kepler geometry of iho elliptical orbits · kepler geometry of iho (isotropic harmonic oscillator)...
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Kepler Geometry of IHO (Isotropic Harmonic Oscillator) Elliptical Orbits(Ch. 9 and Ch. 11 of Unit 1)
Constructing 2D IHO orbits by phasor plotsReview of phasor “clock” geometry (From Lecture 7)Integrating IHO equations by phasor geometry
Constructing 2D IHO orbits using Kepler anomaly plotsMean-anomaly and eccentric-anomaly geometryCalculus and vector geometry of IHO orbitsA confusing introduction to Coriolis-centrifugal force geometry
Some Kepler’s “laws” for central (isotropic) force F(r)Angular momentum invariance of IHO: F(r)=-k·r with U(r)=k·r2/2 (Derived rigorously) Angular momentum invariance of Coulomb: F(r)=-GMm/r2 with U(r)=-GMm·/r (Derived later)Total energy E=KE+PE invariance of IHO: F(r)=-k·r (Derived rigorously)Total energy E=KE+PE invariance of Coulomb: F(r)=-GMm/r2 (Derived later)
Brief introduction to matrix quadratic form geometry
Lecture 8 Revised 12.21.12 from 9.13.2012
1Friday, December 21, 2012
Constructing 2D IHO orbits by phasor plotsReview of phasor “clock” geometry (From Lecture 7)Integrating IHO equations by phasor geometry
2Friday, December 21, 2012
0 12
3
4
5
6
78-7-6
-5
-4
-3
-2-1
01
2
3 4 5
6
78
-7-6
-5
-4-3
-2-1
(2,4)(3,5)(4,6)
(5,7)
(6,8)
(7,-7)
x-position
x-velocity vx/ω
position
x
velocity vx/ω
(a) 1-D Oscillator Phasor Plot
(b) 2-D Oscillator Phasor Plot
Phasor goes
clockwise
by angle ω t
ω t
(8,-6)(9,-5)
y-velocity
vy/ω
(x-Phase 45°
behind
the y-Phase)y-position
φ counter-clockwise
if y is behind x
clockwise
orbit
if x is behind y
(1,3) Left-
handed
Right-
handed
(0,2)
Fx
v0Fy
F=-r(a) (b)
Isotropic Harmonic Oscillator phase dynamics in uniform-body
Unit 1Fig. 9.10
3Friday, December 21, 2012
0 12
3
4
5
6
78-7-6
-5
-4
-3
-2-1
0123 4 5
67
8-7
-6-5-4-3-2-1
(0,4) (1,5)(2,6)(3,7)
(4,8)(5,9)
x-position
x-velocity vx/ω(a) Phasor Plots
for
2-D Oscillator
or
Two 1D Oscillators
(x-Phase 90° behind
the y-Phase)
a
b b
a
a
0 12
3
4
5
6
78-7-6
-5
-4
-3
-2-1
0123 4 5
67
8-7
-6-5-4-3-2-1
(0,0)(1,1)
(5,5)
(2,2)(3,3)
(4,4)
x-position
a
b b
a
a
y-position
y-velocity
vy/ω
x-velocity vx/ω
(b)
x-Phase 0° behind
the y-Phase
(In-phase case)
y-velocity
vy/ω
0 12345
678-7
-6-5-4-3-2-1
(0,4)(1,5)(2,6)(3,7)
b
y-position
b
Fig. 9.11
Unit 1Fig. 9.12
These are more generic exampleswith radius of x-phasor differing from that of the y-phasor.
4Friday, December 21, 2012
x
y
121
2
3
4
56
7
8
9
10
121
2
3
4
56
7
8
9
10
11
00°°--1155°°--3300°°--4455°°++1155°°++3300°°
++4455°°
--6600°°
++6600°°
--7755°°
++7755°°
--9900°°
++9900°°
--110055°°
++110055°°
--112200°°
++112200°°
--113355°°
++113355°°
--115500°°
++115500°°
--116655°°
++116655°°
118800°°
118800°°++227700°° ++224400°°++330000°°336600°° ++221100°°++333300°°
vx /ω
vy /ω
Δαy-x
xphasor
yphasor
x-yspace
x
y
xvx
y
v y
++334455°°--334455°°
...after time advances by 180°:(αx=120°-180°=-60°,αy= +135°-180°=-45°)
r(180°)
Ellipsometry Contact Plotsvs.
