Full text: The collected mathematical papers of Arthur Cayley, Sc.D., F.R.S., sadlerian professor of pure mathematics in the University of Cambridge (Vol. 6)

421 
412] 
A MEMOIR ON CUBIC SURFACES. 
or substituting for /3, y, 8 in the first and last lines their values 
this is 
(= x + z + w, xz + xw + zw, xziu), 
4«Y (y -®)(y- z) (y - w) 
+ a 2 {(12 7 - /3 2 ) y 4 - (8/3 7 + 368) f + (30/38 + 8 7 2 ) if - 36y8y + 278-} 
+ 2a {(6 7 2 - /3 2 7 - 9/38) f + (12/3 2 8 - 2/3 7 2 - 18 7 8) y + 2 7 3 + 278 2 - 9/3 7 8} 
— (x — zf (x — w) 2 (z — w)- = 0. 
123. The nodal curve is made up of the lines (y = x = z), (y = x = w), (y = z = w), 
reciprocals of the three transversals. 
To show this I remark that, writing 
/3' = (x - y) + (z - y) + (w - y), 
y = (as- y) (z-y) + (as- y) (w -y) + (z-y)(w - y), 
% =(v-y)(z-y)(w-y), 
the equation of the surface may be written 
4ci 3 f (y-x)(y-z) (y-w) 
+ a 2 [f (12/3'8' - 7 2 ) + x. 18 7 8' + 278' 2 } 
+ 2a {;y (- 6/3' 2 8' + 2/3V 2 + 9 7 '8') + 2 7 ' 3 + 278' 2 - 9/3' 7 '8'} 
— (x — z) 2 (« — w) 2 — ic) 2 = 0, 
whence observing that y is of the order 1 and S' of the order 2 in (x — y), (z — y) 
conjointly, each term of the equation is at least of the second order in (x — y), (z — y) 
conjointly; or we have y = x = z, a nodal line; and similarly the other two lines are 
nodal lines. 
124. The foregoing transformed equation is most readily obtained by reverting to 
the cubic in T, U, viz. writing p = x — y, r = z — y, s — io — y, and therefore x = y + p, 
z = y + r, w = y + s, the cubic function (putting therein T= V + yU) becomes 
a(V+yU) V* + (V-pU)(V-rU)(V-sU)-, 
writing /3', y, 8' = p + r + s, pr + ps + rs, prs, the coefficients are (3 (a + 1), ay - /3', y, — 38'), 
and the equation of the surface is thus obtained in the form 
27 (a + l) 2 8' 2 
+ 18 (a + 1) (ay - ¡3') y'8' 
+ 4(a + l) 7 ' 3 
— 4 (ay — (3'f 8' 
- (ay - ¡3J y' 2 = 0, 
which, arranging in powers of a, and reversing the sign, is the foregoing transformed 
result.
	        
Waiting...

Note to user

Dear user,

In response to current developments in the web technology used by the Goobi viewer, the software no longer supports your browser.

Please use one of the following browsers to display this page correctly.

Thank you.