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mathematical_physics_2007_17.pdf, Study Guides, Projects, Research of Mathematical Physics

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34
DIFFERENTIAL AND INTEGRAL OPERATIONS
(2.70)
Finally, the right-hand side of Equation 2.70 is converted back into vector notation
to obtain the result
v
XVXV=V(V-5)
-v2V.
(2.7
1)
Notice that the Laplacian operator can act on both vector and scalar fields.
In
Equation
2.68, the Laplacian operates on a scalar field to product a scalar.
In
Equation 2.71,
it
operates on a vector field to produce a vector.
-
2.4
INTEGRAL DEFJNITIONS
OF
THE
DIFFERENTLAL
OPERATORS
In Equations 2.25,2.27, and 2.29, we provided expressions for calculating the gradi-
ent, divergence, and curl. Each of these relations is valid only in a Cartesian coordinate
system, and all are in terms of spatial derivatives
of
the field. Integal definitions of
each of the differential operators
also
exist. We already derived one such definition
for the curl in Equation 2.63.
In
this
section,
we
present similar definitions for the
gradient and divergence,
as
well
as
an alternate definition for the curl. Their deriva-
tions, which are all similar to the derivation
of
Equation 2.63, are in most introductory
calculus texts. We present only the results here.
The gradient of a scalar field at a particular point can be generated
from
(2.72)
where
V
is a volume that includes the point of interest, and
S
is the closed surface
that surrounds
V.
Both
S
and
V
must be
shrunk
to infinitesimal size for
this
equation
to hold.
To get the divergence of a vector field at a point, we integrate the vector field over
an
infinitesimal surface
S
that encloses that point, and divide by the infinitesimal
volume:
We already derived the integral definition
(2.73)
(2.74)
which generates the curl.
This
definition is a bit clumsy because it requires the
calculation of three different integrals, each with a different orientation of
S,
to get
all three components of the curl. The following integral definition does not have this
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34 DIFFERENTIAL AND INTEGRAL OPERATIONS

Finally, the right-hand side of Equation 2.70 is converted back into vector notation to obtain the result

v X V X V = V ( V - 5 ) -v2V. (2.7 1)

Notice that the Laplacian operator can act on both vector and scalar fields. In Equation

2.68, the Laplacian operates on a scalar field to product a scalar. In Equation 2.71, it operates on a vector field to produce a vector.

2.4 INTEGRAL DEFJNITIONS OF THE DIFFERENTLAL OPERATORS

In Equations 2.25,2.27, and 2.29, we provided expressions for calculating the gradi- ent, divergence,and curl. Each of these relations is valid only in a Cartesian coordinate system, and all are in terms of spatial derivatives of the field. Integal definitions of each of the differential operators also exist. We already derived one such definition for the curl in Equation 2.63. In this section, we present similar definitions for the gradient and divergence, as well as an alternate definition for the curl. Their deriva- tions, which are all similarto the derivation of Equation 2.63, are in most introductory calculus texts. We present only the results here. The gradient of a scalar field at a particular point can be generated from

where V is a volume that includes the point of interest, and S is the closed surface that surrounds V. Both S and V must be shrunk to infinitesimal size for this equation to hold. To get the divergence of a vector field at a point, we integrate the vector field over an infinitesimal surface S that encloses that point, and divide by the infinitesimal volume:

We already derived the integral definition

which generates the curl. This definition is a bit clumsy because it requires the calculation of three different integrals, each with a different orientation of S, to get all three components of the curl. The following integral definition does not have this

THE THEOREMS 35

problem, but it uses an uncommon form of the surface integral:

2.5 THE THEOREMS

The differential operators give us information about the variation of vector and scalar fields on an infinitesimal scale. To apply them on a macroscopic scale, we need to introduce four important theorems. Gauss’s Theorem, Green’s Theorem, Stokes’s Theorem, and Helmholtz’s Theorem can be derived directly from the integral definitions of the differential operators. We give special attention to the proof and discussion of Helmholtz’s Theorem because it is not covered adequately in many texts.

2.5.1 Gauss’s Theorem

Gauss’s Theorem is derived from Equation 2.73, written in a slightly different form:

(2.76)

In this equation, the closed surface S completely surrounds the volume dr, which we have written as an infinitesimal. Equation 2.76 can be applied to two adjacent differential volumes dr1 and d72 that have a common surface, as shown in Figure 2.11:

V. A d r 1 + V - A d r 2 = dZF-%+ (2.77)

The contributions to the surface integral from the common surfaces cancel out, as depicted in the figure, so Equation 2.77 can be written as

d izdrr.A.

Figure 2. 11 The Sum^ of^ Two^ Differential^ Volumes