A History of MechanicsRoutledge & Paul, 1957 - 671 стор. |
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Сторінка 544
... trajectory about a fixed nucleus ) . The polar and parabolic coordinates used by Epstein both allow the ... trajectory passes as near as may be desired to all the points of a region of E , defined by hyperspheres of n - 1 dimensions . If ...
... trajectory about a fixed nucleus ) . The polar and parabolic coordinates used by Epstein both allow the ... trajectory passes as near as may be desired to all the points of a region of E , defined by hyperspheres of n - 1 dimensions . If ...
Сторінка 560
... trajectory , must be an integral multiple of 27 in order that the association of the waves and the particle may remain coherent . For the path dl of the point on the trajectory , the phase varies by do = 2πν dl By integrating along a ...
... trajectory , must be an integral multiple of 27 in order that the association of the waves and the particle may remain coherent . For the path dl of the point on the trajectory , the phase varies by do = 2πν dl By integrating along a ...
Сторінка 569
... trajectory , taking 27 as the unit . • uni- “ To write that the integral in question is a whole multiple of h amounts to the same as to write that the phase of the wave is a form ' function along the trajectory , that is to say that the ...
... trajectory , taking 27 as the unit . • uni- “ To write that the integral in question is a whole multiple of h amounts to the same as to write that the phase of the wave is a form ' function along the trajectory , that is to say that the ...
Зміст
Nicholas Copernicus 14721543 His system of the world | 5 |
The priority of Herman and Euler in the matter of dAlemberts | 6 |
Transformation of Maxwells equations including convection | 11 |
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Загальні терміни та фрази
acceleration Albert of Saxony Archimedes Aristotle assumed axis Bernoulli Blasius of Parma Carnot centre of gravity classical mechanics concept conservation considered coordinates d'Alembert Daniel Bernoulli deduced Descartes differential direction displacement distance Duhem dynamics Earth Einstein elastic electron energy equal equations equilibrium Euler experiment fall Fermat fluid function Galileo generalised given heavy body Huyghens hypothesis impact impetus inclined plane inertia instant Jean Bernoulli Jordanus Kepler Lagrange least action Leibniz length Leonardo lever living forces Louis de Broglie mass Maupertuis means moving body natural necessary Newton observation obtained Oresme oscillation particle pendulum physical problem projectile proportional Proposition quantity of motion quantum mechanics ratio relation relative resistance rest Roberval rotation solution space sphere statics supposed surface theory trajectory travelled treatise uniformly variables velocity vertical wave weight XIIIth Century ди ду дх