and when q is stationary, the acceleration is normal to the surface H
= constant, and the stream line is a geodesic.
Calling the sum of the pressure and potential head the statical head,
surfaces of constant statical and dynamical head intersect in lines on
H, and the three surfaces touch where the velocity is stationary.
Equation (3) is called Bernoulli's equation, and may be interpreted as
the balance-sheet of the energy which enters and leaves a given tube
of flow.
If homogeneous liquid is drawn off from a vessel so large that the
motion at the free surface at a distance may be neglected, then
Bernoulli's equation may be written
H = p/[rho] + z + q²/2g = P/[rho] + h, (8)
where P denotes the atmospheric pressure and h the height of the free
surface, a fundamental equation in hydraulics; a return has been made
here to the gravitation unit of hydrostatics, and Oz is taken
vertically upward.
In particular, for a jet issuing into the atmosphere, where p = P,
q²/2g = h - z, (9)
or the velocity of the jet is due to the head k - z of the still free
surface above the orifice; this is Torricelli's theorem (1643), the
foundation of the science of hydrodynamics.
27. _Uniplanar Motion._--In the uniplanar motion of a homogeneous
liquid the equation of continuity reduces to
du dv
-- + -- = 0, (1)
dx dy
so that we can put
u = -d[psi]/dy, v = d[psi]/dx, (2)
where [psi] is a function of x, y, called the stream- or
current-function; interpreted physically, [psi] - [psi]0, the
difference of the value of [psi] at a fixed point A and a variable
point P is the flow, in ft.³/second, across any curved line AP from A
to P, this being the same for all lines in accordance with the
continuity.
Thus if d[psi] is the increase of [psi] due to a displacement from P
to P´, and k is the component of velocity normal to PP´, the flow
across PP´ is d[psi] = k·PP´; and taking PP´ parallel to Ox, d[psi] =
vdx; and similarly d[psi]= -udy with PP´ parallel to Oy; and generally
d[psi]/ds is the velocity across ds, in a direction turned through a
right angle forward, against the clock.
In the equations of uniplanar motion
dv du d²[psi] d²[psi]
2[zeta] = -- - -- = ------ + ------ = -[Nabla]²[psi], suppose, (3)
dx dy dx² dy²
so that in steady motion
dH d[psi] dH d[psi] dH
-- + [Nabla]²[psi]------ = 0, -- + [Nabla]²[psi]------ = 0, ------ + [Nabla]²[psi] = 0, (4)
dx dx dy dy d[psi]
and [Nabla]²[psi] must be a function of [psi].
If the motion ia irrotational,
d[phi] d[psi] d[phi] d[psi]
u = - ------ = - ------, v = - ----- = ------, (5)
dx dy dy dx´
so that [psi] and [phi] are conjugate functions of x and y,
Public-domain text, read in full here on John Shaqi.
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