systems of quadrics associated with a point of a surface

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Systems of Quadrics Associated with a Point of a Surface Author(s): Louis Green Source: American Journal of Mathematics, Vol. 60, No. 3 (Jul., 1938), pp. 649-666 Published by: The Johns Hopkins University Press Stable URL: http://www.jstor.org/stable/2371604 . Accessed: 06/12/2014 00:01 Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at . http://www.jstor.org/page/info/about/policies/terms.jsp . JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. . The Johns Hopkins University Press is collaborating with JSTOR to digitize, preserve and extend access to American Journal of Mathematics. http://www.jstor.org This content downloaded from 142.51.1.212 on Sat, 6 Dec 2014 00:01:11 AM All use subject to JSTOR Terms and Conditions

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Page 1: Systems of Quadrics Associated with a Point of a Surface

Systems of Quadrics Associated with a Point of a SurfaceAuthor(s): Louis GreenSource: American Journal of Mathematics, Vol. 60, No. 3 (Jul., 1938), pp. 649-666Published by: The Johns Hopkins University PressStable URL: http://www.jstor.org/stable/2371604 .

Accessed: 06/12/2014 00:01

Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at .http://www.jstor.org/page/info/about/policies/terms.jsp

.JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range ofcontent in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new formsof scholarship. For more information about JSTOR, please contact [email protected].

.

The Johns Hopkins University Press is collaborating with JSTOR to digitize, preserve and extend access toAmerican Journal of Mathematics.

http://www.jstor.org

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Page 2: Systems of Quadrics Associated with a Point of a Surface

SYSTEMS OF QUADRICS ASSOCIATED WITH A POINT OF A SURFACE.*

By Louis GREEN.

1. Introduction. One of the popular methods of studying the local geometry of an analytic surface immersed in a three-dimensional projective space is to examine the properties of algebraic osculants. For, these osculants can be used to obtain simple characterizations of many elements intimately related to the given surface. The osculating quadrics at a point of a surface are of particular importance in this respect, and it is the purpose of this paper to make a more comprehensive study of certain of these quadrics, obtaining as a result significant properties of the surface.

Among other things, the problem of determining the envelope of a two- parameter family of Moutard quadrics is solved, the singularity of the curve of intersection of the surface and one of its Moutard quadrics is investigated, certain individual members of each Moutard pencil of quadrics 1 are char- acterized, and three new pencils of quadrics which we call the Darboux-Segre pencils of quadrics are defined and discussed.

2. Analytic basis. The local co6rdinate tetrahedron of G. M. Green (with a modified unit point) is taken as the projective co6rdinate system throughout this paper, and the equations of the various configurations to be used are obtained in this section by transformation from Fubini's coordinate system.

Fubini's canonical differential equations of an analytic curved surface S are given by

x-upx + Ouxu +I3xv, Xvv = qX + yXu + 6vxv, (O = log/3y).

Let 0 be an ordinary point of S, chosen as the vertex (1, 0, 0, 0) of two local tetrahedrons, one of Fubini and the other of Green. If a point of the ambient three-space has the two sets of coordinates (xl, * *, X4), (Xl, * * *, X4)

relative to these respective tetrahedrons, then the following relations exist: 2

* Presented to the Society, April 9, 1937. Received by the Editors October 30, 1937. 1 So called because each of these pencils contains a quadric of Moutard. These

pencils were first studied by Su and Ichida, Japanese Journal of Mathematics, vol. 10 (1933), pp. 209-216.

2Lane, " Power series expansions in the neighborhood of a point on a surface," Proceedings of the National Academy of Sciences, vol. 13 (1927), pp. 808-813.

649

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Page 3: Systems of Quadrics Associated with a Point of a Surface

650 LOUIS GREEN.

X= 4X2 + 3lc1X2 + 3mIfX3 + (9/4)n(p/ - OUV) X2 -121X2- 9nm X4, X3 -12mX3 9nc X4, X4 36nX4,

where 1, m, n, p, 1, have the values

-/ l(/32y)1/3, m =-/(/3y2)1/3 n I lm,

'i (log/ly2)f, *g =_ (log &2y)V.

With the introduction of non-homogeneous coordinates X, Y, Z defined in the customary way, 0 becomes the origin of a local non-homogeneous coordinate system, and the co6rdinates of a point on S sufficiently "near" 0 satisfy a convergent power series expansion of the form

(2) Z =XY+X3 + Y3 +AX3Y+BXY3+ COX5 +01X4Y + C2 X3Y2 + C3X2Y3 + C4XY4 + C5Y5 + ,

where all the coefficielnts are absolute invariants of the surface, and in particular,

A = -3mf/2, B - 31P/2,

20CO 3612p - 912ku - 27m'1 - (9/4) l2ci2 + 912O,(po

16C= 24nfr, - 12n4)v + 135nmq4 - 135, (3) 16C2=- 135m2q + 72m2,/V + 27m2./2 -18014) + 72m2,r(83V/1),

1603 = - 1312p + 7212,+ + 2712p2 180mf + 7212p(-y/y), 16C4 24n4v - 12n*t' + 135m4(/ - 135, 20C5 36m2q - 9M2V 2710 - (9/4)m2t/2 + 9m2A&OV.

