Xdx + Ydy = 0

has to be integrated where X = p(x), Y = [phi](y) are given as curves. If

we write

au = [Integral]Xdx, av = [Integral]Ydy,

then u as a function of x, and v as a function of y can be graphically

found by the integraph. The general solution is then

u + v = c

with the condition, for the determination for c, that y = y_0, for x = x_0.

This determines c = u_0 + v_0, where u_0 and v_0 are known from the graphs

of u and v. From this the solution as a curve giving y a function of x can

be drawn:--For any x take u from its graph, and find the y for which v = c

- u, plotting these y against their x gives the curve required.

If a periodic function y of x is given by its graph for one period c, it

can, according to the theory of Fourier's Series, be [Sidenote: Harmonic

analysers.] expanded in a series.

y = A_0 + A_1 cos [theta] + A_2 cos 2[theta] + ... + A_n cos n[theta] +

...

+ B_1 sin [theta] + B_2 sin 2[theta] + ... + B_n sin n[theta] +

...

where [theta] = 2[pi]x / c.

The absolute term A_0 equals the mean ordinate of the curve, and can

therefore be determined by any planimeter. The other co-efficients are

A_n = 1/[pi] [Integral,0:2[pi]] y cos n[theta].d[theta];

B_n = 1/[pi] [Integral,0:2[pi]] y sin n[theta].d[theta].

A harmonic analyser is an instrument which determines these integrals, and

is therefore an integrator. The first instrument of this kind is due to

Lord Kelvin (_Proc. Roy Soc._, vol xxiv., 1876). Since then several others

have been invented (see Dyck's _Catalogue_; Henrici, _Phil. Mag._, July

1894; _Phys. Soc._, 9th March; Sharp, _Phil. Mag._, July 1894; _Phys.

Soc._, 13th April). In Lord Kelvin's instrument the curve to be analysed is

drawn on a cylinder whose circumference equals the period _c_, and the sine

and cosine terms of the integral are introduced by aid of simple harmonic

motion. Sommerfeld and Wiechert, of Konigsberg, avoid this motion by

turning the cylinder about an axis perpendicular to that of the cylinder.

Both these machines are large, and practically fixtures in the room where

they are used. The first has done good work in the Meteorological Office in

London in the analysis of meteorological curves. Quite different and

simpler constructions can be used, if the integrals determining A_n and B_n

be integrated by parts. This gives

nA_n = - 1/[pi] [Integral,0:2[pi]] sin n[theta].dy;

nB_n = 1/[pi] [Integral,0:2[pi]] cos n[theta].dy.

An analyser presently to be described, based on these forms, has been

constructed by Coradi in Zurich (1894). Lastly, a most powerful analyser

has been invented by Michelson and Stratton (U.S.A.) (_Phil Mag._, 1898),

which will also be described.

[Illustration: FIG. 23.]

The _Henrici-Coradi_ analyser has to add up the values of dy.sin n[theta]

and dy.cos n[theta]. But these are the components of dy in two directions

perpendicular to each other, of which one makes an angle n[theta] with the

axis of x or of [theta]. This decomposition can be performed by Amsler's

registering wheels. Let two of these be mounted, perpendicular to each

other, in one horizontal frame which can be turned about a vertical axis,

the wheels resting on the paper on which the curve is drawn. When the

tracer is placed on the curve at the point [theta] = 0 the one axis is

parallel to the axis of [theta]. As the tracer follows the curve the frame

is made to turn through an angle n[theta]. At the same time the frame moves

with the tracer in the direction of y. For a small motion the two wheels

will then register just the components required, and during the continued

motion of the tracer along the curve the wheels will add these components,

and thus give the values of nA_n and nB_n. The factors 1/[pi] and -1/[pi]

are taken account of in the graduation of the wheels. The readings have

then to be divided by n to give the coefficients required. Coradi's

realization of this idea will be understood from fig. 23. The frame PP' of

the instrument rests on three rollers E, E', and D. The first two drive an

axis with a disk C on it. It is placed parallel to the axis of x of the

curve. The tracer is attached to a carriage WW which runs on the rail P. As

it follows the curve this carriage moves through a distance x whilst the

whole instrument runs forward through a distance y. The wheel C turns

through an angle proportional, during each small motion, to dy. On it rests

a glass sphere which will therefore also turn about its horizontal axis

proportionally, to dy. The registering frame is suspended by aid of a

spindle S, having a disk H. It is turned by aid of a wire connected with

the carriage WW, and turns n times round as the tracer describes the whole

length of the curve. The registering wheels R, R' rest against the glass

sphere and give the values nA_n and nB_n. The value of n can be altered by

changing the disk H into one of different diameter. It is also possible to

mount on the same frame a number of spindles with registering wheels and

glass spheres, each of the latter resting on a separate disk C. As many as

five have been introduced. One guiding of the tracer over the curve gives

then at once the ten coefficients A_n and B_n for n = 1 to 5.

All the calculating machines and integrators considered so far have been

kinematic. We have now to describe a most remarkable instrument based on

the equilibrium of a rigid body under the action of springs. The body

itself for rigidity's sake is made a hollow [v.04 p.0981] [Sidenote:

Michelson and Stratton analyzer] cylinder H, shown in fig. 24 in end view.

It can turn about its axis, being supported on knife-edges O. To it springs

are attached at the prolongation of a horizontal diameter; to the left a

series of n small springs s, all alike, side by side at equal intervals at

a distance a from the axis of the knife-edges; to the right a single spring

S at distance b. These springs are supposed to follow Hooke's law. If the

elongation beyond the natural length of a spring is [lambda], the force

asserted by it is p = k[lambda]. Let for the position of equilibrium l, L

be respectively the elongation of a small and the large spring, k, K their

constants, then

[Illustration: FIG. 24.]

nkla = KLb.

The position now obtained will be called the _normal_ one. Now let the top

ends C of the small springs be raised through distances y_1, y_2, ... y_n.

Then the body H will turn; B will move down through a distance z and A up

through a distance (a/b)z. The new forces thus introduced will be in

equilibrium if

ak([Sigma]y - n (a/b) z) = bKz.

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