A History of MechanicsRoutledge, 1955 - 671 стор. |
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Сторінка 23
... taken to the ends of the World be allowed to reunite at the centre ; let the Earth be formed by a different procedure - the result will be exactly the same . If the parts are taken to the ends of the World and are taken there similarily ...
... taken to the ends of the World be allowed to reunite at the centre ; let the Earth be formed by a different procedure - the result will be exactly the same . If the parts are taken to the ends of the World and are taken there similarily ...
Сторінка 143
... taken it as a principle in his Pro- blems of Mechanics . Hence the assertion , that two weights of unequal size are in equilibrium with each other , and have equal momenti , when- ever their gravities are in inverse ratio to the ...
... taken it as a principle in his Pro- blems of Mechanics . Hence the assertion , that two weights of unequal size are in equilibrium with each other , and have equal momenti , when- ever their gravities are in inverse ratio to the ...
Сторінка 153
... taken on the line of the direction of the weight , the line parallel to one of the strings is drawn to the other string , the sides of the triangle thus formed will be homologous to the weight and the two powers . 99 It is interesting ...
... taken on the line of the direction of the weight , the line parallel to one of the strings is drawn to the other string , the sides of the triangle thus formed will be homologous to the weight and the two powers . 99 It is interesting ...
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