For use in ? 7 the formulas for the derivatives of the local co6rdinates XI, *- , X4 will now be obtained. Equations (1) are first solved for the Xi, the resulting equations are then diffferentiated with respect to u (v), and the xi (xi,) which appear are replaced by their known values 3 in terms of the xi. The right members are then expressed in terms of the Xi by means of (1), and when simplified with the use of (3) take the form

361X1u 6BX, + (60Co -72A)X2 + (12C4 -45AB + 108)X3 + (36C2 - 108B - 54A2)X4,

36lX2U = 12X1 + 2BX2 + (120,- 45AB + 216) X4,

361X3U = - 36X2 - 2BX3 + (60Co - 108A)X4,

361X4U =12X3 6BX4; (4) 36mXv = 6AX, + (12C, -45AB + 108)X2 + (60C5 -72B)X3

+ (36C3- 108A - 54B2)2X4, 36mX2V - 2AX2 - 36X3 + (60C5 - 108B)X4,

36mX3V 12X1 + 2AX3 + (12C, -45AB + 216))X4, 36mX4V 12X2 - 6AX4.

3 Lane, Projective Differential Geometry of Curves and Surfaces, Chicago, 1932, p. 111.

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Page 4: Systems of Quadrics Associated with a Point of a Surface

SYSTEMS OF QUAIDRICS ASSOCIATED WITH A POINT OF A SURFACE. 651

By means of transformation (1) all the remaining results of this section are readily established.

The tangents of Darboux through 0 are given by

X2 3+ X33 0 =4;

the equation of a quadric of Darboux,

X2X3 -iX4 + hx42 0 (h h(u,v) ), becomes (5) X2X3 -X1X4 + KX42 0, K (9/23y) (Ouv + 2h);

the equations of a canonical line of the second kind,

Xi - PX2 - k7bX3 0 = 4,

have the form

x1- (B/2) (1 + 4k)X2- (A/2) (1 + 47c) X3 0 =X4,

and its polar line with respect to a quadric of Darboux joins 0 to the point

(O, (A/2) (1 + 4k), (B/2) (1 + 4k), 1)-

If the corresponding equations of a plane in the above-mentioned co6rdi- nate systems are

4 4

1 1

then the transformation of Cech in Fubini's system,

pXl =234 - j(723 + 3 3), pX2 = 2t32,

pX3 - 223 X4 - 0 (j = const.),

is expressed in Green's system by the equations

UX1 = 2q3q4 + 3j(q23+ q3%), X2 =- 2q3, 013 -2 23, X4 0.

A curve on S which passes through 0 in a non-asymptotic direction and satisfies the differential equation

dv -du 0 (= (u, v)),

has for its osculating plane at 0 the plane represented by

2X(XX2 -X3) + ( -yX3 -OU + 0VX2 + X')x4=-O (A'= vf x + XXv).

Under transformation of co6rdinates (1) this equation becomes

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Page 5: Systems of Quadrics Associated with a Point of a Surface

652 LOUIS GREEN.

(6) 61 (JX2-X3) + (9X3 _9 + AP-2 B- 9')X4 =0,

where ,u, 11', are defined by

(7) = Xl/m, I" l(y + /V) =- i/u + m/v

The osculating plane at 0 of the pangeodesic which passes through this point in a non-Darboux direction X3/X2 = # is expressed by

(8) 2(3+ 1) (X2 -X3) + (3,6- 3 + Ai2-B,B4)X4 O,

and the quadric of Moutard in the non-asymptotic direction ,k at 0 has the equation

(9) P3 (X2X3 - X1X4) + p2(2 -3)X2X4 + p (2/3 _) )X3X4

+ (Ag2 + B4 -6-23 _1)X42 0.

3. The curve of intersection of a surface and a quadric. The equation of the most general quadric having second-order contact with the surface S at the point 0 is

(10) XY-Z + K2XZ + K3YZ + K4Z2 0,

where K2, K3, K4 are arbitrary functions of u and v. The curve of inter- section C of this quadric and S is expressed by (10) and

(11) 0 X3- K2X2Y- K3XY2 + Y3 + (A-K22)X3Y -(2K2K3 + K4)X2Y2 + (B-K32)XY3 +

the latter equation being obtained by solving (10) for Z as a power series in X,. Y and then subtracting from (2). The curve C has a triple-point at 0 with triple-point tangents satisfying the equations

(12) X3- K2X2Y- K3XY2 + Y3 0 =Z.

Comparison of equations (10) and (12) leads to the following conclusion:

Two arbitrary non-asymptotic tangents to S at 0 determine a pencil of quadrics having second-order contact with S at 0 and meeting S in a one- parameter family of curves each containing these tangents as two of its triple-

point tangents. The residual tangent at 0 is the same for all the curves of the family.

A particular quadric of such a pencil is uniquely determined, ordinarily, by characterizing the osculating plane at 0 of any one of the three branches of the curve C.4

4The Moutard pencils of quadrics are the only pencils for which this is not the case. But, as is shown in ?? 5, 6, for such a pencil of quadrics in a direction , the

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Page 6: Systems of Quadrics Associated with a Point of a Surface

SYSTEMS OF QUADRICS ASSOCIATED WITH A POINT OF A SURFACE. 653

Several particular examples of the above theorem are worth noting. If two of the triple-point tangents lie in distinct Darboux directions at 0, the third tangent must lie in the residual Darboux direction and the resulting quadrics are the quadrics of Darboux.