Relative phase Δα=αx-αyΔα=−15°
(Right-polarized anti-clockwise case)
...after time advances by 180°:(αx=120°-180°=-60°,αy= +135°-180°=-45°)
Initial phase (αx=120°,αy=+135°)
vxv y
vx-vyspace
v(180°)-45°
-60°
5Friday, December 21, 2012
Constructing 2D IHO orbits by phasor plotsReview of phasor “clock” geometry (From Lecture 7)Integrating IHO equations by phasor geometry
6Friday, December 21, 2012
121
2
3
4
56
7
8
9
10
11
121
2
3
4
56
7
8
9
10
11
x
y
x
y
vx/ω
vy/ω
vx/ω
vy/ω
Initial position: r(0)=(7.0 3.0)
Inital velocity: v(0)=(-8.0 5.0)
7Friday, December 21, 2012
121
2
3
4
56
7
8
9
10
11
121
2
3
4
56
7
8
9
10
11
x
y
x
y
vx/ω
vy/ω
vx/ω
vy/ω
Initial position: r(0)=(7.0 3.0)
Inital velocity: v(0)=(-8.0 6.0)
8Friday, December 21, 2012
121
2
3
4
56
7
8
9
10
11
121
2
3
4
56
7
8
9
10
11
x
y
x
y
vx/ω
vy/ω
vx/ω
vy/ω
Initial position: r(0)=(7.0 3.0)
Inital velocity: v(0)=(-8.0 6.0)
9Friday, December 21, 2012
121
2
3
4
56
7
8
9
10
11
121
2
3
4
56
7
8
9
10
11
x
y
x
y
vx/ω
vy/ω
vx/ω
vy/ω
Initial position: r(0)=(7.0 3.0)
Inital velocity: v(0)=(-8.0 6.0)
10Friday, December 21, 2012
121
2
3
4
56
7
8
9
10
11
121
2
3
4
56
7
8
9
10
11
x
y
x
y
vx/ω
vy/ω
vx/ω
vy/ω
Initial position: r(0)=(7.0 3.0)
Inital velocity: v(0)=(-8.0 6.0)
11Friday, December 21, 2012
121
2
3
4
56
7
8
9
10
11
121
2
3
4
56
7
8
9
10
11
x
y
x
y
vx/ω
vy/ω
vx/ω
vy/ω
Initial position: r(0)=(7.0 3.0)
Inital velocity: v(0)=(-8.0 6.0)
12Friday, December 21, 2012
121
2
3
4
56
7
8
9
10
11
121
2
3
4
56
7
8
9
10
11
x
y
x
y
vx/ω
vy/ω
vx/ω
vy/ω
Initial position: r(0)=(7.0 3.0)
Inital velocity: v(0)=(-8.0 6.0)
13Friday, December 21, 2012
121
2
3
4
56
7
8
9
10
11
121
2
3
4
56
7
8
9
10
11
x
y
x
y
vx/ω
vy/ω
vx/ω
vy/ω
Initial position: r(0)=(7.0 3.0)
Inital velocity: v(0)=(-8.0 6.0)
14Friday, December 21, 2012
121
2
3
4
56
7
8
9
10
11
121
2
3
4
56
7
8
9
10
11
x
y
x
y
vx/ω
vy/ω
vx/ω
vy/ω
Initial position: r(0)=(7.0 3.0)
Inital velocity: v(0)=(-8.0 6.0)
15Friday, December 21, 2012
Constructing 2D IHO orbits using Kepler anomaly plotsMean-anomaly and eccentric-anomaly geometryCalculus and vector geometry of IHO orbitsA confusing introduction to Coriolis-centrifugal force geometry
16Friday, December 21, 2012
b bsin ω t
ω t
ω ta cos ω t
ay=bsin ω t
x=a cos ω t
ω t
r
φ
b
-b
-b
a
a
-a
ω t
a
y=bsin ω t
x=a cos ω t
r
b
-b
-b
a
a
-a
-a
ω t
Step 1. Draw concentriccircles of radius a and band a radius OA at angleω t
Step 3. Draw horizontial line BRfrom b-circle at ω t to line AX.Intersection is orbit point R.
Step 2. Draw vertical line AXfrom a-circle at ωt to x-axis
O
A
O
A
O
A
X X
BR
abω t
b
-b
-b
a
-a
-a
ab
O X O X
Step 4-NRepeatas oftenas needed
ba
Linear HarmonicForce-FieldOrbits
Unit 1Fig. 11.1
(top 2/3’s)
Kepler’s Mean Anomaly Line(slope angle θ =ωt)
Kepler’s Eccentric Anomaly Line
(slope is polar angle φ=atan[y/x])
17Friday, December 21, 2012
b bsin ω t
ω t
ω ta cos ω t
ay=bsin ω t
x=a cos ω t
ω t
r
φ
b
-b
-b
a
a
-a
ω t
a
y=bsin ω t
x=a cos ω t
r
b
-b
-b
a
a
-a
-a
ω t
Step 1. Draw concentriccircles of radius a and band a radius OA at angleω t
Step 3. Draw horizontial line BRfrom b-circle at ω t to line AX.Intersection is orbit point R.
