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Material Type: Notes; Professor: Bromley; Subject: Physics; University: San Diego State University; Term: Fall 2007;
Typology: Study notes
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The Kepler Problem (Section 3.8)
Hohmann Transfer
Parabolic motion
e = 1
Hyperbolic motion
e >
Intro to Scattering (Section 3.10)
Requires two velocity changes for planet transfer
which is the most energy efficient way to do so!
ℓ 3
mk
2 ∫ θ θ 0
dθ
(1+
e (^) cos(
θ − θ ))′ 2
eg. For Parabola’s
e = 1)
use
1 + cos
(^) θ
= 2 cos
2 (^) (
2 θ^ )
3
mk
2 ∫
θ
0
sec
4 (
2 θ^ )
dθ
3
mk
2 ∫
tan
2 θ (^) )
0
x 2 ) dx
3
mk
2 ( tan
2 θ^ )
tan
3 (
2 θ^ ))
Above used
x
= tan
(^2) θ^ )
so
dx
2 1 sec
2 (^) (
2 θ^ ) dθ^
and also
sec
2 = (1 + tan
2 )
So we have
π < θ < π
where
θ = − π → t =
where
θ
= 0
t
= 0(
r
= apsidal)
Voyager 2 path (departing 1977)
this procedure is also known as gravity assist.
Consider effective one-body scattering
where problem has rotational symmetry about axis
Define cross section
σ (Ω)
, of units of area, for scattering
in given direction as:
σ (Ω)
d Ω =
σ (Ω)
π (^) sin Θ
d Θ =
the # of particles scattered into solid angle (
d Ω ) per
unit time DIVIDED by the incident intensity
which is
The # of particles scattered into
d Ω = 2
π (^) sin Θ
d Θ
(lying between
and
d Θ
is equal to the # of particles with
s
to
s (^) +
ds
ie:
πIs
ds
| = 2
πσ
sin Θ
d Θ
|
Given that can consider
s (Θ
, differential cross section
σ (Θ) =
s
sin Θ
d ds Θ
∣ ∣ ∣ ∣
eg. for repulsive scattering
Want to find an expression for
s ) , take
so we go back to the equation of orbital motion
θ ( r ) =
θ 0
r
r 0
dr
r 2 √
2 ℓ mE 2
2 ℓ mV 2
r 2 1
with
r 0 =
, θ
π
and for
θ ( r min
θ min
π
−
π
−
θ min
∞
r min
dr
r 2 √
2 ℓ mE 2
2 ℓ mV 2
r 2 1
rewrite using
s √
2 mE
π
= Ψ + Ψ + Θ
s ) =
π
−
(^2)
∫
u min
0
s du
V (^) ( u )
E
(^) s 2 u 2