A History of MechanicsRoutledge & Paul, 1957 - 671 стор. |
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Результати 1-3 із 93
Сторінка 55
... Earth alone may be understood equally for the whole aggre- gate formed by the Earth and the waters . These two elements undoub- tedly form a total and unique gravity whose centre of gravity is at the centre of the World . " At this same ...
... Earth alone may be understood equally for the whole aggre- gate formed by the Earth and the waters . These two elements undoub- tedly form a total and unique gravity whose centre of gravity is at the centre of the World . " At this same ...
Сторінка 63
... Earth is moved diurnally just as , to us on the Earth , the Heavens seem to move . And similarily , if the Earth is moved with a diurnal motion and the Heavens not , it will seem to us that the Earth is still and that the Heavens move ...
... Earth is moved diurnally just as , to us on the Earth , the Heavens seem to move . And similarily , if the Earth is moved with a diurnal motion and the Heavens not , it will seem to us that the Earth is still and that the Heavens move ...
Сторінка 85
... Earth . We shall quote from Copernicus ' De revolutionibus orbium caelestium . " The Earth is spherical because , on all sides , it strives towards the centre . The element of the Earth is the heaviest of all , and all heavy bodies are ...
... Earth . We shall quote from Copernicus ' De revolutionibus orbium caelestium . " The Earth is spherical because , on all sides , it strives towards the centre . The element of the Earth is the heaviest of all , and all heavy bodies are ...
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