A History of MechanicsRoutledge, 1955 - 671 стор. |
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Результати 1-3 із 64
Сторінка 56
... remains uncovered . " The weakness of this argument is clear . But undoubtedly the theory was in harmony with the belief , common at that time , in the existence of a terrestrial hemisphere completely covered by a vast ocean . It is ...
... remains uncovered . " The weakness of this argument is clear . But undoubtedly the theory was in harmony with the belief , common at that time , in the existence of a terrestrial hemisphere completely covered by a vast ocean . It is ...
Сторінка 160
... remains that Descartes ' contribution was not lasting and much less than that of Galileo , whose progress from 1604 to 1638 was conti- nuous . Moreover , Galileo had a respect for observation , which Des- cartes eschewed . 3. DESCARTES ...
... remains that Descartes ' contribution was not lasting and much less than that of Galileo , whose progress from 1604 to 1638 was conti- nuous . Moreover , Galileo had a respect for observation , which Des- cartes eschewed . 3. DESCARTES ...
Сторінка 328
... remains after the impact and the second is , consequently , necessarily destroyed by the impact . If only the first motion is imparted to the system , it will necess- arily be received without alteration . Under the influence of the ...
... remains after the impact and the second is , consequently , necessarily destroyed by the impact . If only the first motion is imparted to the system , it will necess- arily be received without alteration . Under the influence of 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 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