A History of MechanicsRoutledge, 1955 - 671 стор. |
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Результати 1-3 із 75
Сторінка 29
... fluid with part of it above the surface . Let the fluid be at rest . Suppose that a plane which passes through the centre of the Earth intersects the fluid and the A B H x ז M R N S P D K Fig . 3 body immersed in it in such a way that ...
... fluid with part of it above the surface . Let the fluid be at rest . Suppose that a plane which passes through the centre of the Earth intersects the fluid and the A B H x ז M R N S P D K Fig . 3 body immersed in it in such a way that ...
Сторінка 30
... fluid contained in XO are compressed by the body EHTF and also by the fluid contained by the surfaces LM , XO and those of the pyramid . The parts contained in PO are compressed by the solid RSQY and by the fluid contained by the ...
... fluid contained in XO are compressed by the body EHTF and also by the fluid contained by the surfaces LM , XO and those of the pyramid . The parts contained in PO are compressed by the solid RSQY and by the fluid contained by the ...
Сторінка 297
... fluid , and the fluid will run along the forward surface as far as the point at which dy again becomes parallel to the axis . " With regard to the backward part , it seems at first sight that the motion must be different from that at ...
... fluid , and the fluid will run along the forward surface as far as the point at which dy again becomes parallel to the axis . " With regard to the backward part , it seems at first sight that the motion must be different from that at ...
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