If we can make

(4[pi][rho]A + [alpha])x² = (4[pi][rho]B + [beta])b²

= (4[pi][rho]C + [gamma])c², (16)

the surfaces of equal pressure are similar to the external case, which

can then be removed without affecting the motion, provided [alpha],

[beta], [gamma] remain constant.

This is so when the axis of revolution is a principal axis, say Oz;

when

[Omega]1 = 0, [Omega]2 = 0, [xi] = 0, [eta] = 0. (17)

If [Omega]3 = 0 or [theta]3 = [zeta] in addition, we obtain the

solution of Jacobi's ellipsoid of liquid of three unequal axes,

rotating bodily about the least axis; and putting a = b, Maclaurin's

solution is obtained of the rotating spheroid.

In the general motion again of the liquid filling a case, when a = b,

[Omega]3 may be replaced by zero, and the equations, hydrodynamical

and dynamical, reduce to

d[xi] 2c² d[eta] 2a²

----- = - -------[Omega]2 [zeta], ------ = -------[Omega]1 [zeta],

dt a² + c² dt a² + c²

d[zeta] 2c²

------- = -------([Omega]2 [xi] - [Omega]2 [eta]) (18)

dt a² + c²

d[Omega]1 a² + c²

--------- = [Omega]2 [zeta] + -------[eta][zeta],

dt a² - c²

d[Omega]2 a² + c²

--------- = [Omega]1 [zeta] + -------[xi][zeta]; (19)

dt a² - c²

of which three integrals are

a²

[xi]² + [eta]² = L - --[zeta]², (20)

c²

(a² + c²)²

[Omega]1² + [Omega]2² = M + ------------ [zeta]², (21)

2c²(a² - c²)

a² + c²

[Omega]1 [xi] + [Omega]2 [eta]N = + ------- [zeta]²; (22)

4c²

and then

/ d[zeta]\² 4c^4

( ------- ) = --------- ([Omega]2[xi] - [Omega]1²[eta])²

\ dt / (a² + c²)

4c^4

= ---------- [([xi]² + [eta]²)([Omega)1² + [Omega]2²) -([Omega]1[xi] + [Omega]2[eta])²]

(a² + c²)²

_

4c^4 | / (a² + c²)² a² (a² + c²)\

= ---------- | LM - N² + ( L------------ - M --- - N --------- ) [zeta]²

(a² + c²)² |_ \ 2c²(a² + c²) c² 2c² /

_

(a² + c²)(9a² - c²) |

- ------------------- [zeta]^4 | = Z, (23)

16c^4(a² - c²) _|

where Z is a quadratic in [zeta]², so that [zeta] is an elliptic

function of t, except when c = a, or 3a.

Put [Omega]1 = [Omega] cos [phi], [Omega]2 = -[Omega] sin [phi],

d[phi] d[Omega]1 d[Omega]2 (a² + c²)

[Omega]2 ------ = -----------[Omega]2 - [Omega]1 --------- = [Omega]²[zeta] - ---------([Omega]1 [xi] + [Omega]2 [eta])[zeta], (24)

dt dt dt (a² - c²)

a² + c²

N + -------

d[phi] (a² + c²) 4c²

------ = [zeta] - --------- · -------------------------, (25)

dt (a² - c²) (a² + c²)²

M + ------------[zeta]²

2c²(a² - c²)

a² + c²

_ _ N + -------[zeta]²

/ [zeta]d a² + c² / 4c² [zeta] d[zeta]

[phi] = | ------- - ------- | ------------------------ · --------------, (26)

_/ [root]Z a² - c² _/ (a² + c²)² [root]Z

M + ------------[zeta]²

2c²(a² - c²)

which, as Z is a quadratic function of [zeta]², are non-elliptic

integrals; so also for [psi], where [xi] = [omega] cos [psi], [eta] =

-[omega] sin [psi].

Encyclopaedia Britannica, 11th Edition, "Hydromechanics" to "Ichnography" Volume 14, Slice 2 · 第 51 / 120 题