Calculus of Variations/CHAPTER VII

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CHAPTER VII: REMOVAL OF CERTAIN LIMITATIONS THAT HAVE BEEN MADE. INTEGRATION OF THE DIFFERENTIAL EQUATION G=0 FOR THE PROBLEMS OF CHAPTER I.

  • 96 Instead of a sing-le regular trace, the curve may consist of a finite number of such traces.
  • 97 The first derivatives of F with respect to x and y vary in a continuous manner for the curve G=0, even if there are sudden changes in the direction of this curve.
  • 98 Explanation of the result given in the preceding article.
  • 99 Summary.
  • 100 Solution of the differential equation for Problem I of Chapter I.
  • 101,102 The discontinuous solution.
  • 103 The equation G=0 solved for Problem II, Article 9.
  • 104 The two fixed points must lie on the same loop of the cycloid.
  • 105 Through two points may be drawn one and only one cycloidal-loop, which does not include a cusp.
  • 106 Problem III. Problem of the shortest line on a surface.
  • 107 The same result derived in a different manner.
  • 108 Problem IV. Surface of rotation which offers the least resistance.
  • 109,110 Solution of the equation G=0 for Problem IV of Chapter I.

Article 96.
In the derivation of the formulae of Chapter V, it was presupposed that the portion of curve under consideration changed its direction in a continuous manner throughout its whole trace ; that is, x, y varied in a continuous manner. We shall now assume only that the curve is composed of regular portions of curve ; so that, therefore, the tangent need not vary continuously at every point of the curve. Then it may be shown as follows that each portion of curve must satisfy the differential equation G=0. For if the curve consists of two regular portions AC and CB, then among all possible variations of AB there exist those in which CB remains unchanged and only AC is subjected to variation.

As above, we conclude that this portion of curve must satisfy the differential equation G=0. The same is true of CB.

We may now do away with the restriction that the curve consists of one regular trace, and assume that it consists of a finite number of regular traces.

Article 97.
Suppose that the function F does not contain explicitly the variable x, and consequently Fx=0. Instead of the equation G=0, let us take G1=0, or

FxddtFx=0.

It follows that

Fx= constant,

the constant being independent of t; a priori, however, we do not know that Fx does not undergo a sudden change at points of discontinuity of x and y. Consequently, the more important is the following theorem for the integration of the differential equation G=0:

Even if x, y, and thereby also the direction of the curve, suffer at certain points sudden changes, nevertheless, the quantities Fx, Fy vary in a continuous manner throughout the whole curve for which G=0.

If t is a point of discontinuity in the curve, then on both sides of t we take the points τ and τ in such a manner that within the portions τt and tτ there is no other discontinuity in the direction of the curve. Then a possible variation of the curve is also the one by which t0τ and τt1 remain unaltered and ττ b only the portion ττ is varied. Here the points τ and τ are supposed to remain fixed, while t is subjected to any kind of sliding.

The variation of the integral

I=t0t1F(x,y,x,y)dt,

then depends only upon the variations of the sum of the integrals

τtF(x,y,x,y)dt+tτF(x,y,x,y)dt.

Since the first variation of this expression must vanish, we necessarily have (Art. 79)

0=τtG(yξxη)dt+tτG(yξxη)dt+[Fxξ+Fyη]τt+[Fxξ+Fyη]tτ.

Since G=0 along the whole curve, it follows that

[Fxξ+Fyη]τt+[Fxξ+Fyη]tτ=0.

The quantities ξ and η are both zero at the fixed points τ and τ; and, if we denote the values that may belong to the quantity Fx, according as we approach the point t from the points τ or τ by

[Fx]t and [Fx]t+,

the above expression becomes

([Fx]t[Fx]t+)(ξ)+([Fy]t[Fy]t+)(η)=0,

where (ξ) and (η) are the values of ξ and η at the point t. Since the quantities (ξ) and (η) are quite arbitrary, it follows that their coefficients in the above expression must respectively vanish, so that

[Fx]t=[Fx]t+ and [Fy]t=[Fy]t+;

that is, the quantities Fx and Fy vary in a continuous manner by the transition from one regular part of the curve to the other, even if x and y at this point suffer sudden changes.

This is a new necessary condition for the existence of a maximum or a minimum of the integral I, which does not depend upon the nature of the differential equation G=0.

