A Treatise on Physics ...E. A. Churchill, 1901 |
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Outras edições - Ver todos
A Treatise on Physics: Dynamics and properties of matter, Volume 1 Andrew Gray Visualização completa - 1901 |
A Treatise on Physics: Dynamics and properties of matter, Volume 1 Andrew Gray Visualização completa - 1901 |
Termos e frases comuns
acceleration angular velocity applied forces attraction axes axis balls body Boyle's law called centre centroid circle co-ordinates component consider constant couple cross-section curvature curve cylinder denote density direction displacement distance drawn earth element ellipse ellipsoid equal equation equilibrium equipotential surface external field-intensity fixed fluid friction funicular given gravity Hence horizontal inertia instant interval invariable plane inverse kinetic energy length liquid Lord Kelvin mass matter mercury moment of inertia momentum moon motion moving normal normal force obtained orbit parallel particle pendulum perpendicular plane plate position potential pressure produced quantity radius radius-vector ratio resultant right angles rotation round side simple harmonic motion space specific gravity sphere spherical strain stress suppose surface taken tangent theorem tidal tide tion tube uniform unit vertical vibration weight wire zero
Passagens mais conhecidas
Página 495 - The squares of the periods of revolution of any two planets are proportional to the cubes of their mean distances from the sun.
Página 177 - ... is the ratio of the specific heat at constant pressure to the specific heat at constant volume, is a constant.
Página 104 - Every body continues in its state of rest, or of uniform motion in a straight line, except in so far as it may be compelled to change that state by forces impressed upon it.
Página 497 - ... density that causes sound to pass rapidly through them. "Other things remaining the same, an augmentation of density always produces a diminution of velocity.
Página 4 - American inches, a standard of linear measure supposed to be the ten-millionth part of the distance from the equator to the north pole, as ascertained by actual measurement of an arc of the meridian.