If two of the tangents coincide in a non-asymptotic direction X3/X2 , the third must lie in the direction _

1/J2, and the quadrics determined form the Moutard pencil of quadrics in the direction p. If p3 = - 1 the triple- point tangents all coincide in one of the Darboux directions, while if A3= 1

two of the tangents coincide in a Segre direction and the third tangent lies in the conjugate Darboux direction.

If two of the tangents lie in distinct Segre directions, the third is seen to lie in that Darbouxi direction which is conjugate to the residual Segre direction. Every Darboux direction thus determines a different pencil of such quadrics, so that each of the three pencils -may be designated as the Darboux- Segre pencil of quadrics in the particular Darboux direction considered.

The Darboux quadrics and the three Darboux-Segre pencils of quadrics are special cases of the pencil

XY-Z 3

+ 1x

k 3

+ 1YZ + K4Z2 0 (K4 arbitrary),

which is deternmined by the tangents in the directions AO, -2 /k2, where U is a primitive cube root of unity.

The quadrics of Darboux are thus seen to constitute the only pencil which can be determined by three tangents apolar to the asymptotic tangents at 0. Similarly, there exists a unique triple of tangents apolar to a given pair of conjugate tangents X3/X2 = L ,4 = 0, which according to the above theorem can determine a pencil of quadrics. These quadrics, whose equations can be shown to have the form

XY - Z - 392XZ - (3/2) YZ + K4Z2 = 0, (K4 arbitrary),

were defined by Davis 5 in an entirely different manner.

4. Quadrics associated with the tangents of Darboux and of Segre. The theorem of the last section is applied here to the quadrics of Darboux, the Moutard pencils in the Segre directions, and the Darboux-Segre pencils of quadrics.

osculating plane at 0 of a properly chosen branch of C does determine a unique quadric of the pencil, except when , is a Darboux direction. In this latter case the osculating plane at 0 of each of the three branches of C coincides with the tangent plane to X, unless the quadric is the quadric of Moutard of the pencil.

6 "Contributions to the theory of conjugate nets," Chicago Dissertation (1933), p. 12.

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Page 7: Systems of Quadrics Associated with a Point of a Surface

654 LOUIS GREEN.

The surface S and an arbitrary quadric of Darboux with parameter K meet in a curve C whose three branches are representable, as is seen from (2) and (5), by the series

Y _ -,E. + 1 (A E,2 + Be, + K) X2 + MX3+**,

Z --EX2 + 3 (Ac,2 + BE +K)X3+ 1(i= ,2,3),

where 5

_9E,2M 2ABEi + 2B2 + AK + 3BKE,2 + K2,E + 3 E Cj (-et) j-O

(13) 'El = I, E2 - (0, IE3 602

and X is a primitive cube root of unity. The osculating plane at 0 of each branch of C has the equation

(14) 2 X + Eiy + (AE2 + BE + K)Z = 0,

from which it follows that these osculating planes are coaxial if, and only if, the given quadric is the quadric of Wilczynski (K = 0). The common axis of the three planes then becomes the canonical line of the first kind for which k - 5/12, which we shall designate as the first axis of Bompiani.6

It m-ay be remarked here that the Moutard quadric in a Darboux direction - et meets a Darboux quadric (5) in the asymptotic tangents through 0 and in a conic lying in the plane (14). As a consequence the Moutard quadrics in the three Darboux directions have a residual point of intersection on the first axis of Bompiani.

If the parameter K is left arbitrary, then the planes (14) correspond under a transformation of Cech with parameter j to three collinear points if, and only if, K = - 18j (the line thereby determined being the polar with respect to a Darboux quiadric of the first axis of Bompiani, independently of the value of K). This equation defines a correspondence at each point of the surface between the Cech transformations and those Darboux quadries for which K is independent of u, v. Thus, the quadries of Lie and Fubini for which K -9/2 and - 3 respectively, characterize the transformations of (Cech for which j = 1/4 and 1/6, whereas the transformation of Segre (j = 1) characterizes the quadric of Darboux for which K = - 18.

The osculating plane (14) is a stationary osculating plane if, and only if,

- 9cEm (AE,2+ BE + K) 2;

the value of K is thereby uniquely determined 7 and when substituted into

6 This line was first characterized in a more complicated way by Bompiani in the Rendiconti dei Lincei, ser. 5, vol. 33, (1924), pp. 85-90.

7 The value of K depends on the particular Darboux direction chosen, so that there exist three distinct Darboux quadrics with the property considered.

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Page 8: Systems of Quadrics Associated with a Point of a Surface

SYSTEMS OF QUADRICS ASSOCIATED WITH A POINT OF A SURFACE. 655

(14) gives as the equation of the stationary osculatinig plane

5

(15) (AE -B) (EjX +- Y) + [ E CjO(-Ei)]Z = O. j=o

The Moutard pencil of quadrics at 0 in the Segre direction X3/X2 =E

has the form (16) XY Z + E,2XZ + EiYZ + K Z2 0,

with Ki as parameter of the pencil. The curve of intersection of the surface S and an arbitrary quadric of this pencil has a branch in the conjugate Darboux direction, the osculating plane at 0 of this branch being expressed by

(17) ej2X + eiY + 4-(Act2 + Be + Ki)Z = 0.