Article 98.
The question naturally arises: How is it possible that the functions Fx, Fy, which depend upon x and y, vary in a continuous manner, even when x and y experience discontinuities? To answer this question we may say that the composition of these functions is of a peculiar nature, viz., the terms which contain x, y are multiplied by functions which vanish at the points considered. This is illustrated more clearly in the example treated in Art. 100. The theorem is of the greatest importance in the determination of the constant. In the special dp case of the preceding article, where Fx= constant it is clear that this constant must have the same value for all points of the curve. The theorem may also be used in many cases to prove that the direction of the curve nowhere changes in a discontinuous manner, and consequently does not consist of several regular portions but of one single regular trace. This is also illustrated in the examples which follow (Arts. 100 et seq.).

Article 99.
We may give here a summary of what has been obtained through the vanishing of the first variation as necessary conditions for the existence of a maximum or a minimum of the integral I:

1) The curve offering the maximum or minimum must satisfy the differential equation

G2Fxy2Fyx+F1(xdydtydxdt)=0,

or, what is the same thing, the two equations

G2Fxddt(Fx)=0, G2Fyddt(Fy)=0;

2) The two derivatives of the function F with respect to x and y must vary in a continuous m,anner even at the points where the direction of the curve does not vary continuously.

In order to establish the criteria by means of which it may be ascertained whether the curve determined through the equation G=0 offers a maximum or a minimum, we must investigate the terms of the second dimension in ΔI of Chapter V. First, however, to make clear what has already been written, we may apply our deductions to some of the problems already proposed.

\begin{center}SOLUTION OF THE DIFFERENTIAL EQUATION G=0 FOR THE PROBLEMS OF CHAPTER I.\end{center}

Article 100.
Let us consider Problem I of Art. 7. The integral which we have to minimize is

S2π=t0t1yx'2+y'2dt. [1]

Hence

F=yx'2+y'2, [2]

and consequently

Fx=yxx'2+y'2; Fy=yyx'2+y'2. [3]

From this it is seen that Fx and Fy are proportional to the direction cosines of the tangent to the curve at any point x(t), y(t); and, since Fx and Fy must vary everywhere in a continuous manner, it follows also that the direction of the curve varies everywhere in a continuous manner except for the case where y=0. But the quantity x'2+y'2 varies in a discontinuous manner if x and y are discontinuous; at the same time, however, y is equal to zero, as is more clearly seen in the figure below.

Since F does not contain x explicitly, we may use the equation

G1=0, or Fx=yxx'2+y'2=β, [4]

where β is the constant of integration. Hence

y2(dxdt)2=β2[(dxdt)2+(dydt)2]. [5]

The solution of this equation is the catenary:

x=α+βt, y=β2(et+et), [6]

where α is a second arbitrary constant.

Article 101.
A discontinuous solution. If we take the arc s as independent variable instead of the variable t, the differential equation of the curve is

ydxds=β.

Suppose that β=0, which value it must retain within the whole interval t0t1. Further, since y0 at the point P0. it dx follows that dxds=cos(ϕ)=0 (where ϕ is the angle which the tanas gent makes with the X-axis), and that cos(ϕ) must remain zero until y=0; that is the point which describes the curve must move along the ordinate P0M0 to the point M0. At this point dxds cannot, and must not, equal zero if the point is to move to P1. Hence, at M0 there is a sudden change in the direction of the curve, as there is again at the point M1. The curve giving the minimum surface of revolution is consequently, in this case, offered by the irregular trace P0M0M1P1. The case where β=0 may be regarded as an exceptional case. The unconstrained lines P0M0 and P1M1, i.e., x=x0 and x=x1 satisfy the condition G=0, since yG=G1, and for these values G1=0; also for these lines, y0. But G0 for the restricted portion M0M1 and is, in fact, equal to 1.

Article 102.
We may prove as follows that the two ordinates and the section of the X-axis give a minimum. This is seen at once when we have shown that the first variation for all allowable deformations is positive. The problem is a particular case of Art. 79.

The first variation may be decomposed into several parts (cf. Arts. 79 and 81):

δI=M0P0GwNds+[Fxξ+Fyη]M0P0M1M0GwNds+[Fxξ+Fyη]M1M0P1M1GwNds+[Fxξ+Fyη]P1M1.

Now all the boundary terms are zero, since

Fx=yxx'2+y'2, Fy=yyx'2+y'2,

and therefore both are zero at the points M0 and M1, while ξ and η are zero at P0 and P1. In the first and third integrals G=0; in the second this function equals unity, and if we reverse the limits, ds is positive, as is also wN. Hence the first variation δI is always positive.

