It is convenient to introduce the function

[Omega] = log [zeta] = log(Q/q) + [theta]i (4)

so that the polygon representing [Omega] conformally has a boundary

given by straight lines parallel to the coordinate axes; and then to

determine [Omega] and w as functions of a variable u (not to be

confused with the velocity component of q), such that in the conformal

representation the boundary of the [Omega] and w polygon is made to

coincide with the real axis of u.

[Illustration: FIG. 4.]

It will be sufficient to give a few illustrations.

Consider the motion where the liquid is coming from an infinite

distance between two parallel walls at a distance xx´ (fig. 4), and

issues in a jet between two edges A and A´; the wall xA being bent at

a corner B, with the external angle [beta] = ½[pi]/n.

The theory of conformal representation shows that the motion is given

by

_ _

| [root](b - a´·u - a) + [root](b - a·u - a´) |^1/n

[zeta] = | ------------------------------------------- | , u = ae^(-[pi]w/m); (5)

|_ [root](a - a´·u - b) _|

where u = a, a´ at the edge A, A¹; u = b at a corner B; u = 0 across

xx´ where [phi] = [oo]; and u = [oo], [phi] = [oo] across the end JJ´

of the jet, bounded by the curved lines APJ, A´P´J´, over which the

skin velocity is Q. The stream lines xBAJ, xA´J´ are given by [psi] =

0, m; so that if c denotes the ultimate breadth JJ´ of the jet, where

the velocity may be supposed uniform and equal to the skin velocity Q,

m = Qc, c = m/Q.

If there are more B corners than one, either on xA or x´A´, the

expression for [zeta] is the product of corresponding factors, such as

in (5).

Restricting the attention to a single corner B,

/ Q \^n [root](b - a´·u - a) + [root](b - a·u - a´)

[zeta]^n = ( --- ) (cos n[theta] + i sin n[theta] = -------------------------------------------, (6)

\ q / [root](a - a´.u - b)

/ Q \^n / Q \^n

ch n[omega] = ch log( --- ) cos n[theta] + i sh log ( --- ) sin n[theta]

\ q / \ q /

/b - a´ /u - a´

= ½([zeta]^n + [zeta]^(-n)) = / ------ / ------ (7)

\/ a - a´ \/ u - b´

/ Q \ / Q \^n

sh n[Omega] = sh log ( --- ) cos n[theta] + i ch log ( --- ) sin n[theta]

\ q / \ q /

/b - a´ /u - a´

= ½([zeta]^n - [zeta]^(-n)) = / ------ / ------ (8)

\/ a - a´ \/ u - b´

[oo] > a > b > 0 > a´ > -[oo] (9)

and then

d[Omega] 1 [root](b - a´·b - a´) dw m

-------- = - -- ---------------------------, -- = - ------ (10)

du 2n (u - b)[root](a - a·u - a´) du [pi]u´

the formulas by which the conformal representation is obtained.

For the [Omega] polygon has a right angle at u = a, a´, and a zero

angle at u = b, where [theta] changes from 0 to ½[pi]/n and [Omega]

increases by ½i[pi]/n; so that

d[Omega] A [root](b - a·b - a´)

-------- = ---------------------------, where A = --------------------. (11)

du (u - b)[root](u - a·u - a´) 2n

And the w polygon has a zero angle at u = 0, [oo], where [psi] changes

from 0 to m and back again, so that w changes by im, and

dw B m

-- = ---, where B = - ----. (12)

du u [pi]

Along the stream line xBAPJ,

[psi] = 0, u = ae^(-[pi][phi]/m); (13)

and over the jet surface JPA, where the skin velocity is Q,

d[phi]

------ = -q = -Q, u = ae^([pi]sQ/m) = ae^([pi]s/c), (14)

ds

denoting the arc AP by s, starting at u = a;

/b - a´ /u - a´

ch n[Omega] = cos n[theta] = / ----- / ------ (15)

\/ a - a´ \/ u - b´

/a - b /u - a´

sh n[Omega] = i sin n[theta] = i / ------ / ------ (16)

\/ a - a´ \/ u - b´

[oo] > u = ae^([pi]s/c) > a, (17)

and this gives the intrinsic equation of the jet, and then the radius

of curvature

ds 1 d[phi] i dw i dw / d[Omega]

[rho] = - -------- = --- -------- = --- ------- = --- -- / -------

d[theta] Q d[theta] Q d[Omega] Q du / du

c u - b [root](u - a·u - a´)

= ----·2n----- --------------------, (18)

[pi] u [root](a - b·b - a´)

not requiring the integration of (11) and (12)

If [theta] = [alpha] across the end JJ´ of the jet, where u = [oo], q

= Q,

/b - a´ /a - b

ch n[Omega] = cos n[alpha] = /-------, sh n[Omega] = i sin n[alpha]= / ------, (19)

\/ a - a´ \/ a - a´

Encyclopaedia Britannica, 11th Edition, "Hydromechanics" to "Ichnography" Volume 14, Slice 2 · 第 53 / 120 题