A Collection of Problems in Illustration of the Principles of Theoretical Hydrostatics and Hydrodynamics |
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Page v
... Solids . Sect . I. - Homogeneous incompressible fluids II . Heterogeneous incompressible fluids CHAPTER III . Resultant pressures of fluids on curved surfaces of immersed solids CHAPTER IV . Equilibrium of Solid Bodies floating freely ...
... Solids . Sect . I. - Homogeneous incompressible fluids II . Heterogeneous incompressible fluids CHAPTER III . Resultant pressures of fluids on curved surfaces of immersed solids CHAPTER IV . Equilibrium of Solid Bodies floating freely ...
Page vi
William Walton. CHAPTER V. Equilibrium of Solid Bodies floating under constraint . Page Sect . I. - Incompressible homogeneous fluids II . - Incompressible heterogeneous fluids 65 69 CHAPTER VI . Specific gravity . 72 CHAPTER VII ...
William Walton. CHAPTER V. Equilibrium of Solid Bodies floating under constraint . Page Sect . I. - Incompressible homogeneous fluids II . - Incompressible heterogeneous fluids 65 69 CHAPTER VI . Specific gravity . 72 CHAPTER VII ...
Page vii
... Solid Bodies acted on by Fluids . Sect . I. - Finite vertical oscillations in incompressible fluids II . — Motion of bodies subject to the action of aeriform fluids III . - Small oscillations of floating bodies 186 194 215 218 221 ...
... Solid Bodies acted on by Fluids . Sect . I. - Finite vertical oscillations in incompressible fluids II . — Motion of bodies subject to the action of aeriform fluids III . - Small oscillations of floating bodies 186 194 215 218 221 ...
Page 1
... Solids . LET K denote any indefinitely small element of the surface of a solid immersed in a fluid , and let z represent the depth of K below the surface of the fluid ; then , g denoting the accelerating force of gravity and p the ...
... Solids . LET K denote any indefinitely small element of the surface of a solid immersed in a fluid , and let z represent the depth of K below the surface of the fluid ; then , g denoting the accelerating force of gravity and p the ...
Page 2
... solid is not known , and it cannot be subdivided into any finite number of areas of which the centres of gravity are known , the evaluation of the expression gpΣ ( Kx ) must be effected by means of the Integral Calculus . We have ...
... solid is not known , and it cannot be subdivided into any finite number of areas of which the centres of gravity are known , the evaluation of the expression gpΣ ( Kx ) must be effected by means of the Integral Calculus . We have ...
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Common terms and phrases
ABCD Albert Girard altitude angular velocity aperture axis axis of revolution axis vertical base Bernoulli Bossut Traité Cambridge centre of gravity centre of pressure cone constant quantity cos² Daniel Bernoulli denote the density denote the length denote the radius depth determine distance dx dy Edition elastic equal equation filled with fluid floating fluid displaced free surface given hemisphere Hence humidum inclination incompressible fluid integrating James Bernoulli John Bernoulli lamina latus rectum mass motion oscillation parabola paraboloid of revolution parallel particles Phoronomia portion position of equilibrium position of rest problem ratio represent right angles sesquialterum sin² small orifice solid cylinder specific gravity sphere supposed Traité d'Hydrodynamique Treatise triangle tube vertex volume w³y² weight whole pressure
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