Gravity of Extended Bodies

Practice

practice problem 1

Find the separation at which a degenerate star would suck the surface matter off of a companion star.

solution

r be the separation between the objects
a, b be the radius of the degenerate and companion star, respectively
ma, mb be the mass of the degenerate and companion star, respectively

Ignore any centrifugal effects and set the two gravitational forces equal to one another on the surface of the companion star.

gdegenerate star  =  gcompanion star
GMa  =  GMb
(r − b)2 b2

And now for the dirty work. Solve this apparently simple formula for the separation, r.

mab2 =  mb(r − b)2 = mbr2 − 2mbrb + mbb2
0 =  mbr2 − 2mbrb + (mb − ma)b2

The variable r is quadratic in this equation. Use the quadratic equation to solve it.

r =  + 2mbb ± √[4mb2b2 − 4mb(mb − ma)b2]
2mb

Believe it or not, this simplifies to something simple.

r = b 
1 ±   ma
mb

Additional discussion needed.

practice problem 2

Suppose that the earth was an infinite flat slab of thickness t with the same mean density as the earth. Calculate t in order that this earth has the same acceleration due to gravity at the surface.

solution

Answer it.

practice problem 3

The word nebula (plural nebulae) means cloud in latin. In astronomy, a nebula is a diffuse collection gas and dust that looks something like a cloud. Nebulae are larger than stars, but smaller than galaxies — on the order of 10-1000 solar systems in diameter. A few representative images are shown below.
Helix Nebula Rosette Nebula Horsehead Nebula
Helix Nebula
(Source: STScI)
Rosette Nebula
(Source: Unknown)
Horsehead Nebula
(Source: NOAO)

A simplified model of a nebula is a spherical collection of matter whose density varies linearly from a maximum at its center to zero at its "surface". Determine the following quantities both inside and outside such a simplified nebula in terms of its radius R, the distance from the center r, the density at the center ρ0, and fundamental constants …

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  1. density
  2. gravitational field strength
  3. gravitational potential energy per unit mass

solution

  1. A linear function can be written in the form …
     
    y = a + bx
     
    where x is the independent variable, y is the dependent variable, and a and b are constants. In our case, we should modify this into the more appropriate generic equation …
     
    ρ(r) = a + br
     
    At the center of the nebula …
         
    r = 0 & ρ(0) = ρ0
         
    and on the surface …
         
    r = R & ρ(R) = 0
         
    Substituting these values into our generic equation will give us two equations with two unknowns: a and b. This is how we will generate the equation for density inside the nebula.
                     
    ρ(0) =  a + b 0  = ρ0  ⇒  a =  ρ0

     ⇒ 
    ρ(r) = ρ0
    1−  r
    R
    ρ(R) =  a + b R  = 0  ⇒  b =  0/R
                     
    Everywhere outside the nebula, the density is zero.
     
    ρ(r) = 0
     
    When graphed, the density looks like this …
     
    [magnify]
     
  2. Start with the basic idea that at some distance r from the center of the nebula, the only matter m(r) that contributes to the gravitational field is within the sphere defined by r. Divide the nebula up into a series of infinitely thin shells of radius r, surface area r2, and thickness dr. Multiply the volume of this spherical shell by the density function, then integrate. Use the resulting expression for mass in the gravitational field formula.
            r  
    g(r) = −  Gm(r)  = −  G
    ρ(r) dV
    r2 r2
            0  
    Replace density with the function we just derived and clean it up a bit.
        r               r          
    g(r) = −  G
    ρ0 
    1−  r
     4πr2 dr = −  4πρ0G

    r2 −  r3
     dr
    r2 R r2 R
        0               0          
    Calculate the integral from the center out to the variable distance r.
                   
    g(r) = −  4πρ0G  
    r3  −  r4
    r2 3 4R
                   
    Simplify and you're done. The gravitational field inside the nebula is given by the expression …
               
    g(r) = − 4πρ0G 
    r  −  r2
    3 4R
               
    Repeat this procedure changing the limits of integration. Calculate the integral from the center (r = 0) all the way out to the edge of the nebula (r = R). The gravitational field outside the nebula is given by the expression …
            R     R            
    g(r) = −  Gm(R)  = −  G
    ρ(r) dV = −  G
    ρ0
    1−  r
     4πr2 dr
    r2 r2 r2 R
            0     0            
        R                        
    g(r) = −  4πρ0G

    r2 −  r3
     dr = −  4πρ0G  
    R3  −  R4
    r2 R r2 3 4R
        0                        
       
    g(r) = −  πρ0GR3
    3r2
       
    When graphed over the appropriate ranges, the the two expressions together look like this …
     
    [magnify]
     
  3. Integrate the field from to a position r outside the nebula. This is not too difficult.
      r   r      
    Vg(r) = −
    g(rdr = −
    −  πρ0GR3  dr = 
    −  πρ0GR3
    3r
    3r2
             
    Integrate the field from to the surface R and then again from R to a position r inside the nebula. This is a tedious procedure.
      r  
    Vg(r) = − 
     g(rdr
      R   r  
    Vg(r) = − 
     g(rdr  − 
     g(rdr
      R     Rr  
    Vg(r) = −
    −  πρ0GR3  dr  −
     − 4πρ0G 
    r  −  r2
     dr
    3r2 3 4R
        R   R   r  
    Vg(r) = −      πρ0GR3  
    1
     +    4πρ0G 
    r2  −  r3
        3 r   6 12R
              R  
    Vg(r) = −      πρ0GR3  
    1  −  1
      4πρ0G 
    r2  −  r3  −  R2  +  R3
        3 r   6 12R 6 12R
         
    Simplify at the end.
                 
    Vg(r) = −  πρ0G  
    r3  − 2r2 +2R2
    3 R
                 
    When graphed, the gravitational potential looks like this …
     
    [magnify]
     

practice problem 4

The data in the text file earth.txt gives the density of the earth at varous depths below the surface. Using data analysis software (preferably something that can do numerical integration) generate a data column for the the gravitational field strength at various depths below the surface. Remember that the value of the field is 9.8 N/kg on the surface of the earth and 0 N/kg in the center.

solution

Answer it.

  • No condition is permanent.