Step 2. Draw vertical line AXfrom a-circle at ωt to x-axis
O
A
O
A
O
A
X X
BR
abω t
b
-b
-b
a
-a
-a
ab
O X O X
Step 4-NRepeatas oftenas needed
ba
Linear HarmonicForce-FieldOrbits
Unit 1Fig. 11.1
Kepler’s Mean Anomaly
Line
Kepler’s Eccentric Anomaly Line
(slope is polar angle φ=atan[y/x])
18Friday, December 21, 2012
Constructing 2D IHO orbits using Kepler anomaly plotsMean-anomaly and eccentric-anomaly geometryCalculus and vector geometry of IHO orbitsA confusing introduction to Coriolis-centrifugal force geometry
19Friday, December 21, 2012
r(t) φv(t)/ω
90°
a(t)/ω2
j(t)/ω3
acceleration
jerk
velocity
position
90°
r(t)φ=ω tv(t)/ω
a(t)/ω2
j(t)/ω3
acceleration
jerk
velocity
position
90°
90°
Time frame angle
φ=ω t(Mean Anomaly)
(a) Orbits (b) Tangents
radius vector :r =rxry
⎛
⎝⎜⎜
⎞
⎠⎟⎟= x
y⎛
⎝⎜
⎞
⎠⎟ =
acosω tbsinω t
⎛
⎝⎜⎜
⎞
⎠⎟⎟=
acosφbsinφ
⎛
⎝⎜⎜
⎞
⎠⎟⎟
velocity vector : v =vxvy
⎛
⎝⎜⎜
⎞
⎠⎟⎟=
−aω sinω tbω cosω t
⎛
⎝⎜⎜
⎞
⎠⎟⎟= dr
dt= r =
acos φ + 2π( )
bsin φ + 2π( )
⎛
⎝
⎜⎜⎜
⎞
⎠
⎟⎟⎟
( for ω = 1)
Unit 1Fig. 11.5
Calculus of IHO orbitsTo make velocity vector v just rotate by π/2 or 90°the mean-anomaly φ of position vector r
mean-anomaly φ of position vector r rotated by π/2 or 90° is m.a. of vector v
20Friday, December 21, 2012
r(t) φv(t)/ω
90°
a(t)/ω2
j(t)/ω3
acceleration
jerk
velocity
position
90°
r(t)φ=ω tv(t)/ω
a(t)/ω2
j(t)/ω3
acceleration
jerk
velocity
position
90°
90°
Time frame angle
φ=ω t(Mean Anomaly)
(a) Orbits (b) Tangents
radius vector :r =rxry
⎛
⎝⎜⎜
⎞
⎠⎟⎟= x
y⎛
⎝⎜
⎞
⎠⎟ =
acosω tbsinω t
⎛
⎝⎜⎜
⎞
⎠⎟⎟=
acosφbsinφ
⎛
⎝⎜⎜
⎞
⎠⎟⎟
velocity vector : v =vxvy
⎛
⎝⎜⎜
⎞
⎠⎟⎟=
−aω sinω tbω cosω t
⎛
⎝⎜⎜
⎞
⎠⎟⎟= dr
dt= r =
acos φ + 2π( )
bsin φ + 2π( )
⎛
⎝
⎜⎜⎜
⎞
⎠
⎟⎟⎟
( for ω = 1)
accelerationor force vector : Fm= a =
axay
⎛
⎝⎜⎜
⎞
⎠⎟⎟=
−aω 2 cosω t
−bω 2 sinω t
⎛
⎝⎜⎜
⎞
⎠⎟⎟= dv
dt= v = r = d2r
dt2=
acos φ + 22π( )
bsin φ + 22π( )
⎛
⎝
⎜⎜⎜
⎞
⎠
⎟⎟⎟
Unit 1Fig. 11.5
or changeof velocity
Calculus of IHO orbitsTo make velocity vector v just rotate by π/2 or 90°the mean-anomaly φ of position vector r
mean-anomaly φ of position vector r rotated by π/2 or 90° is m.a. of vector v
m.a. φ+π/2 of vector v rotated byanother π/2 is m.a. of vector a
21Friday, December 21, 2012
r(t) φv(t)/ω
90°
a(t)/ω2
j(t)/ω3
acceleration
jerk
velocity
position
90°
r(t)φ=ω tv(t)/ω
a(t)/ω2
j(t)/ω3
acceleration
jerk
velocity
position
90°
90°
Time frame angle
φ=ω t(Mean Anomaly)
(a) Orbits (b) Tangents
radius vector :r =rxry
⎛
⎝⎜⎜
⎞
⎠⎟⎟= x
y⎛
⎝⎜
⎞
⎠⎟ =
acosω tbsinω t
⎛
⎝⎜⎜
⎞
⎠⎟⎟=
acosφbsinφ
⎛
⎝⎜⎜
⎞
⎠⎟⎟
velocity vector : v =vxvy
⎛
⎝⎜⎜
⎞
⎠⎟⎟=
−aω sinω tbω cosω t
⎛
⎝⎜⎜
⎞
⎠⎟⎟= dr
dt= r =
acos φ + 2π( )
bsin φ + 2π( )
⎛
⎝
⎜⎜⎜
⎞
⎠
⎟⎟⎟
( for ω = 1)
accelerationor force vector : Fm= a =
axay
⎛
⎝⎜⎜
⎞
⎠⎟⎟=
−aω 2 cosω t
−bω 2 sinω t
⎛
⎝⎜⎜
⎞
⎠⎟⎟= dv
dt= v = r = d2r
dt2=
acos φ + 22π( )
bsin φ + 22π( )
⎛
⎝
⎜⎜⎜
⎞
⎠
⎟⎟⎟
jerk or changeof acceleration : j=jxjy
⎛
⎝⎜⎜
⎞
⎠⎟⎟=
+aω 3sinω t
−bω 3cosω t
⎛
⎝⎜⎜
⎞
⎠⎟⎟= da
dt= a = v = r = d3r
dt3=
acos φ + 23π( )
bsin φ + 23π( )
⎛
⎝
⎜⎜⎜
⎞
⎠
⎟⎟⎟
Unit 1Fig. 11.5
or changeof velocity or changeof velocity
Calculus of IHO orbitsTo make velocity vector v just rotate by π/2 or 90°the mean-anomaly φ of position vector r
mean-anomaly φ of position vector r rotated by π/2 or 90° is m.a. of vector v
m.a. φ+π/2 of vector v rotated byanother π/2 is m.a. of vector a
...and so forth...
