A heavy body of mass m (shown in grey) approaching Earth with initial velocity v 0 in the absence of interaction has an aiming parameter a . At the instant of closest approach to Earth, its distance from the surface of Earth is given by
b = ( v 0 ) y G M e ⎣ ⎡ x + ( z G M e a ( v 0 ) y ) 2 − 1 ⎦ ⎤ − R e ,
where x , y , and z are positive constants.
Find x + y + z .
Details and Assumptions:
This section requires Javascript.
You are seeing this because something didn't load right. We suggest you, (a) try
refreshing the page, (b) enabling javascript if it is disabled on your browser and,
finally, (c)
loading the
non-javascript version of this page
. We're sorry about the hassle.
Nice problem, but one slight error (I was a bit puzzled but managed to get the correct answer): the denominator of the quadratic solution should be 2 v 0 2 not 2 .
Log in to reply
This means that my further calculations are wrong. Now wonder why many people got the answer wrong. Very thankful to you for pointing this mistake out.
I have made necessary corrections to the problem.
Shouldn't we include field intensity at a distance a as well? In the equation after ( 3 ) , equation will be LaTeX: 2 1 m v 0 2 − a G M e m = 2 1 m r 2 a 2 v 0 2 − r G M e m
Log in to reply
You missed an important part of the problem statement:
A heavy body of mass m (shown in grey) approaching Earth with initial velocity v 0 in the absence of interaction has an aiming parameter a .
Which indirectly tells us that the grav. field intensity at the initial case was 0.
The figure is a bit wrong.The mass will not go in a straight line path as shown in the figure .It will follow a curved path as it approaches earth.
Log in to reply
Yes. I know that. But the tool I used to make this figure wasn't fit for drawing curves of that sort.
What software do you use.
A really nice problem, that I decided to post my handwritten solution to it, even though it shares a similar approach discussed in past solutions here.
Enjoy.
Problem Loading...
Note Loading...
Set Loading...
At the instant of closest approach the particle velocity is perpendicular to the radius vector joining the center of the Earth to the particle. Thus applying law of conservation of angular momentum, we get
m v 0 a = m v ( R e + b ) .
where v is the speed of the particle at the instant of closest approach.
For the sake of calculations we'll denote R e + b as r .
So, from the above equation
v = r a v 0 . . . ( 1 )
Also applying conservation of mechanical energy, we get
2 1 m v 0 2 = 2 1 m v 2 + E . . . ( 2 )
where E denotes the field intensity of Earth at distance r from the center.
Now,
E = − r G M e m . . . ( 3 )
Substituting the value for v and E from equations ( 1 ) and ( 3 ) in equation ( 2 ) , we get
2 1 m v 0 2 ⟹ 2 1 ( r 2 a 2 v 0 2 − v 0 2 ) ⟹ 2 v 0 2 ( r 2 a 2 − r 2 ) ⟹ v 0 2 a 2 − v 0 2 r 2 ⟹ v 0 2 r 2 + 2 G M e r − v 0 2 a 2 = 2 1 m r 2 a 2 v 0 2 − r G M e m = r G M e = r G M e = 2 G M e r = 0 .
Which is a quadratic in r . Solving for r , we get
r = 2 v 0 2 − 2 G M e + 4 G 2 M e 2 + 4 v 0 4 a 2 Neglecting negative value = − v 0 2 G M e + v 0 2 G M e 1 + G 2 M e 2 v 0 4 a 2 = ( v 0 ) 2 G M e ⎣ ⎡ 1 + ( G M e a v 0 2 ) 2 − 1 ⎦ ⎤ .
As r = b + R e , therefore
b = ( v 0 ) 2 G M e ⎣ ⎡ 1 + ( G M e a ( v 0 ) 2 ) 2 − 1 ⎦ ⎤ − R e .
which gives
x = 1 y = 2 z = 1 ⟹ x + y + z = 4 .