Transactions of the Cambridge Philosophical Society, المجلد 22University Press, 1923 |
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الصفحة 44
... velocity . Since the relative magnitudes of Ra and M are so disproportionate , the slightest error in this adjustment , even if the line of action of R " be only To of an inch out , causes a considerable percentage error in the measured ...
... velocity . Since the relative magnitudes of Ra and M are so disproportionate , the slightest error in this adjustment , even if the line of action of R " be only To of an inch out , causes a considerable percentage error in the measured ...
الصفحة 46
... velocity at the surface of the journal . The pressure p is of course given in poundals per square foot . The first row of the double sets of data comprises those obtained by obser- vation , the second row those calculated from the ...
... velocity at the surface of the journal . The pressure p is of course given in poundals per square foot . The first row of the double sets of data comprises those obtained by obser- vation , the second row those calculated from the ...
الصفحة 47
... velocity increases ; ( 2 ) the position of the maximum pressure is displaced nearer to the point of closest approach ; ( 3 ) the position of the minimum pressure is displaced further from that point . Steady Flow of Air under Pressure ...
... velocity increases ; ( 2 ) the position of the maximum pressure is displaced nearer to the point of closest approach ; ( 3 ) the position of the minimum pressure is displaced further from that point . Steady Flow of Air under Pressure ...
الصفحة 53
... velocity the fall of the minimum pressure below atmospheric pressure is the same as the rise of the maximum pressure above , yet the effect of elasticity is to make the rise of the maximum pressure above atmospheric pressure greater ...
... velocity the fall of the minimum pressure below atmospheric pressure is the same as the rise of the maximum pressure above , yet the effect of elasticity is to make the rise of the maximum pressure above atmospheric pressure greater ...
الصفحة 54
... velocity , while its position approaches continuously to C ; ultimately the pressure reaches a maximum at B and then falls continuously to atmospheric pressure at C. The behaviour of the air , therefore , for large velocities is in ...
... velocity , while its position approaches continuously to C ; ultimately the pressure reaches a maximum at B and then falls continuously to atmospheric pressure at C. The behaviour of the air , therefore , for large velocities is in ...
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a₁ angle approximately asymptotic expansion atmosphere Axiom of Archimedes axis b₁ c₁ calculated coefficients considered constant convergent convex set cordon corresponding cos² curve d₁ definition denote density determined differential equations disturbance diurnal diurnal variations dyadic earth equal escape expression factor finite follows formula free path function G. H. Hardy giant star given h₂ Hence integral equation invariant Jacobian k₁ k₂ magnitude molecules obtained orbit paper parameters partitions plane positive potential Primitive Roots ratio relation respectively result rotation scalar shew shewn sin² solar solid angle solutions substitution suppose surface t₁ theorem theory v₁ values vector velocity w₁ X₁ XXII zero Σ Σ дх