A History of MechanicsRoutledge & Paul, 1957 - 671 стор. |
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Результати 1-3 із 81
Сторінка 62
... measure has the same measure as the uniformly deformed quality represented by the triangle ACB , because the area ACB is equal to the area AFGB . Oresme declares , Any uniformly deformed quality or velocity is thus found to be ...
... measure has the same measure as the uniformly deformed quality represented by the triangle ACB , because the area ACB is equal to the area AFGB . Oresme declares , Any uniformly deformed quality or velocity is thus found to be ...
Сторінка 236
... measure . This common measure is the time ; at least I can take the time or the times to be equal . . . . " Now given this , in the effects of a body which has twice as much velocity , I only find an effect which is double and not ...
... measure . This common measure is the time ; at least I can take the time or the times to be equal . . . . " Now given this , in the effects of a body which has twice as much velocity , I only find an effect which is double and not ...
Сторінка 621
... measure A , at the time t = 0 and find the result a2 , we are able to predict with certainty that x will have the same value for t = tą . But it is essential that the simultaneous measurement of A1 and A is impossible . Indeed , it is ...
... measure A , at the time t = 0 and find the result a2 , we are able to predict with certainty that x will have the same value for t = tą . But it is essential that the simultaneous measurement of A1 and A is impossible . Indeed , it is ...
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