Since the equation of the osculating plane at 0 of the curve of Darboux in the direction - et is

( 18) e 2X +,E,y + ? (A t2 + Bet 18) Z 0,

it follows that the planes (17) and (18) coincide only if

Ki - (A/3) E2 - (B/3) et -12.

This value of Ki determines a unique quadric of the pencil (16), and since there are three Moutard pencils in the Segre directions at 0, three corre- sponding quadrics are obtained in all. These quadrics intersect in the asymp- totic tangents through 0 and in a residual point lying on the canonical line of the first kind for which k = - 1/12. Under the transformation of Cech with j = 1/2 the three planes (18) are carried into collinear points on the second axis of Cech.

The condition that the osculating plane (17) contain a line I joining 0 to an arbitrary point (0, a, b, 1) requires that

Ki =-- (4a + A)E2- (4b + B)Ei.

The line I obtains in this way a single quadric out of each of the three Moutard pencils in the Segre directions, the residual point of intersection P of these quadrics having the co6rdinates

(4a+A)(4b +-B), 4a +A, 4b4 +B, 1.

As the line I varies in the bundle at 0, the point P generates the quadric of Wilczynskci; P lies on I if, and only if, I is the first axis of Bornmpiani.

The quadric of Moutard in the Segre direction Ei at 0 is that quadric of the pencil (16) for which

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Page 9: Systems of Quadrics Associated with a Point of a Surface

656 LOUIS GREEN.

K Ae,2 +Be - 4;

the osculating plane (17) determined by this value of Ki can also be described as the plane containing the non-degenerate conic of intersection of the Moutard quadrics in the conjugate directions + ei. The residual point of intersection of the Moutard quadrics in the three Segre directions lies on the canonical line of the first kind for which k= 3/4, while the transformation of Cech for which j- 1/6 carries the three planes (17) determined by these quadrics into collinear points on the second directrix of Wilczynski.

The Darboux-Segre pencils of quadrics will now be considered. For each choice of c let et, Cj, Ek represent the three values in (13). Then the three directions

X3/X2 = E- X3/X2 = {Ej X3/X2 = {k

at 0 determine a Darboux-Segre pencil of quadrics in the Darboux direction -et, having the equation

(19) XY - Z - 2Ei2XZ - 2ECYZ + KEZ2 = 0 (Ki arbitrary).

If the osculating planes at 0 of the three branches of the curve of intersection of the surface S and one of these quadrics be denoted by 7rTh, 7rij 7rik corre- sponding to the respective directions - Ej, ck, then

7rwj: E2X +,EY + (A E2 + Bei + K)Z =- O,

7rih: ch2X EhY + P,hZ 0 (h =j, k), where

-Aeh B + 4,E2 + K Eh2 Plt7 =

2Ej2 + 4Eh -4-+ 3Ch2

The condition that the plane 7r? coincide with the osculating plane of a curve of Darboux at 0 determines a unique quadric out of each Darboux-Segre pencil. The residual point of intersection of these three quadrics is the point of intersection (besides 0) of the quadric of Fubini with the canonical line of the first hind for which le = - 11/24.

A unique quadric in each Darboux-Segre pencil is also obtained from the condition that the three planes -iri, lj, rii- be coaxial, the parameters Ki then having the values

KIR= 4/5 (A ,2 + Bet + 2) (i= 1, 2, 3).

The three quadrics thus found have their residual point of intersection on the canonical line of the first 7hind for which 7c 9/20.

The locus of the line of intersections of the planes rij, 7ri for all quadrics

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SYSTEMS OF QUADRICS ASSOCIATED WITH A POINT OF A SURFACE. 657

in the pencil (19) is a plane passing through the Segre tangent X3/X2 et, X4- 0 and through the canonical line of the first kind for which k = - 3/4. The quadric determined by the condition that the planes 7rij, qrik contain this canionical linle corresponids to the parametric value

Ki S A E,2 -2BEi -4,

and the three quadrics so obtained for i = 1, 2, 3 have their residual point of intersection on this same line.

5. The Moutard pencils of quadrics. This section is concerned essen- tially with an examination of the singularity of the curve of intersection of the surface S anid a quadric of the Moutard pencil. The curve determined by the Moutard quadric of the pencil is found to differ radically from the curves determined by the other quadrics of the pencil.

The Moutard pencil of quadrics determined at a point 0 of S by a di- rection X3/X2 = ,h has the form

(20) XY- Z+ (1/4) (2-_3)XZ+ (I/x2)(2pY3 1)YZ+ KZ2 ==0,

where KM, is an arbitrary function of u, v. The quadric of Moutard of the pencil is obtained wheni

(21) p3KM = Af2 + B/4 - (f3 + 1 ) 2.

Let the equation

(22) Z n(Y - X) (it n 0)

represent an arbitrary plane through the tanigent X3/X2 =, X 0, CUttilng the surface S in a curve s and a quadric of the pencil (20) in a conic q. Then s and q have third-order contact at 0 for all values of m and K7i. Conversely, if every plane of the form (22) meets the surface S and a quadric Q in a pair of curves which have contact of the third order at 0, then Q belongs to the pencil (20). The quadric of Moutard (9) is the unique quadric of the pencil for which the contact between s and q is of the fourth order for all values of n.