When the arbitrary constant <β0, the curve consists of one regular trace that lies wholly above the X-axis. Further investigation is necessary to determine when this curve offers in reality a minimum.

Article 103.
In the second problem (Art. 9) we have for the time of falling the integral

T=t0t1x'2+y'24gy+α2dt. [1]

That this expression may, in reality, express the time of falling (the time and, therefore, also the increment dt being essentially a positive quantity), the two roots that appear under the integral sign must always have the same sign. Since 4gy+α2 can always be chosen positive, it follows that x'2+y'2 must be positive within the interval T0t1.

It might happen, however, if we express x and y in terms of t, that x and y might both vanish for a value of t within the interval t0t1. In this case the curve has at the point x,y, which belongs to this value of t, a singular point, at which the velocity of the moving point is zero.

Suppose that this is the case for t=t, and that the corresponding point is x0, y0 so that we have

x=x0+a(tt)m+, y=y0+(tt)m+,

where m2, and at least one of the two quantities a and b is different from zero.

Then is

x'2+y'2=m2(a2+b2)(tt)2(m1)+,

and

x'2+y'2=ma2+b2(tt)m1+.

Here we may suppose a2+b2 positive.

If now m is odd, then for small values of tt, the expression on the right is positive, and hence x'2+y'2 always has a positive sign.

If on the contrary m is even, equal to 2, say, then the curve has at the point x0,y0 a cusp, since here x'2+y'2 has a positive or a negative value according as t>t or t<t.

If therefore the above integral is to express the time, x'2+y'2 cannot always be put equal to the same series of t, but must after passing the cusp be put equal to the opposite value of the series. We therefore limit ourselves to the consideration of a portion of the curve which is free from singular points.

Such limitations must often be made in problems, since otherwise the integrals have no definite meaning. Hence with this supposition x'2+y'2 will never equal zero.

We may then write:

F=x'2+y'24gy+α2, [2]

and consequently

Fx=14gy+α2xx'2+y'2, Fy=14gy+α2yx'2+y'2. [3]

From this we may conclude, in a similar manner as in the first example, that Fx,Fy are proportional to the direction cosines of the tangent of the curve at the point x, y. Since now Fx,Fy vary in a continuous manner along the whole curve, and since, further, 4gy+α2 has a definite value which is different from zero, it follows also that the direction of the required curve varies in a continuous manner, or the curve must consist of one single trace.

Also here F is independent of x, and consequently we employ the differential equation G1=0, from which we have

Fx=14gy+α2xx'2+y'2=C, [4]

where C is an arbitrary constant.

If C is equal to zero, then in the whole extent of the curve C must equal zero; and consequently, since 4gy+α2 is neither 0 nor , xx'2+y'2=cos(α) must always equal zero; that is, the curve must be a vertical line. Neglecting this self-evident case, C must have a definite value which is always the same for the whole curve and different from zero.

From [4], it follows that

dx2=C2(4gy+α2)(dx2+dy2),

or, if we absorb 4g in the arbitrary constant and write

α24g=a, and 4gC2=c2,

we have

dx2=c2(y+a)(dx2+dy2);

whence

dx=c(y+a)dy(y+a)[1c2(y+1)]]. [5]

In order to perform this last integration, write

dϕ=cdy(y+a)[1c2(y+a)]; [6]

therefore

dx=(y+a)dϕ. [5a]

In the expression for dϕ, write

2c2(y+a)=1ξ. [7]

Then is

2[1c2(y+a)]=1+ξ, [8]

and

2c2dy=dξ. [9]

Therefore

dϕ=dξ1ξ2, [10]

and hence

ξ=cos(ϕ). [11]

Here the constant of integration may be omitted, since ϕ itself is fully arbitrary.

Hence,

y+a=12c2(1cos(ϕ)), and, from [5a], x+x0=12c2(ϕsin(ϕ)); [12]

equations, which represent a cycloid.

The constants of integration x0, c are determined from the condition that the curve is to go through the two points A and B. Now develop x and y in powers of ϕ: then in y the lowest power is ϕ2, and in x it is ϕ; so that the curve has in reality a cusp for ϕ=0, and this is repeated for ϕ=2π,4π,.

A and B must lie between two consecutive cusps (Art. 104).

The curve may be constructed, if we draw a horizontal line through the point x0, a, and construct on the under side of this line a circle with radius 1/(2c2), which touches the horizontal line at the point x0, a. Let this circle roll in the positive X-direction on the horizontal line, then the original point of contact describes a cycloid which goes through A and B and which satisfies the differential equation.

