Title: Discovery of Neptune and Planetary Perturbation
1Discovery of Neptune and Planetary Perturbation
- Tse Hon Ning
- Wong Mau Fung
2Content
- Introduction
- Forward problem - Uranus Perturbation
- Inverse problem Orbital element of Neptune
- Very brief story of Pluto
- Summary
3Introduction
4Uranus
- Discovered in 1781
- 1821, irregularities in Uranuss orbit were
observed. - Radial distance from the Sun
- Heliocentric longitude
-
5The discrepancy in HL of Uranus,
6The main features of
- Typical magnitude 50 100s of arc
- Approximate period 110 yrs
- Secular variation appeared
- ?fraise through 0 at 1777
7Possible reasons for the irregularities
- Observational error?
- Correction of Newtons law of gravitation for
distance object? - Perturbed by an undiscovered planet?
8Perturbed by an undiscovered planet!!
John Couch Adams
Urbain Le Verrier
?f?orbital elements of the unknown planet
(inverse problem!)
9- Neptune was found in 1864!!!
10The forward problem in celestial mechanics
- The perturbation of Uranus
11Forward Problem
model parameters ? data
Orbital elements of Neptune
12- Formulation
- Equations of motion
- u radial displacement
- v tangential displacement
- The homogeneous solutions of u, v
- Brief calculation
- Interpretation
- The inhomogeneous solutions of u, v
- Brief calculation
- Interpretation
- The complete solution of
- Finding constants by fitting
- Physical Interpretation
- The effect of the 2 solutions
13Formulation
- Approximations
- angle of inclination of orbits ignored
- (U0.77 N1.78)
- Eccentricities are ignored
- (U0.0471 N0.0085)
14??f remaining discrepancy in HL after subtracted
other planetary perturbations ? all other planets
can be ignored ? 3 bodies problem (Sun, Uranus,
Neptune)
15Inertial frame U,N no interaction
- Unperturbed
- Coplanar circular orbits
- Radii RU, RN known semimajor axes
16Inertial frame U,N no interaction
Units Length AU Time year Mass solar mass
TU, TN orbital period of U and N O2p/T
orbital frequency t t-t0 t0 1822 time of
conjunction
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18Rotating frame U,N no interaction
- Rotating with U
- angular velocity of N - O
- ? OU gt ON
- O OU ON 3.666 x 10-2
19Rotating frame U,N no interaction
Polar co-ordinates of U ?U(t), fU(t)
Unperturbed solution ?U(0)(t) RU fU(0)(t) OUt
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21 22The homogeneous solutions of u, v
- Linear, second-order DEs describing a
non-dissipative system - u, v 2 coupled oscillators
- ? Finding the normal modes!
23The homogeneous solutions of u, v
- Frequencies of the normal mode 0, OU
- I) freq. 0
Where ai are constants.
24The homogeneous solutions of u, v
25Interpretation on the homo. solutions
- The 2 homo. Solutions represent
- the difference between 2 nearby Kepler orbits
- Denote by semimajor axis a and eccentricity e
- Unperturbed orbit a RU e 0
26Interpretation on the homo. solutions
- 2 independent classes of nearby Kepler orbits
- a RU ?a e 0
- a RU e ?e ? 0
27Interpretation on the homo. solutions
- a RU ?a e 0
- Circular orbit of slightly larger radius
- ? slightly lower frequency
- Circular ? u constant
- Slightly different frequency ? v has a term
linear in t
28Interpretation on the homo. solutions
u constant
linear in t
29Interpretation on the homo. solutions
Keplers third law
Varying about O OU R RU
Putting
30Interpretation on the homo. solutions
- II) a RU e ?e ? 0
- Period independent of eccentricity
- ? frequency no changed OU
- ? u, v also have freq. OU
- Remark for Freq. OU
31Interpretation on the homo. solutions
Keplers second law
Varying about O OU R RU
Putting
32Interpretation on the homo. solutions
- ?The homo. solutions contain the info. given by
Keplers laws.
33The inhomogeneous solutions of u, v
y
Expressing the force in ?
