. This product rule is shown below in general curvilinear coordinates, where is a contravariant basis vector, and where denotes differentiation with respect to the the coordinate in the basis, and where means . Evaluating the left-hand side of the identity to be proved yields
where the first line holds by the definition of divergence of tensor, the second line by the product rule, the third line by the distributive property, the fourth line by the definition of the outer product, and the last line by the definitions of the gradient and divergence of a vector. Note: This was a homework problem in Ref. [8].
Below is a less general version of the proof, included for readers unfamiliar with Ricci calculus. In orthonormal index notation, the left-hand side of the identity to be proved in one line, by the product rule:
- for time-harmonic and .
To show this, suppose and . Then, since ,
Taking the time derivative of the product yields
The time-average of having angular frequency , where is the period, is defined as
Thus the time average of Eq. is
since . Thus, at least for time-harmonic functions, . Since the theory on this website only involves time-harmonic functions, this property will be exploited when deriving the acoustic radiation stress tensor.
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, where rank-2 tensors on this website are denoted by being underlined. The left-hand side of the identity is manipulated:
The first line holds by the definition of the divergence of a tensor, the second line holds by the product rule, the third line by the commutative property of multiplication, and the fourth line by the definition of the divergence of a tensor and vector.
For a less general version of this proof, appeal to orthonormal index notation. As in Item 1, the statement is proved in one line by the product rule:
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For two time-harmonic functions and represented by the real parts of the complex-valued functions and (where and ), the time average of their product, , is given by , where "" denotes "real part".
To show this, note that and . thus
Since , Eq. becomes (by letting and )
Noting that , Eq. becomes
The time-averaging operation amounts to an integral, which is a linear operation. Thus Eq. becomes
The first term on the left-hand side is 0. Meanwhile, the second term does not depend on time, and therefore its time average is itself:
Noting that is , which by the relations and is , Eq. becomes
where the final equality holds by noting that .
A consequence of this relation is that the time-averaged intensity of a time-harmonic acoustic field is as can be seen by letting and in Eq.
- , where is the position vector. Note that the gradient of a vector field is defined by {See Eq. (1.4.10) of Ref. [8]}
where is the contravariant basis vector. Evaluating Eq. for yields
But {See Eq. (1.3.4) of Ref. [8]}, so Eq. becomes
The right-hand side of Eq. is simply the identity tensor, as is shown by considering an arbitrary vector . By the definition of the identity tensor,
Dotting Eq. by on both sides results in
Since the basis and its dual are orthogonal,
Multiplying both sides of Eq. by results in
In view of Eqs. and , , so Eq. becomes
where the definition of the outer product has been used in the second equality. Since is arbitrary,
Thus , and Eq. becomes
proving the first of the two desired equalities. To prove the second of the two equalities, note that for two arbitrary vectors [which equals ] equals [which equals ], one can use the definition of the transpose to write
showing that . Thus Eq. can be transposed and equated to itself, i.e., .
- . Introduce auxiliary vectors and , and invoke the definition of the transpose:
By the definiton of the outer product, the right-hand side equals . Since is a scalar, it the right-hand side becomes by the associative property. Again invoking the definition of the outer product yields
Since and are arbitrary, it has been shown that .
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. This is proved by invoking auxiliary vectors and and utilizing the definition of transpose in the first, third, and fourth lines below,
where the composition property has been used in the second and final lines above. Since and are arbitrary, the proof is complete.
, known as the vector triple product. It is straightforward to prove this in index notation for orthonormal bases:
Since this applies to , the above statement becomes , as desired.
Definition of the axial vector of a skew-symmetric tensor : is defined in terms of the skew-symmetric tensor as
To show this, note that the skew tensor satsfies
where Item 6 has been used in the second equality. By comparison of the above to Eq. , it can be seen that
Since any skew-symmetric tensor can be built on the basis of , all skew-symmetric tensors have an axial vector satisfying Eq. .
Equation is defined only in terms of a skew-symmetric tensor . To extend the definition of the axial vector to any tensor , let
This discussion was adapted from Ref. [8], pp. 18 and Eqs. (1.2.16) and (1.2.17).
- For differentiable tensor and vector fields and in a region with boundary having outward normal , a consequence of the divergence theorem is
where the axial vector of a tensor is defined in Item 7. This identity is found in Ref. [8], Exercise 1.5-2.
- . According to Ref. [8] [See Eq. (1.4.36)], this identity is in fact definitional and is regarded as the "generalized vector product" (Compare it to the vector triple product in Item 6). Noting that allows for this identity to be equivalently written as