F²(X² + Y²) = y1² + y2² + y3² - G², (21)

Fy3 - Gx3 + i[root]X3

F(X + Yi) = --------------------- [epsilon]^[psi]_i. (22)

[root](F² - x3²)

Suppose x3 - F is a repeated factor of X3, then y3 = G, and

_ _

| p´ - p q´ - q |

X3 = (x3 - F)² | ------(x3 + F)² + 2------G(x3 + F) - G² |, (23)

|_ r r _|

and putting x3 - F = y,

_

/ dy \² | p´ - p q´ - q

( -- ) = r²y² | 4 ------ F² + 4 ------ FG - G²

\ dt / |_ r r

_

/ p´ - p q´ - q \ p´ - p |

+ 2 ( 2 ------ F + ------ G ) y + ------ y² |, (24)

\ r r / r _|

so that the stability of this axial movement is secured if

p´ - p q´ - q

A = 4 ------F² + 4 ------FG - G² (25)

r r

is negative, and then the axis makes r[V-](-A)/[pi] nutations per

second. Otherwise, if A is positive

_

/ dy

rt = | ----------------------

_/ y[root](A + 2By + Cy²)

1 sh^(-1) [root]A[root](A + 2By + Cy²) 1 ch^(-1) A + By

= ------- ---------------------------- = ------- ---------------, (26)

[root]A ch^(-1) y[root](B² ~ AC) [root]A sh^(-1) y[root](B² ~ AC)

and the axis falls away ultimately from its original direction.

A number of cases are worked out in the American Journal of

Mathematics (1907), in which the motion is made algebraical by the use

of the pseudo-elliptic integral. To give a simple instance, changing

to the stereographic projection by putting tan ½[theta] = x,

(Nxe[psi]i)^3/2 = (x + 1)[root]X1 + i(x - 1)[root]X2, (27)

X1

-- = ±ax^4 + 2ax³ ± 3(a + b)x² + 2bx ± b, (28)

X2

Encyclopaedia Britannica, 11th Edition, "Hydromechanics" to "Ichnography" Volume 14, Slice 2 · 第 71 / 120 题