A Collection of Problems in Illustration of the Principles of Theoretical Hydrostatics and Hydrodynamics |
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Page 14
... unit of pressure of the fluid at the area K ; then pK will repre- sent the pressure of the fluid on K , and the magnitude of the pressure on the whole surface of the solid will be equal to Σ ( Kp ) , where Σ denotes the summation of a ...
... unit of pressure of the fluid at the area K ; then pK will repre- sent the pressure of the fluid on K , and the magnitude of the pressure on the whole surface of the solid will be equal to Σ ( Kp ) , where Σ denotes the summation of a ...
Page 16
... , below the upper surface of the th fluid . Then , p being the unit of pressure at the annulus , p = g ( p1 a1 + P2 a2 + Pz Az + ... + P2 - 1 a ̧ - 1 ) + gp2 z : • but , the masses of the several fluids being 16 NORMAL PRESSURE OF FLUIDS .
... , below the upper surface of the th fluid . Then , p being the unit of pressure at the annulus , p = g ( p1 a1 + P2 a2 + Pz Az + ... + P2 - 1 a ̧ - 1 ) + gp2 z : • but , the masses of the several fluids being 16 NORMAL PRESSURE OF FLUIDS .
Page 22
... unit of pressure of the fluid at the centre of the envelope , and let a denote its radius ; then the required pressure will be equal to Σπαβ . ( ελα – ελα ) . λ If λ be a very small quantity , then , supposing a not to be large , this ...
... unit of pressure of the fluid at the centre of the envelope , and let a denote its radius ; then the required pressure will be equal to Σπαβ . ( ελα – ελα ) . λ If λ be a very small quantity , then , supposing a not to be large , this ...
Page 23
... unit of pressure of the fluid , viz . B. 4. A fluid being supposed to consist of an indefinite number of particles at finite intervals , and the repulsive force between two neighbouring particles being supposed to vary inversely as the ...
... unit of pressure of the fluid , viz . B. 4. A fluid being supposed to consist of an indefinite number of particles at finite intervals , and the repulsive force between two neighbouring particles being supposed to vary inversely as the ...
Page 35
... unit of pressure vary discontinuously , we must subdivide the fluid into a series of horizontal strata , such that the law of the variation of the density and unit of pressure shall be continuous throughout each of them . We must then ...
... unit of pressure vary discontinuously , we must subdivide the fluid into a series of horizontal strata , such that the law of the variation of the density and unit of pressure shall be continuous throughout each of them . We must then ...
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Common terms and phrases
Albert Girard altitude angular velocity aperture axem axes axis vertical base Bernoulli body Bossut Bossut Traité Cambridge centre of gravity centre of pressure coinciding cone cos² cube Daniel Bernoulli denote the density denote the length depth determine distance dx dy Edition efflux elastic equal equation filled with fluid floating fluid displaced force free surface given hemisphere Hence humidum Hydrodynamique immersed vertically inclination incompressible fluid James Bernoulli lamina late Fellow latus rectum motion parabola parallel particles portion position of equilibrium position of rest problem quæ ratio required pressure resultant pressure right angles sesquialterum sin² small orifice solid cylinder specific gravity sphere supposed tangent Treatise triangle Trinity College unit of pressure University of Cambridge vertex vertical line vessel volume weight whole pressure
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Page 11 - The Greek Testament : with a critically revised Text ; a Digest of Various Readings ; Marginal References to Verbal and Idiomatic Usage ; Prolegomena ;"and a Critical and Exegetical Commentary. For the Use of Theological Students and Ministers. By HENRY ALFORD, DD, Dean of Canterbury. Vol. I., containing the Four Gospels.
Page 17 - Wilson's Illustration of the Method of explaining the New Testament, by the early opinions of Jews and Christians concerning Christ.
Page 23 - FREDERICK M<CoY, FGS, Hon. FCPS, Professor of the Natural Sciences in the University of Melbourne; formerly Professor of Geology and Mineralogy in the Queen's University in Ireland; author of "Characters of the Carboniferous Limestone Fossils of Ireland;" " Synopsis of the Silurian Fossils of Ireland ;" "Contributions to British Palaeontology,
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