Integration of the Classical Action for the Quartic
Oscillator in 1 + 1 Dimensions
Robert L. Anderson
Department of Physics and Astronomy, University of Georgia, Athens, USA Email: [email protected]
Received July 11, 2013; revised August 11, 2013; accepted August 18, 2013
Copyright © 2013 Robert L. Anderson. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
ABSTRACT
In this paper, we derive an explicit form in terms of end-point data in space-time for the classical action, i.e. integration
of the Lagrangian along an extremal, for the nonlinear quartic oscillator evaluated on extremals.
Keywords: Action; Integral
1. Introduction
The action
extremal
d
, ; , , d
d b
a
t qo a a b b qo
t
S t y t y L y t y t t
t
, (1.1)where
2 4
4
d
2 d 4
qo
k y
m y
L
t
equals the Lagrangian for
the quartic oscillator in 1 + 1 dimensions, is integrated along an extremal and expressed in terms of the space- time end-point data
ta,ya
, t yb, b
.We begin in a well-known way by adding and sub- tracting the kinetic energy to the Lagrangian. Thus we obtain from (1.1), after changing the variable of integra- tion in the remaining integral, the following equivalent expression.
extremal
extremal d
, ; , d
d
,
b
a
y
qo a b
y
b a
S t y t y m y y
t
E t t
(1.2)where is the energy on the extremal (See e.g. Gold- stein [1]). Equation (1.2) is the form of the action that we will start from and then derive by integrating the first term in (1.2), which we call the momentum integral, thus the desired expression for qo is obtained. (Some au-
thors call this momentum integral the action.) For our convenience, we refer to the second term in (1.2) as the energy term. The derived action depends only on the end-point data in space-time.
E
S
qo
S
In Part 2 Alternative derivation of the Quartic Oscillator Solution, we present an approach in which we
arrive at the linearization map in [2]. This maps the solu- tions to Newton’s equations of motion for the quartic oscillator 1 − 1 onto those of the harmonic oscillator in a way which lends itself to integrating the momentum in- tegral in (1.2). It involves a parametization of time t in
terms of an angular coordinate (a cyclic coordinate which takes advantage of the periodic motion of the quartic oscillator and is intrinsic to the harmonic oscilla- tor ho). This results in the time being given by a quadra-
ture involving a known function of , as in [2]. As stated in [2] R. C. Santos, J. Santos and J. A. S. Lima [3], first demonstrated the possibility of linearization of the quartic oscillator to the harmonic oscillator.
In Part 3 Integration of the momentum integral, the
results in Part 2 lead to an integration of (1.2). This is a
new result and an extension of the results in [3].
In Part 4 Derivation of qo, using the results in Part
2 and Part 3, we derive a classical action qo evaluated
on an extremal in terms of space-time endpoint data and show that Hamilton’s equations are satisfied.
S
S
In Part 5 Equivalent Actions, we present two equi-
valent actions as variations on the result in Part 4. By
equivalent we mean they are equal in value on extremals and they produce the same Hamilton’s equations.
In Part 6 Conclusion, we indicate briefly how the
ap-proach in Parts 3 and 4 can be directly extended to all
members of a hierarchy with potential energies
2
2 2 2 2 1
1 .
2
n
n n n n n
V y k y t
n
2. Alternative Derivation of the Quartic
Oscillator Solution
To begin with, we must establish the sign conventions implied by (1.2) for the quartic oscillator
2
1
2
1
extremal
extremal
d d
d 2
1 d
y y y
qo y
m y t y
t
V y
E
m y
m E
,(2.1)
where
4 4 4
qo
V y k y
E E
Taking advantage of the periodicity of any extremal for the quartic oscillator qo, we execute a change of
variable to the angular variable by setting
4 42
0 ,
sin
4
qo
V y k y
E E
(2.2) where
0
0
0 0 0y t y y t y
and
0
0 0
d d
d d 2
d d t
y y
y t t t E m
t t
and E = energy on the extremal. We have opted not to
change the symbol for a function when it depends on a variable through a nested function in order to avoid un- necessarily heavy notation. Making the signs explicit, (2.1)-(2.2) yield
1 4
0 1 4 2
4 0
sin
4 .
sin
E y
k
(2.3)
and
0d 2 cos .
d
y E
t m
(2.4)Note, for future use (2.3) implies
1 4
0 1 4 2
4 0
cos
4 1
d
2 sin
E y
k
d .