22Friday, December 21, 2012
r(t) φv(t)/ω
90°
a(t)/ω2
j(t)/ω3
acceleration
jerk
velocity
position
90°
r(t)φ=ω tv(t)/ω
a(t)/ω2
j(t)/ω3
acceleration
jerk
velocity
position
90°
90°
Time frame angle
φ=ω t(Mean Anomaly)
(a) Orbits (b) Tangents
radius vector :r =rxry
⎛
⎝⎜⎜
⎞
⎠⎟⎟= x
y⎛
⎝⎜
⎞
⎠⎟ =
acosω tbsinω t
⎛
⎝⎜⎜
⎞
⎠⎟⎟=
acosφbsinφ
⎛
⎝⎜⎜
⎞
⎠⎟⎟
velocity vector : v =vxvy
⎛
⎝⎜⎜
⎞
⎠⎟⎟=
−aω sinω tbω cosω t
⎛
⎝⎜⎜
⎞
⎠⎟⎟= dr
dt= r =
acos φ + 2π( )
bsin φ + 2π( )
⎛
⎝
⎜⎜⎜
⎞
⎠
⎟⎟⎟
( for ω = 1)
accelerationor force vector : Fm= a =
axay
⎛
⎝⎜⎜
⎞
⎠⎟⎟=
−aω 2 cosω t
−bω 2 sinω t
⎛
⎝⎜⎜
⎞
⎠⎟⎟= dv
dt= v = r = d2r
dt2=
acos φ + 22π( )
bsin φ + 22π( )
⎛
⎝
⎜⎜⎜
⎞
⎠
⎟⎟⎟
jerk or changeof acceleration : j=jxjy
⎛
⎝⎜⎜
⎞
⎠⎟⎟=
+aω 3sinω t
−bω 3cosω t
⎛
⎝⎜⎜
⎞
⎠⎟⎟= da
dt= a = v = r = d3r
dt3=
acos φ + 23π( )
bsin φ + 23π( )
⎛
⎝
⎜⎜⎜
⎞
⎠
⎟⎟⎟
inaugurationor changeof jerk :i =ixiy
⎛
⎝⎜⎜
⎞
⎠⎟⎟=
+aω 4 cosω t
+bω 4 sinω t
⎛
⎝⎜⎜
⎞
⎠⎟⎟= dj
dt= j= a = v = r = d4r
dt4=
acos φ + 24π( )
bsin φ + 24π( )
⎛
⎝
⎜⎜⎜
⎞
⎠
⎟⎟⎟
Unit 1Fig. 11.5
or changeof velocity or changeof velocity or changeof velocity
Calculus of IHO orbitsTo make velocity vector v just rotate by π/2 or 90°the mean-anomaly φ of position vector r
mean-anomaly φ of position vector r rotated by π/2 or 90° is m.a. of vector v
m.a. φ+π/2 of vector v rotated byanother π/2 is m.a. of vector a
...and so forth...
...and so on...
23Friday, December 21, 2012
Constructing 2D IHO orbits using Kepler anomaly plotsMean-anomaly and eccentric-anomaly geometryCalculus and vector geometry of IHO orbitsA confusing introduction to Coriolis-centrifugal force geometry
24Friday, December 21, 2012
F = -kr
orbital velocity=V
(b) “Carnival kid” orbiting inspace attached to a spring
centrifugalforce=+kr=+mω2r
ω t
centripetalforce=
(due to spring)
Carnival kidsays:
“This is awful!I can hardlyhold ontothis darnspring.”
