The Brachistochrone
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Transcript of The Brachistochrone
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A bit of optics
We begin with an apparently unrelated problem from optics.
A ray of light travels from point A to point P with velocity 1v and then,
entering a denser medium, travels from P to B with a smaller velocity 2v .
The total time T required for the journey is given by
( )
2
22
1
22
v
xcb
v
xaT
++
+= .
If we assume that this ray of light is able to select its path from A to B byway of P in such a way as to minimize T, then 0=dx
dT and by some
elementary calculus we find that
( ) 222
22
1 xcbv
xc
xav
x
+
=
+
or2
2
1
1sinsin
vv
=
This is Snells law of refraction. The assumption that light travels from one
point to another along the path requiring the shortest time is called
Fermats principle of least time. This principle not only provides a rational
basis for Snells law, but can also be applied to find the path of a ray of light
through a medium of variable density, where in general light will travel along
curves instead of straight lines.
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In the individual layers the velocity of light is constant, but the velocity
decreases from each layer to the one below it. As the descending ray of
light passes from layer to layer, it is refracted more and more toward the
vertical, and when Snells law is applied to the boundaries between the
layers, we obtain
4
4
3
3
2
2
1
1sinsinsinsin
vvvv
=== .
If we next allow these layers to grow thinner and more numerous, then in
the limit the velocity of light decreases continuously as the ray descends,
and we conclude that
=v
sina constant.
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A return to Bernoullis problem
Imagine the following coordinate system and that the bead (like the ray of
light) is capable of selecting the path down which it will slide from A to B in
the shortest possible time.
The argument given above yields
=v
sina constant. (1)
If the bead has mass m, so that mgis the downward force that gravity
exerts on it, then the principle of conservation of energy, the fact that the
work done by gravity in pulling the bead down the wire equals the increase in
kinetic energy of the bead tells us that 22
1m vm g y= . This gives
gyv 2= . (2)
From the geometry of the situation we also have
( ) 22 1
1
tan1
1
sec
1cossin
y+=
+
===
. (3)
On combining equations (1), (2), and (3) obtained from optics, mechanics,
and calculus we get
( ) cyy =+ 21
(4)
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as the differential equation of the brachistochrone.
Solving the brachistochrone
When y is replaced bydx
dyand the variables are separated, (4) becomes
dyyc
ydx
21
= . (5)
At this point we introduce a new variable by putting
tan
21
=
ycy
, (6)
so that 2sincy = , dcdy cossin2= , and
dydx tan=
dc 2sin2=
( ) dc 2cos1= .
Integration now yields
( )1
2sin22
cc
x += .
Our curve is to pass through the origin, so by (6) we have x= y= 0 when0= , and consequently 01 =c . Thus
( ) 2sin22
=c
x (7)
and
( ) 2cos12
sin 2 == ccy . (8)
if we now put2
ca = and 2= , then (7) and (8) become
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( ) sin=ax and ( )cos1=ay .
(9)
The Cycloid
The cycloidis the curve traced out by a point as a circle rolls along a line
(the x-axis).
We will use parametric equations to get the equation for the cycloid.
Since the distance the circle rolls is equal the amount of the circumference
that has been traced out, to get the x-value of our parametric equation we
need only to subtract the horizontal distance P is from C (i.e. PQ) from the
size of the segment of the circumference that has been traced out.
Since QP = sina , we get
( ) sinsin == aaax . (10)
For the y-value we simply subtract CQ from the radius, giving us
( ) cos1cos == aaay . (11)
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But (10) and (11) are the equations for the brachistochrone!