U
x
S
N
34The inhomogeneous solutions of u, v
- First term acceleration of U toward N
- Second term acceleration of S toward N
- ?1st 2nd acceleration of U relative to S
- Substitute the ?terms
- where
35The inhomogeneous solutions of u, v
36The inhomogeneous solutions of u, v
- Fr and Ffare periodic,
- They contain harmonics at freq. nO
- ? Fourier Series!
odd
even
Fourier coeff.
37The inhomogeneous solutions of u, v
38The inhomogeneous solutions of u, v
- 2 coupled oscillators, driven by forces with
- freq. nO
- ? the inhomo. soln also hv freq. nO
- Let , sub. Into
- The coeff.
- Then
39Interpretation of the inhomogeneous solution
- for
n2 - Hence n2 term dominate
- Sub into the solution to get
- The period and phase nearly agree with observed
data - But amplitude too large!!
40The complete solution
- The complete solution sum of the homogeneous and
inhomogeneous solutions -
- determined by initial values and time
derivatives of u and v - But no reason to prefer the data at the initial
time than any other time
41The complete solution
- Thus use linear least-squares-fitting, minimize
- With many data points
- The best fit is found to be
42Partial contribution of the homogeneous and
inhomogeneous solution
43Partial contribution of the homogeneous and
inhomogeneous solution
- Magnitudes of these sinusoidal terms
- As their frequencies are approximately equal
-
- the complete solution would show beats.
- The discussed time has small beat amplitude of
, but will get larger and larger in later
time, since adding, not cancelling of the
solutions.
44Partial contribution of the homogeneous and
inhomogeneous solution
45Sum of the contribution
46Inverse problem in celestial mechanics
- Orbital element of Neptune
47Inverse problem
- To Determine orbital elements from the historical
data on . - Fit the data to the complete solution
- Situation
- Neptunes mass unknown
- Frequency of Neptune unknown
- Time of conjunction unknown
48Inverse problem
- is proportional to Neptune mass
- Use ratio
- assumed Neptune mass/ true
Neptune mass - Frequency of the Neptune
- Thus D is now a function of seven variables
49Inverse problem
- To minimize with respect to
all seven variables ?determine the Neptunes
orbital elements - Given , we can find best and
analytically and define - But can be found numerically only!!!!
50Inverse problem
- By modern knowledge , expected value of and
are known - Try the results close to the expected values of
them - Thus , and can be determined, results
- Root mean square is smaller than in the
forward problem
51The best fit is incorrect?
- The inhomogeneous solution
- True frequency leads to a driving force slightly
under resonance - But the fitted frequency corresponds to a force
slightly above resonance - and not individually constrained by the
data. - But we just need to show resonance!!
52Inverse problem (phase ambiguity)
- Second harmonic (n2) ? phase ambiguity
- i) after displacing N by 180 degrees
- ( )
- ii) the inhomogeneous solution would be
completely unchanged - iii) thus another good fit can be found by
the local minimum
53Inverse problem (phase ambiguity)
- Thus there are two solutions for the heliocentric
longitude of Neptune, diametrically opposite each
other - And they are not too different in terms of the
quality of the fit to the data
54Brief review on the model
- forward problem orbital elements?
-
-
55Brief review on the model
- Inverse problem ?orbital elements
- Result agrees but have phase ambiguity
56Brief story of Pluto
- Immense distance from Earth
- Discovered until 1930(by Lowell)
- Lowell believe planet X exists, based on
calculations done with study of the motions of
Uranus and Neptune - Then set up Lowell Observatory
- Tombaugh used photographs
57Brief story of Pluto
- Any shifting of object against backdrop of the
stars ? present of planetary body - Pluto finally found on 18, Feb, 1930.
- However, pluto too small to affect the orbit of
Neptune - Continue efforts ? turned out to be error in
calculations when Voyager 2 was used.
58Whether a planet exists?
- How bright the planet is?
- How fast it was moving at the time of search?
- How accurate the predictions are from the
celestial mechanics calculations? - How good quality is the observations?
59Summary
- Ephemerides have been improving
- But a consistent one could not be prepared based
on all available data - Two planets have already been discovered based on
the motion of Uranus - Are there more?
60The End?