F = -kr
orbital velocity=V
(a) “Earthronaut” orbitingtunnel inside Earth
centrifugalforce=+kr=+mω2r
ω t
centripetalforce=
(due to gravity)
Earthronautsays:
“This is great!I’m weightless.”
apogee(x=a, y=0)aphelion=a
perigee(x=0,y=b)
θperhelion=bmass gaining speed
as it falls
VelocityV
θVelocityV centripetal force F=-kr
Negative power( F•V=|F||V|cos θ <0)
Positive power( F•V=|F||V|cos θ >0)
mass losing speedas it rises
Unit 1Fig. 11.2
Unit 1Fig. 11.3
(Radius r decreasing)(Radius r increasing)
25Friday, December 21, 2012
Velocity
V
centripetal force F=-kr
centrifugal force
Total inertial force F=+kr
Coriolis force
centrifugal force
Velocity
along
radial
path
Coriolis force
(depends on
radial path
speed)
Rotational
velocity
V=ωr
circle
of
curvature
Velocity
V
centrifugal force is
Total inertial force F=+kr
circle
of
curvature
(a) Centrifugal and Coriolis
Forces on Merry-Go-Round
(b) Centrifugal and Coriolis
Forces on Oscillator Orbit
(Falling phase)
(c) Centrifugal and Coriolis
Forces on Oscillator Orbit
(Rising phase)
centrifugal force
Velocity
along
radial
path
Coriolis force
centripetal force F=-kr
Velocity
V
centripetal force F=-kr
centrifugal force
Total inertial force F=+kr
Coriolis force
circle
of
curvature
(d) Centrifugal Force
on Oscillator Orbit
(apogee and perigee)
Velocity
V
centripetal force F=-kr
centrifugal force is
Total inertial force F=+kr
Unit 1Fig. 11.4
a-d
Quite confusing? Discussion of Coriolisforces will be done more elegantly and made more physically intuitive in Ch. 12 of Unit1 and in Unit 6.
Physicist Force (where m wants to go)
Mathematician Force (would hold m back)
26Friday, December 21, 2012
Some Kepler’s “laws” for central (isotropic) force F(r)Angular momentum invariance of IHO: F(r)=-k·r with U(r)=k·r2/2 (Derived rigorously) Angular momentum invariance of Coulomb: F(r)=-GMm/r2 with U(r)=-GMm·/r (Derived later)Total energy E=KE+PE invariance of IHO: F(r)=-k·r (Derived rigorously)Total energy E=KE+PE invariance of Coulomb: F(r)=-GMm/r2 (Derived later)
27Friday, December 21, 2012
1. Area of triangle rv = r × v/2 is constant
r × v = rxvy − ryvx = acosω t ⋅ bω cosω t( )− bsinω t ⋅ −aω sinω t( ) = ab ⋅ω
t = 0 t = π/3ω t = π/2ωv=a ωv=b ω
r rr
ba
Unit 1Fig. 11.8
Some Kepler’s “laws” for central (isotropic) force F(r)...and certainly apply to the IHO: F(r)=-k·r with U(r)=k·r2/2
for IHO
vxvy
⎛
⎝⎜⎜
⎞
⎠⎟⎟=
−aω sinω tbω cosω t
⎛
⎝⎜⎜
⎞
⎠⎟⎟
rxry
!
"##
$
%&&= x
y
!
"#
$
%& =
acos! tbsin! t
!
"##
$
%&&
(Recall from Lecture 7: k = Gm 4π
3ρ⊕ )
28Friday, December 21, 2012
1. Area of triangle rv = r × v/2 is constant
r × v = rxvy − ryvx = acosω t ⋅ bω cosω t( )− asinω t ⋅ −bω sinω t( ) = ab ⋅ω
2. Angular momentum L = mr × v is conserved
L = m |r × v |= m rxvy − ryvx( ) = m ⋅ab ⋅ω
t = 0 t = π/3ω t = π/2ωv=a ωv=b ω
r rr
ba
Unit 1Fig. 11.8
Some Kepler’s “laws” that apply to any central (isotropic) force F(r)...and certainly apply to the IHO: F(r)=-k·r with U(r)=k·r2/2
for IHO
for IHO
rv
|r×v| =r·v·sinrv
(Recall from Lecture 7: k = Gm 4π
3ρ⊕ )
29Friday, December 21, 2012
1. Area of triangle rv = r × v/2 is constant
r × v = rxvy − ryvx = acosω t ⋅ bω cosω t( )− asinω t ⋅ −bω sinω t( ) = ab ⋅ω2. Angular momentum L = mr × v is conserved
L = m |r × v |= m rxvy − ryvx( ) = m ⋅ab ⋅ω
t = 0 t = π/3ω t = π/2ωv=a ωv=b ω
r rr
ba
Unit 1Fig. 11.8
Some Kepler’s “laws” that apply to any central (isotropic) force F(r)...and certainly apply to the IHO: F(r)=-k·r with U(r)=k·r2/2
for IHO
for IHO
3. Equal area is swept by radius vector in each equal time interval T
AT =r × dr
20
T
∫ =r × dr
dt2
dt0
T
∫ = r × v2
dt0
T
∫ = L2m
dt0
T
∫ = L2m
T for IHO
by 2.
