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Mathematical Methods for Physicists: A concise introduction - Site Map

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VECTOR AND TENSOR ANALYSIS<br />

Proof:<br />

…2†<br />

Z b<br />

a<br />

… r†dl ˆ<br />

ˆ<br />

ˆ<br />

ˆ<br />

Z b<br />

a<br />

Z b<br />

a<br />

Z b<br />

a<br />

Z b<br />

I<br />

a<br />

S<br />

<br />

@<br />

@x ^i ‡ @<br />

@y ^j ‡ @ <br />

@z ^k …dx^i ‡ dy^j ‡ dz ^k†<br />

<br />

<br />

@ @ @<br />

dx ‡ dy ‡<br />

@x @y @z dz<br />

<br />

@dx<br />

@x dt ‡ @ dy<br />

@y dt ‡ @ <br />

dz<br />

dt<br />

@z dt<br />

<br />

d<br />

dt ˆ …b†…a†:<br />

dt<br />

@'<br />

@n<br />

ZV<br />

da ˆ r 2 'dV:<br />

Proof: Set ˆ 1 in Eq. (1.87), then @ =@n ˆ 0 ˆr 2<br />

Eq. (1.91).<br />

Z I<br />

…3†<br />

r'dV ˆ '^nda:<br />

V<br />

S<br />

…1:91†<br />

and Eq. (1.87) reduces to<br />

…1:92†<br />

Proof: In Gauss' theorem (1.78), let A ˆ 'C, where C is constant vector. Then<br />

we have<br />

Z<br />

Z<br />

r…'C†dV ˆ 'C ^nda:<br />

Since<br />

V<br />

r…'C† ˆr' C ˆ C r' and 'C ^n ˆ C …'^n†;<br />

S<br />

we have<br />

Taking C outside the integrals,<br />

Z<br />

C <br />

Z<br />

V<br />

Z<br />

C r'dV ˆ<br />

V<br />

S<br />

C …'^n†da:<br />

Z<br />

r'dV ˆ C …'^n†da<br />

S<br />

and since C is an arbitrary constant vector, we have<br />

Z I<br />

r'dV ˆ '^nda:<br />

…4†<br />

Z<br />

V<br />

V<br />

Z<br />

rBdV ˆ<br />

S<br />

S<br />

^n Bda<br />

…1:93†<br />

46

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