3689
Tutors
1468733
Questions Answered
Start Excelling in your courses, Ask an Expert and get answers for your homework and assignments!!