rdr
|r×dr| =r·dr·sinrdr
(Recall from Lecture 7: k = Gm 4π
3ρ⊕ )
30Friday, December 21, 2012
1. Area of triangle rv = r × v/2 is constant
r × v = rxvy − ryvx = acosω t ⋅ bω cosω t( )− asinω t ⋅ −bω sinω t( ) = ab ⋅ω2. Angular momentum L = mr × v is conserved
L = mr × v = m rxvy − ryvx( ) = m ⋅ab ⋅ω = m ⋅ab ⋅ 2πτ
t = 0 t = π/3ω t = π/2ωv=a ωv=b ω
r rr
ba
Unit 1Fig. 11.8
Some Kepler’s “laws” that apply to any central (isotropic) force F(r)...and certainly apply to the IHO: F(r)=-k·r with U(r)=k·r2/2
for IHO
for IHO
3. Equal area is swept by radius vector in each equal time interval T
AT =r × dr
20
T
∫ =r × dr
dt2
dt0
T
∫ = r × v2
dt0
T
∫ = L2m
dt0
T
∫ = L2m
T for IHO
In one period: τ= 1υ
= 2πω
= 2mAτ
L the area is: Aτ =
Lτ2m
( = ab ⋅π for ellipse orbit)
(Recall from Lecture 7: k = Gm 4π
3ρ⊕ )
31Friday, December 21, 2012
1. Area of triangle rv = r × v/2 is constant
r × v = rxvy − ryvx = acosω t ⋅ bω cosω t( )− asinω t ⋅ −bω sinω t( ) = ab ⋅ω2. Angular momentum L = mr × v is conserved
L = mr × v = m rxvy − ryvx( ) = m ⋅ab ⋅ω = m ⋅ab ⋅ 2πτ
t = 0 t = π/3ω t = π/2ωv=a ωv=b ω
r rr
ba
Unit 1Fig. 11.8
Some Kepler’s “laws” that apply to any central (isotropic) force F(r)...and certainly apply to the IHO: F(r)=-k·r with U(r)=k·r2/2
for IHO
for IHO
3. Equal area is swept by radius vector in each equal time interval T
AT =r × dr
20
T
∫ =r × dr
dt2
dt0
T
∫ = r × v2
dt0
T
∫ = L2m
dt0
T
∫ = L2m
T for IHO
In one period: τ= 1υ
= 2πω
= 2mAτ
L the area is: Aτ =
Lτ2m
( = ab ⋅π for ellipse orbit)
(Recall from Lecture 7: k = Gm 4π
3ρ⊕ )
( Recall from Lecture 7: ω = k /m = Gρ⊕4π / 3 )
32Friday, December 21, 2012
Some Kepler’s “laws” for central (isotropic) force F(r)Angular momentum invariance of IHO: F(r)=-k·r with U(r)=k·r2/2 (Derived rigorously) Angular momentum invariance of Coulomb: F(r)=-GMm/r2 with U(r)=-GMm·/r (Derived later)Total energy E=KE+PE invariance of IHO: F(r)=-k·r (Derived rigorously)Total energy E=KE+PE invariance of Coulomb: F(r)=-GMm/r2 (Derived later)
33Friday, December 21, 2012
1. Area of triangle rv = r × v/2 is constant
r × v = rxvy − ryvx =ab ⋅ Gρ⊕4π / 3 for IHO
a−1/2b GM⊕ for Coul.
⎧⎨⎪
⎩⎪
t = 0 t = π/3ω t = π/2ωv=a ωv=b ω
r rr
ba
Some Kepler’s “laws” that apply to any central (isotropic) force F(r)Apply to IHO: F(r)=-k·r with U(r)=k·r2/2 and Coulomb: F(r)=-GMm/r2 with U(r)=-GMm·/r
for IHO
t = 0 vv
r rrba
v
vrCoulomb:
IHO:
for Coul.
34Friday, December 21, 2012
1. Area of triangle rv = r × v/2 is constant
r × v = rxvy − ryvx =ab ⋅ Gρ⊕4π / 3 for IHO
a−1/2b GM⊕ for Coul.
⎧⎨⎪
⎩⎪2. Angular momentum L = mr × v is conserved
L = mr × v = m rxvy − ryvx( ) = m·ab ⋅ Gρ⊕4π / 3 for IHO
m·a−1/2b GM⊕ for Coul.
⎧⎨⎪
⎩⎪
t = 0 t = π/3ω t = π/2ωv=a ωv=b ω
r rr
ba
Some Kepler’s “laws” that apply to any central (isotropic) force F(r)Apply to IHO: F(r)=-k·r with U(r)=k·r2/2 and Coulomb: F(r)=-GMm/r2 with U(r)=-GMm·/r
for IHO
for IHO
t = 0 vv
r rrba
v
vrCoulomb:
IHO:
for Coul.
for Coul.
35Friday, December 21, 2012
1. Area of triangle rv = r × v/2 is constant
r × v = rxvy − ryvx =ab ⋅ Gρ⊕4π / 3 for IHO
a−1/2b GM⊕ for Coul.
⎧⎨⎪
⎩⎪2. Angular momentum L = mr × v is conserved
L = mr × v = m rxvy − ryvx( ) = m·ab ⋅ Gρ⊕4π / 3 for IHO
m·a−1/2b GM⊕ for Coul.