If f is not a Darboux direction, there are two planes of sextactic section 8

passing through the tangent X3/X2 , X4 = 0, for which the contact between s and q is of the fifth order at 0. The values of n in (22) which determine these planes are the roots of the equation

(23) hn2 + (3 - 3)6- A ,2 + B._4)an+ (IA3 + ) 2 =O,

' Darboux, Bulletin des Sciences Mathemratiques et Astronomiques, ser. 2, vol. 4 (1880), p. 366.

10

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Page 11: Systems of Quadrics Associated with a Point of a Surface

658 LOUIS GREEN.

where h is defined by

h = 2(u3+ 1)3 - 32(i3+ ) (A +B2) +, , and

15

(24) Ct 0

The curve of intersection of S and an arbitrary quadric of the pencil (20) is given by equations (20) and (11). If ,b is not a Darboux direction, this curve has two branches at 0 in the direction ,u, whose equations are

(25) Y=p1X ?rX3/2+ , Z=xy+-. .

where r satisfies the equation

r2 - _ j (A J2 + B,u4 - tk6 -2,3 _1 _t3 Kp) / (/3 + 1 ).

If r = 0 the curve (25) is found to have a tacnode in the direction IA, so that

in view of (21) a necessary and sufficient condition that a quadric of the Moutard pencil in a non-Darboux direction / at 0 be the quadric of Moutard (9) is that its curve of intersection with S have a tacnode at 0 in the direction

,u instead of a cusp. For the case of the Moutard quadric (9) the terms of fifth degree in the

series (11) can be shown to be 5

z TjX5-iY' 0

where

To - CO, J3T, =- f43CJ + /ju.9- 6/,u + 12/3 _8,

=4T2 - C2 - 9IL9 + 3BfJ + 276 + 3A5 - 6B 427- 3 - 64Ah2 + 18, 5 T3 = C3 + 18pY' - 6B,,,7 27/ -6A5 + 3B4 + 27p_3 + 3A4 - 9,

{{6T4I 64- 819 + 12r6 -6I + 1, T5 C5-

The two tacnode branches of the curve of intersection of the surface S and the Moutard quadric (9) are now found to have the equations

(26) Y =--Ax X2+ , * *n Z=XY+ * (i =12),

where cr1, 02 are the roots of the equation

(27) (,A3 + 1)U2&+ (3- 3 6-A2 +BA4)0-+ h 0.

If r +4 0, the osculating plane at 0 of each cusp-branch (25) coincides with the tangent plane Z = 0, whereas if r = 0 the osculating planes at 0 are represented by the equations

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SYSTEMS OF QUADRICS ASSOCIATED WITH A POINT OF A SURFACE. 659

(28) (i - 1 2).

Setting ,/o? ni and using (27) we find that n,, n2 are the roots of equation

(23). Hence, the osculating planes at 0 of the tacnode branches of the curve of intersection of the surface S and the Moutard quadric in the non-Darboux direction ,u at 0 coincide with the planes of sextactic section which pass through the tangent line in the direction pt.

Comparison of the discriminants of (23) and (27) shows that the two planes of sextactic section through the line X,/X2 = i, X= 0 coincide if, and only if, the tacnode branches (26) have maximum-order contact at 0, this situation occurring for twelve values 9 of .

The results concerning the Moutard pencil of quadrics in a Darboux direction X3jX2 - e at 0 will be stated briefly. Each quadric Q of the pencil meets the surface S in a curve C whose triple-point tangents all coincide in the given Darboux direction. If Q is not the Moutard quadric of the pencil, this curve has a superlinear branch of order 3 and the osculating plane at 0 of each branch coincides with the plane Z = 0. If Q is the Moutard quadric then the curve C consists of two cusped branches and one linear branch. The osculating planes of the cusped branches at 0 coincide with the tangent plane to S, while the osculating plane of the linear branch at 0 is none other than the plane (15). This plane can also be obtained as a limiting case of (28) as , approaches -e.

6. Cones associated with the Moutard pencils of quadrics. The prob- lem of characterizing individual members of the Moutard pencils of quadrics in the Segre directions at a point of a surface has already been discussed. We now consider this problem for an arbitrary direction.

The curve of intersection of the surface S and an arbitrary quadric of the Moutard pencil (20) in a non-Darboux direction pt at 0 has a linear branch in the direction - 1/t2. The equations of this branch are

2 6(y3~1k6A,+ 1)2

so that its osculating plane at 0 is of the form

(29) ,2(' + 1) (X + 2Y) + [AI8 + B4- (6t- 1)2 + 6K1]Z = 0.

The condition that this plane contain a line 1 joining 0 to an arbitrary

9 Wilczynski, " Fifth memoir," Tracnsactions of the American MathematicaLl Society, vol. 10 (1909), p. 293.

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Page 13: Systems of Quadrics Associated with a Point of a Surface

660 LOUIS GREEN.

point (0, a, b, 1) determines a unique quadric Qy of the pencil, since the parameter KI, must satisfy the equation

(30) li'K, (6 -1)2- A8- a(F + 1)''- B/4--b(/' + 1)2 4.