Article 104.
That the points A and B cannot lie upon different loops of a cycloid may be seen as follows: For simplicity, let the initial velocity α be zero and shift the origin of coordinates so as to get rid of the constants.

The equation of the cycloid is then

x=r(ϕsin(ϕ)), yr(1cos(ϕ)),

where we have written r in the place of 1/(2c2).

The cycloidal arc is seen from the accompanying figure. Take j two points lying upon different loops very near and symmetrically situated with respect to an apex, and let us compare the time it would take to travel from one of these points to the other by the way of the apex with the time taken over a straight line joining them. The parameters of the two points may be expressed by

ϕ0=2πψ0, ϕ1=2π+ψ0.

The time required to go by the way of the apex is

T=12gt0t1x'2+y'2ydt=12gs0s1dsy.

Now

dx=r(1cos(ϕ))dϕ,

and

dy=rsin(ϕ)dϕ,

so that

ds=dx2+dy2=2rsin(ϕ/2)dϕ,

and consequently

T=12gϕ0ϕ12rsin(ϕ/2)r1cos(ϕ)dϕ=rgϕ0ϕ1dϕ
rg(ϕ1ϕ0)=rg[2π+ψ02π+ψ0]=2rgψ0.

The component of velocity across the horizontal line from ϕ0 to ϕ1 is [vdxds] or, since dxds=sinϕ2 and v2=2gy, this component is equal to

[2gr1cos(ϕ)sinϕ2]ϕ0ϕ1=2grsin2ψ02.

The length of the line to be traversed from ϕ0 to ϕ1 is

x1x0=r[ϕ1ϕ0sinϕ1+sinϕ0]=2r[ψ0sinψ0].

Hence, the time required is

T1=2r(ψ0sinψ0)2grsin2(ψ0/2),

and consequently

T1T=2r(ψ0sinψ0)2grsin2ψ022rgψ0=ψ0sinψ02ψ0sin2ψ02=ψ033!ψ055!+2ψ0[ψ0213!(ψ02)3+]2.

Hence,

T1T<ψ033!2ψ0[ψ0216(ψ02)3+]2,

or

T1T<131(1ψ0224+)3.

It follows, therefore, for small values of ψ0 that

T1<T.

From this it is evident that a path of the particle including an apex cannot give a minimum.

Article 105.
Corresponding to the two constants that are contained in the general solution of the differential equation G=0 of Art. 103, it is seen that we have all the curves of the family G=0, if we vary r and slide the cycloid along the X-axis.

We shall now show that only one of these cycloids can contain the two points A and B on the same loop. Suppose that the ordinates of the points A and B to be such that DB>AC, and consider any other cycloid with the same parameter r described about the horizontal X-axis with the origin at O. Through O draw a chord parallel to AB and move this chord through parallel positions until it leaves the curve. We note that in these positions the ordinate AC increases continuously, since it can never reach the lowest point of the cycloid, and that the arc AB continuously diminishes. Consequently the ratio AB:AC continuously diminishes. When A coincides with the origin this ratio is infinite, and is zero when the chord becomes tangent to the curve.

Then for some one position we must have

ABAC=ABAC.

Since the points A and B are fixed, the length AB and the direction AB are both determined.

If AB=AB, then AC=AC, and a cycloid can be drawn through A and B as required. But if ABAB, then our cycloid does not fulfill the required conditions.

Next choose a quantity r such that

r:r=AC:AC.

With O as the center of similitude increase the coordinates of our cycloid parameters in the ratio r:r. These coordinates then become

x=r(ϕsinϕ), y=r(1cosϕ),

which are the coordinates of a new cycloid.

The latter cycloid is similar to the first, since the transformation moves the ordinate AC and the chord AB parallel to themselves. Their transformed lengths are respectively

rrAC=AC and rrAB=AB,

giving us a cycloid with the requisite lengths for the ordinate AC and the chord AB.

Further, there is but one cycloid which answers the required conditions. For, if we already had AB=AB and AC=AC, the only value of r which could then make rrAB=AB is r=r. Hence through the two points A and B there can be constructed one and only one cycloid-loop with respect to the X-axis.[1]

Article 106.
Problem III. Problem of the shortest line on a surface. This problem cannot in general be solved, since the variables in the differential equation cannot be separated and the integration cannot be performed. Only in a few instances has one succeeded in carrying out the integration and thus represented the curve which satisfies the differential equation.