⎧⎨⎪
⎩⎪
t = 0 t = π/3ω t = π/2ωv=a ωv=b ω
r rr
ba
Some Kepler’s “laws” that apply to any central (isotropic) force F(r)Apply to IHO: F(r)=-k·r with U(r)=k·r2/2 and Coulomb: F(r)=-GMm/r2 with U(r)=-GMm·/r
for IHO
for IHO
3. Equal area is swept by radius vector in each equal time interval T
τ= 1υ= 2πω
= 2mAτ
L= 2m·ab ⋅π
L=
2m·ab ⋅πm·ab ⋅ Gρ⊕4π / 3
= 2πGρ⊕4π / 3
for IHO
2m·ab ⋅πm·a−1/2b GM⊕
= 2πa−3/2 GM⊕
for Coul.
⎧
⎨
⎪⎪
⎩
⎪⎪
t = 0 vv
r rrba
v
vrCoulomb:
IHO:
for Coul.
for Coul.
In one period:
that is ωIHO
that is ωCoul
Applies toany central
F(r)
Applies toIHO and Coulomb
36Friday, December 21, 2012
Some Kepler’s “laws” for central (isotropic) force F(r)Angular momentum invariance of IHO: F(r)=-k·r with U(r)=k·r2/2 (Derived rigorously) Angular momentum invariance of Coulomb: F(r)=-GMm/r2 with U(r)=-GMm·/r (Derived later)Total energy E=KE+PE invariance of IHO: F(r)=-k·r (Derived rigorously)Total energy E=KE+PE invariance of Coulomb: F(r)=-GMm/r2 (Derived later)
37Friday, December 21, 2012
Kepler laws involve -momentum conservation in isotropic force F(r)Now consider orbital energy conservation of the IHO: F(r)=-k·r with U(r)=k·r2/2
Total energy=KE+PE is constant
KE + PE = 12v iM i v + 1
2r iK i r
= 12
vx vy( )• m 00 m
⎛⎝⎜
⎞⎠⎟•
vxvy
⎛
⎝⎜⎜
⎞
⎠⎟⎟+ rx ry( )• k 0
0 k⎛⎝⎜
⎞⎠⎟•
rxry
⎛
⎝⎜⎜
⎞
⎠⎟⎟
= 12mv2
x + 12mv2
y + 12kr2
x + 12kr2
y
= 12m(−aω sinω t)2 + 1
2m(bω cosω t)2 + 1
2k(acosω t)2 + 1
2k(bsinω t)2
vxvy
⎛
⎝⎜⎜
⎞
⎠⎟⎟=
−aω sinω tbω cosω t
⎛
⎝⎜⎜
⎞
⎠⎟⎟
rxry
!
"##
$
%&&= x
y
!
"#
$
%& =
acos! tbsin! t
!
"##
$
%&&
38Friday, December 21, 2012
Kepler laws involve -momentum conservation in isotropic force F(r)Now consider orbital energy conservation of the IHO: F(r)=-k·r with U(r)=k·r2/2
Total IHO energy=KE+PE is constant
KE + PE = 12v iM i v + 1
2r iK i r
= 12
vx vy( )• m 00 m
⎛⎝⎜
⎞⎠⎟•
vxvy
⎛
⎝⎜⎜
⎞
⎠⎟⎟+ rx ry( )• k 0
0 k⎛⎝⎜
⎞⎠⎟•
rxry
⎛
⎝⎜⎜
⎞
⎠⎟⎟
= 12mv2
x + 12mv2
y + 12kr2
x + 12kr2
y
= 12m(−aω sinω t)2 + 1
2m(bω cosω t)2 + 1
2k(acosω t)2 + 1
2k(bsinω t)2
= 12ma2ω 2 (sin2ω t) + 1
2mb2ω 2 (cos2ω t)2 + 1
2ka2 (cos2ω t) + 1
2kb2 (sin2ω t)
= 12mω 2 (a2 + b2 ) Given : k = mω 2
39Friday, December 21, 2012
= 12ma2ω 2 (sin2ω t) + 1
2mb2ω 2 (cos2ω t)2 + 1
2ka2 (cos2ω t) + 1
2kb2 (sin2ω t)
= 12mω 2 (a2 + b2 ) Given : k = mω 2
E = KE + PE = 12mω 2 (a2 + b2 ) = 1
2k(a2 + b2 ) since: ω = k
m = Gρ⊕4π / 3 or: mω 2 = k
Kepler laws involve -momentum conservation in isotropic force F(r)Now consider orbital energy conservation of the IHO: F(r)=-k·r with U(r)=k·r2/2
Total IHO energy=KE+PE is constant
KE + PE = 12v iM i v + 1
2r iK i r
= 12
vx vy( )• m 00 m
⎛⎝⎜
⎞⎠⎟•
vxvy
⎛
⎝⎜⎜
⎞
⎠⎟⎟+ rx ry( )• k 0
0 k⎛⎝⎜
⎞⎠⎟•
rxry
⎛
⎝⎜⎜
⎞
⎠⎟⎟
= 12mv2
x + 12mv2
y + 12kr2
x + 12kr2