Associated with the direction / are two others, ,, /2 which form with / a triple of directions apolar to the asymptotic directions. Thus two other quadrics, Q1,,, Q,2, belonging to the Moutard pencils at 0 in the directions

/o, /w 2, can be defined by this line I in exactly the same way as is Q1i, the equations of these quadrics being obtained from (20) and (30) by replacing ,A by ALw, , respectively. The three quadrics Q1,, Qi, Q,2 intersect in the asymptotic tangents through 0 and in a residual point whose join with 0 is a line 1' containing the point

Zl ?n 2Y2

=(2/3

1[6+ (3 + 1)2]p

(31) X3 =t3(2_1t3)[B +b(tk +j1)2], 2X == 3I(2 _t3) (2/A3 _ 1).

The lines 1 and 1' coincide if, and only if,

(32) a = - Al6/(26 + 1), b=- B (6 + 2),

so that the line I and the quadric Qt are uniquely determined by the given direction y. As , varies, I generates the quadric cone given by

(33) 3XY + 2AYZ + 2BXZ + ABZ2 = 0.

If, however, the line I is kept fixed and the direction ,u is varied, then I' generates a cone which in general is of the fourth order but for special positionis of 1 may be of the second order. To determine the conditions under which this occurs, we note that any qnadric cone generated by the line 1' must be of the form

(34) XY + pYZ + qXZ + -Z2==0

where p, q, r are functions of u, v. Substitutioni of equations (31) into (34) leads to seven equations of which the following five are independent:

b(p-a-A)=-0, a(q-b-B) =0, Ab - 3ab -5pb - 4q(a + A) + 4r 0, aB - 3ab -5aq - 4p(b + B) + 4r 0, 5AB + Ab + aB + 14ab + p(llb - 9B) + (la -9A)q + 33r = 0.

These equations have five sets of solutions for a, b, p, q, r which are exhibited in the following table:

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SYSTEMS OF QUADRICS ASSOCIATED WITII A POINT OF A SURFACE. 661

Case a b p q r (I) A/3 B/3 2A/3 2B/3 AB/3

( II)0 0 - A/3 -B/3 AB/3 (III) - 4A/9 4B/9 5A/9 5B/9 7AB/27

(IV) 0 4B/9 A B 5AB/9 (V) 4A/9 0 A B 5AB/9

Hence, a necessary and sufficient condition that the line 1' generate a quadric cone as ,u varies is that the fixed linte 1, which is the axis of the pencil of planes (29), join 0 to the point (0, a, b, 1) where a, b have any one of the five pairs of values listed in the table.

Five quadries belonging to the Moutard pencil in an arbitrary non-Darboux direction 10 u at 0 are thus characterized, each quadric having associated with it a quadric cone and a fixed line 1. In cases (I) and (II) of the table this line is the first axis of Bompiani and the first edge of Green respectively, while in case (III) it is the canonical line of the first kind for which lk = - 17/36. The lines determined in cases (IV) and (V) can be described as the polars with respect to a quadric of Darboux of the lines AxByp AyBxp where Ax, Ay and Bx, By are the intersections of the asymptotic tangents through 0 with the canonical lines of the second kind for which la = - 17/36, - 1/4.

The quadric cones associated with these five quadries are all mutually tangent along the first axis of Bompiani, the common tangent plane passing through the second canonical tangenlt. Consideratioln of these cones readily leads to the characterization of a number of new canonical lines of the first kind.

The cone (33), which is also one of the cones listed in the table, can be obtained in still another way. The line joining 0 to the residual point of

intersection of the three quadrics of Moutard in the directions p, ,uw, /L(

generates the cone (33) as u varies.11 There is a certain cone of class 3 closely associated with the Moutard

quadries at 0. The quadrics of Mloutard in the conjugate directions u, -, meet in the asymptotic tangents through 0 and in a collic whose plane has the

equation

2.k2(X + ,2 Y) + (A x2 + B,u4 A I6-1)Z=O.

As M varies this plane envelopes the cone, which in local plane co6rdinates

17 . . . n W74 has the equations

10 If ,u is a Darboux direction these quadrics, as well as the quadric determined by

(32), all coincide with the Moutard quadric. 11 Bompiani, " Contributi alla geometria proiettivo-differenziale di una superficie,"

Bollettinto della Matematica Italiana, vol. 3 (1924), pp. 97-100.

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662 LOUIS GREEN.

23 + ?)33-?)2?)3(A?)2 + Bq3 -24) 0 = .

The cusp-planes of this cone pass through the Segre tangents at 0 and intersect in the first directrix of Wilczynski.

7. Envelopes of Moutard quadrics. The problem of determining the envelope of a family of Moutard quadrics is of sufficient importance to warrant consideration. This problem has been discussed only by Kimpara,12 to the best of the writer's knowledge, and then merely for a special case.

The one-parameter family of Moutard quadrics at a point 0 of a surface S has an enveloping surface : which contains the asymptotic tangents through 0 as a locus of singular points. Elimination of pt between (9) and its /- derivative shows that > is an algebraic surface of order 14. The characteristic curve determined by > and a particular quadric of the family in the direction

it is a conic lying in the osculating plane at 0 of the pangeodesic which passes through 0 in the direction ju. Hence, the lines joining 0 to the points on the edge of regression of E generate the cone of Segre.

