An Introduction to Celestial Mechanics

Front Cover
Macmillan, 1902 - 384 pages
 

Contents

Parabolic motion
52
Helmholtzs contraction theory
58
Analytical demonstration of law of areas
67
Differential equation of the orbit
75
ᎪᎡᎢ
77
63
85
66
91
The general equations for the components of attraction
100
74
104
The potential and attraction of a thin homogeneous spherical
106
The attraction of a solid homogeneous ellipsoid upon an exterior
118
CHAPTER V
130
Problem in the plane
136
xiv
143
Solution of Keplers equation
149
Position in hyperbolic orbits
156
Transfer of the origin to the earth
163
110
175
CHAPTER VII
183
The regions of real and imaginary velocity
192
Tisserands criterion for the identity of comets
201
Particular values of the constants of integration
207
Equilateral triangular solutions
214
CONTENTS ART PAGE 131 Dynamical properties of the solutions
216
Problems on particular solutions of the problem of three bodies
218
Historical sketch and bibliography
219
CHAPTER VIII
222
Variation of the elements
223
Derivation of the elements from a graphical construction
224
Resolution of the disturbing force
225
Disturbing effects of the orthogonal component
226
Effects of the tangential component upon the major axis
227
Effects of the tangential component upon the eccentricity
228
Effects of the normal component upon the major axis
229
Effects of the normal component upon the eccentricity
231
Disturbing effects of a resisting medium
232
Problems on perturbations
234
Disturbing effects of a third body
236
Perturbations of the node and inclination
237
Resolution of the disturbing acceleration in the plane of motion
238
Perturbations of the major axis
240
Perturbation of the period
241
The variation
243
The parallactic inequality
244
The motion of the line of apsides
245
Secondary effects
247
Perturbations of the eccentricity
248
The evection
249
Gauss method of computing secular variations
250
The long period inequalities
251
Problems on perturbations
252
Historical sketch and bibliography
253
CONTENTS
255
CHAPTER IX
256
ᎪᎡᎢ PAGE 165 Illustrative example
257
Properties of Lagranges brackets
275
Transformation to the ordinary elements
276
Method of direct computation of Lagranges brackets
277
Computation of w 8 8 i i w
281
Computation of a e e σ o a
282
Computation of σ
284
Change from 8 w and a to 8 π and e
286
Introduction of rectangular components of the disturbing ac celeration
288
Problems on variation of elements
290
Computation of perturbations by mechanical quadratures
292
Development of the perturbative function
294
Development in the mutual inclination
295
Development in e̟ and e
297
Developments in Fourier series
298
Periodic variations
301
Long period variations
303
Secular variations
304
Terms of the second order with respect to the masses
305
Lagranges treatment of the secular variations
307
Problems on the perturbative function
311
Historical sketch and bibliography
312
CHAPTER X
315
Correction for parallax
316
The locus fictus
317
196
318
GENERAL CONSIDERATIONS 199 Formulation of problem
319
Intermediate elements
320
General algebraic solution
322
OLBERS METHOD
324
Outline of Olbers method
325
Explicit development of Olbers equations
326
Second method of eliminating p2 206 Third method of eliminating på
328
The approximation in Olbers method
329
The ratios of the triangles
331
Choice of the linear equation
333
Method of solving the equations
335
Solution of Eulers equation for
336
Solution for r₁ and r3 214 Differential corrections
340
Computation of the heliocentric coördinates
341
Computation of i and 8
342
Computation of the time of perihelion passage
344
RECAPITULATION OF METHOD AND FORMULAS FOR THE COMPU 220 Computation of an ephemeris TATION OF AN APPROXIMATE OR...
345
Computation of the geocentric distances
346
Computation of the elements
348
Comparison with other observations 225 Corrections of the elements
349
Variation of one geocentric distance
350
Variation of the elements
351
Problems on the computation of parabolic orbits Historical sketch and bibliography
354
Solution of equation 16
362
Solution of Gauss equations
368
PAGE 315
369
Variation of the elements
378
351
382
354
383

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Page 77 - that every particle of matter in the universe attracts every other particle, with a force whose direction is that of the line joining the two, and whose magnitude is directly as the product of their masses, and inversely as the square of their distances from each other.
Page 4 - Change of motion is proportional to the impressed force and takes place in the direction of the straight line in which the force acts.
Page 3 - LAW I. Every body continues in its state of rest, or of uniform motion in a straight line, unless it is compelled to change that state by forces impressed upon it.
Page 234 - They communicate this tendency to the whole earth so that the plane of the earth's equator turns in the retrograde " direction on the plane of the ecliptic. On the other hand, it follows ' from the symmetry of the figure with respect to the nodes of the orbits of the particles of the equatorial ring that there will be no change in the inclination of the plane of the equator to that of the ecliptic or the moon's orbit. The mass moved is so great, and the forces acting are so small, that this retrograde...
Page 42 - ... as the differences increase. Theoretically, in all gases the range of the values of the velocities is from zero to infinity, although the extreme cases occur at infinitely rare intervals compared to the others. Under constant pressure the velocities are directly proportional to the square root of the temperature, and inversely proportional to the square root of the molecular weight. Since in all gases all velocities exist, some of the molecules of the gaseous envelopes of the heavenly bodies...
Page 53 - The following may be taken for this purpose : — 1. The locus of the second foci of the paths of all projectiles leaving a given point, with a given velocity, in a vertical plane, is a circle. 2. The direction of projection for the greatest range on a given line, passing through the point of projection, bisects the angle between the vertical and the line. 3. Any other point on the line which can be reached at all, can be reached by two different paths, and the directions of projection for these...
Page 249 - made his head ache and kept him awake so often that he would think of it no more.
Page 55 - CALORIE is the amount of heat required to raise the temperature of one kilogram of water one degree centigrade.
Page 128 - Any two bodies attract each other with a force which is proportional to the product of their masses and inversely proportional to the square of the distance between them.
Page 19 - The coordinates of the vector in the ox'y' system are (x',y') and, furthermore, as may be verified, x' = x cos 6 + y sin 6 y

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