(2.5)
Now, we are in position to present an alternative deri- vation of the solution to Newton’s equations of motion (2.7) below for the quartic oscillator. It involves a pa-
rametization of time in terms of the angular coordinate. As we shall see, this results in the time being given by a quadrature involving a known function of . Now dif- ferentiating (2.4) yields
2
0 2
d 2 sin d .
d d
y E
m t
t
(2.6)
Or from Newton’s equation of motion for the quartic oscillator
2
3 4 2 d
, d
y
m k
t y (2.7)
we obtain
3 4
0
2 sin .
d
k y E
m m
d
t
(2.8)
Thus, it follows from (2.3) that we obtain the equation that yields involving t
1 4 1 2 1
2
1 44 0
dt k E m 2 sin d. (2.9a) Or, it s integrated form which yields (in quadrature) involving a known function of
t
0
1 2 1 4
1 4 2
0 4 2 sin 0 d .
m
t t k E
(2.9b)The inverse of (2.9a) is given by
1 2 1 2 2 4
2
d k y
m
d ,t (2.10a)
and it’s integrated form is given by
0
1 2
1 2 2 4 0
2
( ) d ,
t
t k
t y t
m
t
(2.10b) where the integration is along an extremal.
The equivalence to the linearization map given in [2]
is specified by setting 0 , where
constant of the harmonic oscillator and equals the time of the corresponding to of the .
0 tˆ ˆt
ho
2
2 spring
k m
ho tˆ
t qo
Then (2.9b) and (2.10b) are equivalent to one half of the linearization map in [2]. The other half of the lineari- zation map is given by
1 2 2
0
1 2 1 2
4 2
ˆ
sin .
4 2
ho
y t y t x t
E k E k
(2.11)
Equation (2.2) plus equation (2.4) imply
1 2
1 2
4 4 2 2 2
4
4 2 cos sin
b a b b a a b a b a
E
y y y y y y
k
how does one determine all other quantities. One is given
a,a
tˆatˆb
and
tˆbtˆo
, where refers to times, areknown. Now we can set
ho
ˆ
o o
t t .
y t and
y tb,b
on an ex-tremal. The linearization map yields a
qo x and xb on the
corresponding extremal as well as ho qo .
This implies from (2.12) the time differences
ho E E From [4], as a result of mapping extremals for the ho
1
1
onto extremals to the qo, we have from [4],E ho
1 2 1 2
2 2
1 2
0 4
sin sin
sin 4 ,
sin
b b a a a b
b a
y y t y y t
t E k
(2.13) and
1 2 1 2
2 2
1 2
0 4
cos cos
cos (4 ) ,
sin
b b a a a b
b a
y y t y y t
t E k
(2.14) Now (2.13) and (2.14) imply e.g.
1 2 2
0 2 1 2 1 2
sin tan
cos
b b b a
b
b b b a a
y y
y y y y
2
a
ˆ
a t
where ˆ ˆ
ˆ ˆ
ˆ and yieldsb o a o b
t t t t t t tˆ
0 .
Everything else follows from the development in
Part 3.
3. Integration of
t
extremal
d
d
d
ba
y
qo qo y
y
m
y
The problem of integrating (1.2) is the problem of inte- grating (2.1). Therefore, using (2.2) , (2.4) ,and (2.5), we obtain
4 4 extremal
extremal 1 4
1 4 2
0 0
4
d 2
d 1 d
d 4
2 cos 4 1 sin cos d
2
b b
a a
b
a
y y
y y
k y E
m y t y m y
t m E
E E
m
m k
0
(3.1)
Effecting the integration by parts, where
2
3 40
d d d
, sin
d d d
f g
fg g f f
and
00
2cos 3sin
g
yields
1/ 4 1 2
1 4 4
1 2 1 4
4
extremal 4
1 4 3 4 0
2 2
0 0
0
3 4 1 2
3 4 0
2 1 1 4
0 4
d 2 4 1 2 2 1
d
d 2 3
cos
sin d sin
sin
cos 2
4 sin
3 3 s
b
a
b b
a a
b
a
y qo
qo y
b a
y E E m
m y m k E
t m k m k E
m E
E
t t
k
2
in
(3.2)
Finally, from (2.9b), we have
3 4 1 2
3 4 0
2 0 1 4
0
extremal 4
1 2
3 2 0
2 4
0
d 4 2 cos
d sin
d 3 3 sin
cos
4 1 ,
3 3 2 sin
b b
a a
b
a
y qo
qo b a
y
b a
y E m E
m y t t
t k
mk E
t t y t
(3.3)
4. Determination of a
S
qoThe developments in Part 2 and Part 3 lead directly to
the following determination of Sqo. It follows from (3.3) that (1.2) is given by
extremal extremal
1 2
3 2 0
2 4
0
1 2
3 2 0 3 2 0
2 2
4
0 0
d
, ; , d
d
cos
4 1
3 3 2 sin
cos cos
1
3 2 sin sin 3
b
a
b
a
y
qo a b b b a
y
b a b a
b a
b a
b a
S t y t y m y y E t t
t
mk E
t t y t E t t
mk E
y y
b a
t t
(4.1)
Therefore, using (2.10b), we obtain
0 0
0 0
1 2 1 2
2 2
4 4
1 2
3 2 3 2
2 2
4
1 2 1 2
2 2
4 4
; ; ,
2 2
cos d cos d
1
3 2 2 2 3
sin d sin d
b a
b a
qo a b b
t t
t t
b t a t
t t
S t y t y
k k
y t t y t t
m m
mk E
y y
k k
y t t y t t
m m
b a
t t
(4.2)
This is expressed in the endpoint variables as required. This implies
0
0
0
0
1 2 2 4
1 2
1 2 1 2
1 2 1 2
2 2
4 4
1 2 4
2 4
1 2
1 2 4 2
2
cos d
2
4 cos d
2 sin 2 d 2
2
2 cos d ,
b
b
b b
b
t
t t
qo
qo b b t
b t
t t
t
k
y t t
m
S mk mk E k
p y y y t
y k k
y t t
m
k
mE y t t
m
4 t
m
(4.3)
0
1 2 1 2
3 2 1 2
2 2
4 4
1 2
2 4 2
1 2
1 1
.