We now proceed with the problem of determining the envelope of a two- parameter family of Moutard quadrics. Let C(1) be a one-parameter family of curves on S which satisfy the differential equation

(35) dv - du = (X = A(u, v)),

and let it be assumed that these curves simply cover the portion of the surface under consideration and are nowhere tangent to an asymptotic curve. The tangents to C(1) then determine a two-parameter family of Moutard quadrics Q(2) one at each point of S. A particular point 0 therefore has associated with it a curve C, of the family C(1), whose tangent at 0 is

X3/X2 , X4=0 (=xAl/m),

a iid a quadric Q1L of the family Q 2. An arbitrary curve Cv on S, which passes through 0 in a direction X3/X2 v, determines at each of its points a unique Moutarci quadric belonging to Q (2), the quadrics so obtained forming a one parameter family Q (1) with an envelope E,. The quadric Q,t at 0 is a member of this family and hence touches Ev along a characteristic curve rv.

These curves rv and the envelope E of the family of quadrics Q (2) depend on the given curves C(1), and their properties differ widely in two separate cases, namely, when the curves C(1) are curves of Darboux and when they are nowhere tangent to a curve of Darboux.

12 11 Sur 1'enveloppe des quadriques de Moutard," Ryojun College of Engineering, Commemoration voltume (1934), pp. 33-39.

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SYSTEMS OF QUADRICS ASSOCIATED WITH A POINT OF A SURFACE. 663

(i) Suppose first that the curves C1) form a one-parameter family of curves of Darboux. The quadric Qt, is the Moutard quadric in the Darboux direction X3/X2, = at 0, and has the equation

(36) G X2X3- X1X4- 32X2X4 + 31X3X4 + (Bpt- A12)X42 = 0.

The characteristic curve rv determined by Q[t and a curve Cv through 0 is therefore given by (36) and

G.h + Gv( dv/du) = 0,

where dv/du refers to the direction of the tangent to Cv at 0, and since dvldu = vm/i this may be written

(37) IGu + vrGv = O.

The derivatives of A and B which appear in this equation may be readily evaluated. For,

A ~- (3/2)m),, Aub (3/2) (mip + m.+,), m = I/(/3y2)1/3, MU (m/3) (#3,/i3) - (2m/3) (yu/y),

and consequently, 181A, - 4AB - 27nV/,K.

Now from (3) it is seen that nipu can be expressed in terms of the coefficients appearing in series (2), and hence IA,, is expressible in like fashion. Thus we find

361A,u =278AB-648 -48C1 24C4,

36mBv = 278AB - 648 - 48C4 - 24C1,

36m,A, - 52A2 + 288B - 24C2 - 120C5,

361Bu 52B2 + 288A - 24C3 - 120CO.

With the aid of formulas (4) the left member of (37) can now be expressed in terms of ,u, v, the coefficients of series (2), and the local coordinates Xli , X4. Elimination of the term' X1X4 from the resulting equation by means of (36) finally yields the simplified result

(38) 36(j,- v) (IJX2 -X3) + LX2X4 + MX3X4 + NX42 - 0,

where the coefficients L, M, N have the values

L =12B,u(,u + 2v) -36A + 216(v-,u), M,, =12p (Ap, + B) (j -v) -L,

NT-- 72A(2v-) - 72Bj42(29x--v) + B2(54v + 40p) --A2/2(54? + 40v)

+ 13 1 ABI(v -) + 12 E Ci [ (5-i) + iv]. 0

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664 LOUIS GREEN.

If v & /, the equatiolns of rv can also be written in the non-homogeneous form

Y jX-4-1Lli + 11Ift' 1/2 X3/2 Z),+ 6 (v =/ZZ=XY4-

which simplify to

Y ===uX [i(A - B_2)]'/2X3/21 + Z Y + (v u).

Hence, if v & /, the characteristic curve rv is a quartic curve with a cusp at 0

and a cusp-tangent in the Darboux direction t. If Cv is tangent at 0 to the curve of Darboux CO,, then the characteristic

curve rv consists of the asymptotic tangents through 0 ancd of a non-ldegenerate conic lying in the plane whose equation is

(39) 18 (A, + B) (kX2 - X3)

+ [30a -36yu2(A,p+B) -47(A2,2 -B2)]X4 0,

a being defined in (24). Since this conic is tanlgent to Cy at 0, it follows that if Cv and C0M coincide, then C[, is part of the edge of regression of the en- velope Ev.

The points where the Quadric Q[, touches the envelope E of the two- parameter family of Moutard quadrics Q(2) are determined by the simultaneous solutions of equations (36), (38) and (39), where in (38) the value of v is

arbitrary but different from ,u. Since the plane (39) intersects the cone (38) in the Darboux tangent X3/X2 -, X4 0 and in another line 1 which passes through 0, and since these two lines meet the quadric Q1, at 0 and at some other poilit P not lying on S, it therefore follows that the envelope E consists

of th,e surface S and of another sheet generated by the point P.

(ii) We now assume that the curves C(1) are nowhere tangent to a curve

of Darboux. If H = 0 is the equation (9) of the Moutard quadric Qy in the

direction % at 0, then the characteristic curve rv determined by Ql, and a curve

Cv through 0 has the form

H -0, lHu + vmHv = 0.