y
= 12m(−aω sinω t)2 + 1
2m(bω cosω t)2 + 1
2k(acosω t)2 + 1
2k(bsinω t)2
40Friday, December 21, 2012
Some Kepler’s “laws” for central (isotropic) force F(r)Angular momentum invariance of IHO: F(r)=-k·r with U(r)=k·r2/2 (Derived rigorously) Angular momentum invariance of Coulomb: F(r)=-GMm/r2 with U(r)=-GMm·/r (Derived later)Total energy E=KE+PE invariance of IHO: F(r)=-k·r (Derived rigorously)Total energy E=KE+PE invariance of Coulomb: F(r)=-GMm/r2 (Derived later)
41Friday, December 21, 2012
Kepler laws involve -momentum conservation in isotropic force F(r)Now consider orbital energy conservation of the IHO: F(r)=-k·r with U(r)=k·r2/2
We'll see that the Coul. orbits are simpler: (like the period...not a function of b)
E = KE + PE = 12mv2
x +12mv2
y −kr= 1
2mv2
x +12mv2
y −GM⊕m
r= −GM⊕m
a
Total IHO energy=KE+PE is constant
KE + PE = 12v iM i v + 1
2r iK i r
= 12
vx vy( )• m 00 m
⎛⎝⎜
⎞⎠⎟•
vxvy
⎛
⎝⎜⎜
⎞
⎠⎟⎟+ rx ry( )• k 0
0 k⎛⎝⎜
⎞⎠⎟•
rxry
⎛
⎝⎜⎜
⎞
⎠⎟⎟
= 12mv2
x + 12mv2
y + 12kr2
x + 12kr2
y
= 12m(−aω sinω t)2 + 1
2m(bω cosω t)2 + 1
2k(acosω t)2 + 1
2k(bsinω t)2
= 12ma2ω 2 (sin2ω t) + 1
2mb2ω 2 (cos2ω t)2 + 1
2ka2 (cos2ω t) + 1
2kb2 (sin2ω t)
= 12mω 2 (a2 + b2 ) Given : k = mω 2
E = KE + PE = 12mω 2 (a2 + b2 ) = 1
2k(a2 + b2 ) since: ω = k
m = Gρ⊕4π / 3 or: mω 2 = k
42Friday, December 21, 2012
Quadratic forms and tangent contact geometry of their ellipses
A matrix Q that generates an ellipse by r•Q•r=1 is called positive-definite
r •Q• r = 1
x y( )•1
a20
0 1
b2
⎛
⎝
⎜⎜⎜⎜⎜
⎞
⎠
⎟⎟⎟⎟⎟
• xy
⎛
⎝⎜
⎞
⎠⎟ = 1= x y( )•
xa2
yb2
⎛
⎝
⎜⎜⎜⎜⎜
⎞
⎠
⎟⎟⎟⎟⎟
= x2
a2+ y2
b2
A inverse matrix Q-1 generates an ellipse by p•Q -1•p=1 called inverse or dual ellipse:
p•Q−1•p = 1
px py( )• a2 0
0 b2
⎛
⎝⎜⎜
⎞
⎠⎟⎟•
pxpy
⎛
⎝⎜⎜
⎞
⎠⎟⎟= 1= px py( )• a2 px
b2 py
⎛
⎝
⎜⎜⎜
⎞
⎠
⎟⎟⎟= a2 px
2 + b2 y2
43Friday, December 21, 2012
r(φ)
φ=ω t
ab
b-circle
a-circle
r(φ)ab
r(φ)=r(φ+π/2)•
r(φ)•r(φ)
Original ellipse
r•Q•r = r•p = 1
p(φ)
p(φ)
p(φ)= p(φ+π/2)•
p(φ)•
vector p(φ) isperpendicular
to r(φ)•vector p(φ) isperpendicular
to r(φ)
•Inverse ellipse
p•Q-1•p =p•r = 1
p(φ)
(a) Quadratic form ellipse and
Inverse quadratic form ellipse
(b) Ellipse tangents
r(φ)•
φ=ω t
p =Q i r = 1/ a2 00 1/ b2
⎛
⎝⎜
⎞
⎠⎟ •
xy
⎛
⎝⎜
⎞
⎠⎟ =
x / a2
y / b2
⎛
⎝⎜⎜
⎞
⎠⎟⎟=
(1 / a)cosφ(1 / b)sinφ
⎛
⎝⎜
⎞
⎠⎟ where:
x = rx = acosφ = acosω ty = ry = bsinφ = bsinω t
so: p i r = 1
r • p = 0 = rx ry( ) • pxpy
⎛
⎝⎜
⎞
⎠⎟ = −a sinφ b cosφ( ) • (1 / a) cosφ
(1 / b) sinφ⎛⎝⎜
⎞⎠⎟
where:rx = −a sinφry = b cosφ
and:px = (1 / a) cosφ py = (1 / b) sinφ
Note some quadratic form mutual duality relations:unit
mutual projection
p is perpendicular to velocity v=r , a mutual orthogonality•
Unit 1Fig. 11.6
44Friday, December 21, 2012