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Transcript
November 20, 2003 14:53:25
P. Gutierrez
Physics 5153 Classical Mechanics
Velocity Dependent Potentials
1
Introduction
We have so far only considered forces and therefore potentials, that are dependent only on the
spatial coordinates. In this lecture, we will consider velocity dependent potentials.
1.1
Rayleigh’s Dissipation Function
The standard form of Lagrange’s equations of motion, ignoring the Lagrange multiplier term, are
µ
¶
d ∂L
∂L
= Qi
(1)
−
dt ∂ q̇i
∂qi
where L = T − V and the gradient of the potential V is assumes to be a generalized force
Q0i =
∂V
∂qi
(2)
which could in principle be remove from the Lagrangian and added to the right hand side. But
what if the we have a velocity dependent damping force of the form
(3)
F ∝ −q̇
Examples of this type of force are atmospheric drag, resistive motion through a viscous fluid, and
damping force in a spring. In these cases, we can define a new function, the Rayleigh dissipation
function
n
n
1 XX
1
cij q̇i q̇j
(4)
F = cq̇ 2 or in general F =
2
2
i=1 j=1
and write the equations of motion in the following form
¶
µ
∂L ∂F
d ∂L
−
+
=0
dt ∂ q̇i
∂qi
∂ q̇i
(5)
where we are assuming that the only generalized forces are those that can be written as potentials
and in terms of F. The last term, therefore, represents a generalized force
Q=−
∂F
∂ q̇
(6)
To interpret F, we recall that the rate of energy lost or gained from an applied force in rectangular coordinates is given by
X
dW
~ i · ~vi
F
(7)
=
dt
i
This equation can be transformed to generalized coordinates
X ∂xi
X
dW
=−
Fi
q̇i = −
Qi q̇i = −2F
dt
∂qi
i
(8)
i
Velocity Dependent Potentials-1
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November 20, 2003 14:53:25
P. Gutierrez
where the minus sign is due to the force and velocity acting in opposite directions, and we use
Qi = F i
∂xi
∂F
=
∂qi
∂ q̇i
(9)
in the last step. Hence, F is half the energy lost by the system, and is independent of the set of
coordinates used as would be expected.
1.2
Velocity Dependent Potentials
Another example of a velocity dependent force that can be incorporated into the Lagrangian, is
the Lorentz force. Recall that the basic form of Lagrange’s equation is
∂T
d ∂T
−
= Qi
dt ∂ q̇i ∂qi
(10)
If the force is derivable from a position dependent scalar function (potential), then the Lagrange
equations of motion are given by
d ∂L
∂L
−
=0
(11)
dt ∂ q̇i ∂qi
where L = T − V and V ≡ V (q, t). Let’s now consider a simple generalization of the definition of
a conservative potential
Qi = −
∂V
∂qi
⇒
Qi = −
∂U
d ∂U
+
∂qi
dt ∂ q̇i
with
U ≡ U (q̇, q, t)
(12)
A potential that satisfies this condition, also allows the Lagrange equations to be put into the same
form as Eq. 11
1.2.1
Example—The Lorentz Force
As an example of a velocity dependent potential, we will consider the Lorentz force
~ = e(E
~ + ~v × B)
F
(13)
To use it in the Lagrangian, it has to be written in terms of the scalar and vector potentials

µ
¶
~ = −∇φ
~ − ∂A 
E
~ = e −∇φ
~ − ∂A + ~v × ∇
~ ×A
∂t
⇒ F

∂t
~ ×A
B=∇
To show that the Lorentz force satisfies Eq. 12, we will work in Cartesian coordinates. First,
~ is equivalent to the standard potential that we use. Therefore, we
we note that the term −e∇φ
only need to consider the term
µ
¶
∂A
~ ×A
e −
+ ~v × ∇
(14)
∂t
Velocity Dependent Potentials-2
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November 20, 2003 14:53:25
P. Gutierrez
To simplify the algebra significantly, we will consider only the x coordinate and generalize in the
end. The triple cross product can be expanded out to give
µ
µ
¶
¶
∂A
∂A
∂A
∂A
y
x
x
z
~ × A)x = vy
(~v × ∇
−
− vz
−
∂x
∂y
∂z
∂x
∂Ay
∂Az
∂Ax
∂Ax
∂Ax
∂Ax
+ vz
+ vx
− vx
− vy
− vz
(15)
= vy
∂x
∂x
∂x
∂x
∂y
∂z
where we add and subtract the third and forth terms in the last equation. Since A is a function of
position and time, the total derivative is given by
∂Ay
dAx
∂Ax
∂Az
∂Ax
=
vx +
vy +
vz +
dt
∂x
∂y
∂z
∂t
(16)
Using this expression, the triple cross product can be written in a more compact form
~ × A)x = ∂ (~v · A) − dAx + ∂Ax
(~v × ∇
(17)
∂x
dt
∂t
where we use the fact that the velocity is not an explicit function of the coordinates. Next we
observe that
·
¸
d ∂
dAx
=
(~v · A)
(18)
dt
dt ∂ ẋ
since A is not an explicit function of the velocity. Hence
½
·
¸¾
∂φ ∂~v · A
d ∂
Fx = e −
+
−
(~v · A)
(19)
∂x
∂x
dt ∂ ẋ
which can be generalized to the following expression
·
´¸
d ³~
~
~
∇v (φ − ~v · A)
F = e −∇ (φ − ~v · A) +
dt
(20)
This is in the required form
d
Qi =
dt
µ
∂U
∂ q̇i
¶
−
∂U
∂qi
with
U = e (φ − ~v · A)
(21)
The Lagrangian for a charged particle of mass m traversing an electromagnetic field is given by
1
L = mv 2 − e (φ − ~v · A)
2
From the Lagrangian, we can calculate the generalized momentum, which is
p=
∂L
= m~v + eA
∂ q̇i
(22)
(23)
so if any of the coordinates are cyclic, it is this momentum that is conserved. That is a portion
of the momentum of the particle is associated with the electromagnetic field. The energy of the
particle is
E = T + eφ
(24)
since the magnetic field does not work on the system, because the force acts perpendicular to the
velocity.
Velocity Dependent Potentials-3
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