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Finally, the right-hand side of Equation 2.70 is converted back into vector notation to obtain the result
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.
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
Figure 2. 11 The Sum^ of^ Two^ Differential^ Volumes