This, for example, has been done in the case of the plane, the sphere and all the other surfaces of the second degree.

As a simple example, we will take the problem of the shortest line between two points on the surface of a sphere. The radius of the sphere is put equal to 1, and the equation of the sphere is given in the form

x2+y2+z2=1.

Now writing:

x=cosu, y=sinucosv, z=usinv, [1]

then u= constant and v= constant are the equations of the parallel circles and of the meridians respectively.

The element of arc is

ds=du2+sin2udv2, [2]

and consequently the integral which is to be made a minimum is

L=t0t1u'2+v'2sin2udt; [3]

so that here we have

F=u'2+v'2sin2u

and

Fu=uu'2+v'2sin2u, Fv=vsin2uu'2+v'2sin2u. [5]

Since F does not contain the quantity v, we will use the equation G1=0, and have:

Fv=vsin2uu'2+v'2sin2u=c,

where c is an arbitrary constant, which has the same value along the whole curve.

If for the initial point A of the curve u0, and consequently, therefore not the north pole of the sphere, then c will be everywhere equal to zero, only if v=0. We must therefore have v constant. It follows as a solution of the problem that A and B must lie on the same meridian.

If this is not the case, then always c0. It is easy to see that c<1; we may therefore write sinc instead of c, and have

vsin2uu'2+v'2sin2u=sinc, [6]

or

dv=sincdusinusin2usinc. [7]

If we write

cosu=cosccosw, [8]

then is

dv=sincdw1cos2ccos2w;

since 1 may be replaced by sin2w+cos2w, we have

dv=sincdwsin2w+cos2wsin2c=sincdwcos2wsin2c+tan2w=dtanwsinc1+tan2wsin2c.

Therefore

vβ=tan1(tanwsinc),

where β represents an arbitrary constant.

It follows that

tan(vβ)=tanwsinc. [9]

Eliminating w by means of [8], we have

tanucos(vβ)=tanc. [10]

This is the equation of the curve which we are seeking, expressed in the spherical coordinates u, v.

In order to study their meaning more closely, we may express u, v separately through the arc s, where s is measured from the intersection of the zero meridian with the shortest line.

Through [7] the expression [2] goes into

ds=sinudusin2usin2c,

and this, owing to the substitution [8], becomes

ds=dw,

and, therefore, if b is a new constant,

sb=w. [11]

Hence, from equations [8] and [9] we have the following equations:

cosu=cosccos(sb), cot(vβ)=sinccot(sb). [12]

But these are relations which exist among the sides and the angles of a right-angled spherical triangle.

If we consider the meridian drawn from the north pole which cuts at right angles the curve we are seeking, then this meridian forms with the curve, and any other meridian, a triangle to which the above relations may be applied.

Therefore, the curve which satisfies the differential equation must itself be the arc of a great circle. The constants of integration c, b, β are determined from the conditions that the curve is to pass through the two points A and B.

The geometrical interpretation is: that c is the length of the geodetic normal from the point u=0 to the shortest line; sb, the arc from the foot of this normal to any point of the curve, that is, the difference of length between the end-points of this arc; and vβ, the angle opposite this arc.

If we therefore assume that the zero meridian passes through A, then b is the length of arc of the shortest line from A to the normal, and β the geographical longitude of the foot of this normal.

Article 107.
We may derive the same results by considering the differential equation G=0.

Since

F1u'2=2Fv'2,

we have

F1=sin2u(u'2+v'2sin2u)3/2.

This value, substituted in

G2Fvu2Fuv+F1(vuuv)=0,

causes this expression to become

[2cosuu'2v+sin2ucosuv'3]+sinu(vuuv)=0,

or

dvdu[2+sin2u(dvdu)2]cosu+sinud2vdu2=0.

In this equation write

1)w=sinudvdu,

and we have

cotu(w+w3)+dwdu=0,

or

2)dww+w3+cotudu=0.

Integrating the last equation, it follows that

ln(w1+w2sinu)=c,

and consequently

3)w2sin2u=C2(1+w2).

Suppose that A is the north pole of the sphere, u the angular distance measured from A along the arc of a great circle, and v the angle which the plane of this great circle makes with the plane of a great circle through the point B.

Hence for all curves of the family G=0 that pass through A, we must have C=0, since sinu=0 for u=0. It follows also that w=0, and consequently,

sinudvdu=0,

or

v= constant.