3 2 2 3
sin b d
qo
b t b
b
t
S mk k
y y
t k m
y t t
m
E E
After using (2.11) this checks with m times (2.4) for pqob and tb obviously checks.
The a-differentiations parallel the b-differentiations and yield
0
0
0 0
1 2 2 4
1 2
1 2 1 2
1 2 1 2
2 2
4 4
1 2 4
2 4
1 2
1 2 4 2
2
cos d
2 4
cos d
2 2 2
sin d
2
2 cos d ,
a a
a
a
t
t t
qo
qoa a a t
a t
t t
t
k
y t t
m
S mk mk E k4
p y y y t
y k k
y t t
m
k
mE y t t
m
0
1 2 1 2
3 2 1 2
2 2
4 4
1 2
2 4 2
1 2
1 1
.
3 2 2 3
sin d
a
qo
a t a
a
t
S mk k
y y
t k m
y t t
m
E E
(4.4)
5. Equivalent Actions
Here, we present two examples of equivalent actions as variations on this result. By equivalent we mean they are equal in value on extremals and they both produce the same Hamilton equations.
First Variation:
This variation follows from the indentities
0 max 0 max
0 max 0 max
sin sin cos ,
cos cos sin ,
(5.1)which implies that (4.2) transforms to the expression
max max
max max
extremal extremal
1 2 1 2
2 2
4 4
1 2
3 2 3 2
2 2
4
1 2 1 2
2 2
4 4
d
, ; , d
d
2 2
sin d sin d
1
3 2 2 2
cos d cos d
b
a
b a
b a
y
qo a a b b b a
y
t t
t t
b t a t
t t
S t y t y m y y E t t
t
k k
y t t y t t
m m
mk
y y
k k
y t t y t t
m m
.3 b a
E
t t
(5.2)
Second Variation:
Equation (5.2) is equivalent to
max max max
max max
1 2
3 2 1 2 3 2 1 2 1 2
2 2 2 2 2
4 4 4
3 2 1 2 3 2
2 4 2 2 4
, ; ,
1 2 2 2
cos d cos d sin
3 2
2 2
cos d cos
b b b
a a
qo a a b b
t t t
b b
t t t
t t
a a
t t
S t y t y
mk k k
y y t t y y t t y t
m m
k k
y y t t y
m m
4 d
k
t m
max
1 2 1 2
2 d sin 2 4 2 d
1
. 3
a
t
t
b a
k
y t t y t t
m
E t t
(5.3)
Comment: The signs and the limits of integration have to be carefully watched in these calculations.
The identity
3 2 1 2
2
max max max
3 2 3 4
2 2
max max max
cos 3
2 cos cos
b b b
b b
y y y
y
2
,
y
(5.4)
follows from
2 1 2
2 1 2
max maxcos max .
b b b
y y y y
Similarly for the endpoint, thus we obtain the re- sult reported in [4].
a
The results given in [4] were obtained before the inte- gration result reported here in Part IV was obtained.
6. Conclusions
One can parallel the development in Parts 3 and 4 for an
hierarchy with potential energies
22 2 1
1 2
n
n n n
V y k y
n
(6.1) Starting with setting
2
2 22
0 ,
sin
2
n
n n
V y k y
E nE
(6.2) one can parallel Part 3.
Then integration by parts in these cases is effected by
2
1 20
d d d , sin
d d d
n n
f g
fg g f f
and
0 0
cos 1 sin
n g
n
.
The linearization map for these cases is given in [2].
REFERENCES
[1] H. Goldstein, “Classical Mechanics,” Addison-Wesley Publishing Company, Reading, 1980.
[2] R. L. Anderson, “An Invertible Linearization Map for the Quartic Oscillator,” Journal of Mathematical Physics,
Vol. 51, No. 12, 2010, Article ID: 122904.
[3] R. C. Santos, J. Santos and J. A. S. Lima, “Hamilton- Jacobi Approach for Power-Law Potentials,” Brazilian Journal of Physics, Vol. 36, No. 4A, 2006, pp. 1257-
1261.