The secoind of these equations Call be expressed in terms of %, v, the coefficients

of series (2), and the local coordinates Xl, , Xd, and when combined with (9) to eliminate the term X1X4 becomes

(40) 12(4(JX2 -X3) [ (2v - 3, 3v)X2 -(2 3 3yv 1) X3]

+ DX2X4 + EX3X4 + FX42 = 0,

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SYSTEMS OF QUADRICS ASSOCIATED WITH A POINT OF A SURFACE. 665

where D, E, F have the values

D 4A/5(2,_3v 9ph + 2v) + 4B1t5(u3 + 6,y2v 2)

+ 12,/3 [U6 ( 4v) -_O1K3 (,_-v) + 7p -4v]

-721k4(J( + 1) (IpW + vm,uv),

E~- l2,u(v-jih) (3 63 + An2-B -D, F 12An4[(t4h3+11) +I 2vL3+ 13)]

+ 12B 3[(13 u3 + 1) + ,Iv(11t3 + 5)1 + A2 _(54, + 40v) + B2 6(40j + 54v) + AB,u4[p(445t3 + 176) + v(176'13 + 45)] + 12/,%[(,L9 _l18,6-_21,3 _2) + v( 2U9-21%6-18M3+ 1)]

5

- 12tL3 E CG P[(5-_)' + jv]

+ 36 2 (3 - 3 6- A 2 + B/4) (Iltu + vntflv).

The characteristic curve rv is therefore a quartic curve with a double point at 0, one nodal tangent always lying in the given direction /%, the other depending o01 v. This second tangent lies in the direction ju if, and only if, v = /, and lies in the direction v only if v =- or v - 1/u2. The osculating plane at 0 of that branch of rv which lies in the direction v has the equation

24v4( 3 + ) (%- V) (IX2-X3) - (D + El)X4 0,

which reduces, when v /A, to (8). Hence, if v , the osculating plane at

0 of that nodal branch of the characteristic curve rv which lies in the direction ,u is inidependent of v and is the osculating plane of the pangeodesic in the direction p.

If v = , the osculating plane of the second nodal branch of rv at 0 is expressible in the form

24 /4 (/J3 + 1 ) (,- v) [(2v - 3/j _3V) X2 (2'f3 -3tt2V _ 1 )X3]

+ [D(2 3 - 31L2v 1) + E(2v- 3u - a3v)]X4 0.

As v varies this plane generates an axial pencil, its limiting position as v ap- proaches pt being giveni by

(41) 6,u(/&3 + 1) (1JX2 - X3)

+ [A4(11 4 +)+B/,(4-11/L3)+ 9jU6 9+ 36(t3 +1)']X4 0,

where /' is defined in (7). The plane (41) depends on the curve C, alone, being independent of the other curves of the family C(1), and together with the osculating plane of C, at 0, the osculating plane of the pangeodesic in the direction d at 0, and the tangent plane X4 = 0, determines an invariant cross-

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Page 19: Systems of Quadrics Associated with a Point of a Surface

666 LOUIS GREEN.

ratio of - 4. Hence, the plane (41) coincides at every point of the surface S with the osculating plane of the curve CG, if, and only if, the curves C(1) are pangeodesics.

If v ,u, (40) reduces to

(42) [X4- nl(X3 - fX2)] [X4 n2(X3 -X2)] ?

where ni, n2 are the roots of the equation

(43) Fn2 + En- 12_4(3

+ 1) O (v u).

The characteristic curve r, therefore consists of two non-degenerate conics determined by the intersections of the quadric Q[t and the planes (42). The harmonic conjugate of the plane X4 = 0 with respect to these two planes has the form

24h4(,3+1)(3 X2 X3) +EX4 =0 (v= ),

from which it follows that this plane, the osculating plane of Cu at 0, the osculating plane of the pangeodesic in the direction ,u at 0, and the plane X4 0, determine a cross-ratio of - 2.

The curves C(1) cannot be chosen so that at each point of S the two planes (42) coincide with the planes of sextactic section (28) which pass through the tangents to C(1). However, comparison of equations (43) and (23) shows that this situation does occur at a particular point 0 of S if, and only if,

Cl, has second-order contact at 0 with any one of a set of twelve pangeodesics. The quadric Qf touches the envelope E of the two-parameter family of

Moutard quadrics Q (2) at the points determined by equations (9), (40) and

(42), where the value of v in (40) is arbitrary but different from u. Since the two planes (42) meet the cone (40) in two lines 11, 12 which pass through 0 and are ordinarily distinct, and in the tangent X3/X2 , = 0, and since these three lines intersect QJ. at 0 and at two other points Pl, P2, it follows that the envelope E consists of the surface S and of two other sheets, those generated by the points P1, P2.

The lines 11, 12 coincide if, and only if,

(44) E2 + 48FM4(P3 + 1) 0,

where v a s in the expressions for E, F. Hence, at a particular point 0 of S there are two planes either of which may serve as the osculating plane of the curve C, in order that 11 and 12 coincide. It is impossible, however, to choose the curves C(1) so that the lines 11, 12 coincide for every point of S, since

equation (35) which determines the curves C(1) cannot satisfy (44) which is now a differential equation of the second order and second degree in dv/du.

INDIANA UNIVERSITY,

BLOOMINGTON, INDIANA.

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