Hence, as above, A and B must lie on the arc of a great circle. Next, if A is not taken as the pole, then always C0, and is less than unity. It follows then at once from equations 1) and 3) that

ds2=du2+sin2udv2=du2[1+w2],

or

ds=±sinudusin2usin2C, (where we have written sin2C for C2),

and

dv=sinCdusin(u)sin2usin2C.

Writing cosu=cosCcost, these two equations when integrated become, as in the last article,

cosu=cosCcos(sb), cot(vβ)=sinCcot(sb).

Article 108.
Problem IV. Surface of rotation which offers the least resistance. To solve this problem we saw (Art 12) that the integral

I=t0t1xx'3x'2+y'2dt

must be a minimum.

We have here

F=xx'3x'2+y'2

and we see that F is a rational function of the arguments x and y. For such functions Weierstrass has shown that there can never be a maximum or a minimum value of the integral. But leaving the general problem for a later discussion (Art. 173), we shall confine our attention to the problem before us.

We may determine the function F1 from the relation

2Fxy=xyF1.

It is seen that

F1=2xx(3y'2x'2)(x'2+y'2)3.

We may take x positive, and also confine our attention to a portion of curve along which x increases with t, so that x is also positive.

Consequently F1 has the same sign as 3y'2x'2, or of 3sin2λcos2λ, where λ is the angle that the tangent to the curve at the point in question makes with the X-axis.

F1 is therefore positive, if |tanλ|>13, and is negative, if |tanλ|<13, for the portion of curve considered.

We shall see later (Art. 117) that F1 must have a positive sign in order that the integral be a minimum. Hence, for the present problem, |tanλ| must be greater than 13 for the portion of curve considered; and as this must be true for all points of the curve at which x has a positive sign, the tangent at any of these points cannot make an angle greater than 30 with the X-axis (see Todhunter, Researches in the Calculus of Variations p. 168).

Article 109.
We shall next consider the difEerential equation G=0 of the problem.

Since F does not contain explicitly the variable y, we may best employ the equation

xG=G2FyddtFy=0.

We have at once

Fy= constant,

or

2xx'3y(x'2+y'2)2=C.

Now, if there is any portion of the surface offering resistance, which lies indefinitely near the axis of rotation, then the constant must be zero, since x=0 makes C=0.

If C=0, we have

x'3y=0,

and consequently

x=0 or y=0.

From this we derive

x= constant or y= constant.

In the first case, the surface would be a cylinder of indefinite length, with the Y-axis as the axis of rotation, and with an indefinitely small radius (since by hypothesis a portion of the surface lies indefinitely near the Y-axis); in the second case, the resistingsurface would be a disc of indefinitely large diameter. These solutions being without significance may be neglected, and we may therefore, suppose that the surface offering resistance has no points in the neighborhood of the Y-axis. This disproves the notion once held that the body was egg-shaped.

Article 110.
We consider next the differential equation

2xx'3y(x'2+y'2)2=C,

where C is different from zero. We may take x positive, and as the constant C must always retain the same sign (Art. 97), it follows that the product xy cannot change sign.

Instead of retaining the variable t, let us write

t=y,

and

dxdy=u.

The differential equation is then

2xu3(u2+1)2=C.

That we may write y in the place of t, is seen from the fact that xy cannot change sign, and consequently either x is continuously increasing with increasing y, or is continuously decreasing when y is increased. Hence, corresponding to a given value of y there is one value of x.

We have then

x=C(u2+1)22u3=C2(u+2u1+u3),

and

dxdu=dxdydydu=udydu=C2(12u23u4),

or

dydu=C2(u12u34u5);

consequently

y=C2[lnu+u2+34u4]+C1.

The equations

x=C2(u+2u1+u3), y=C2[lnu+u2+34u4]+C1,

determine a family of curves, one of which is the arc, which generates the surface of revolution that gives a minimum value, if such a minimum exists. For such a curve we have all the real points if we give to u all real values from 0 to +. Among these values is 3, and as we saw above, it is necessary that

dydx=1u>13 continuously,

or

1u<13 continuously.

In other words, if the acute angle which the tangent at any point of the arc makes with the X-axis is less than 30, it must continue less than 30 for the other points of the arc, and if it is greater than 30 for any point of the arc it must remain greater than 30 for all points of the arc. Hence, if P is the point at which the inclination of the tangent with the X-axis is 30, we shall have on one side of P that portion of curve for which the inclination is less than 30, and on the other side the portion of curve for which the inclination is greater than 30. The arc in question must belong entirely to one of the two portions.

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  1. This proof is due to Prof. Schwarz.