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Introduction to vector and tensor analysis

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point in opposite direction). Consequently, the only contributions comes from<br />

the surface S of V .<br />

<br />

a(r) · dS ≈ <br />

<br />

a(r) · dSi<br />

(2.59)<br />

S<br />

i<br />

B(r0,i)<br />

Since each term on the rhs. of Eq. (2.58) equals a corresponding term on the<br />

rhs. of Eq. (2.59) the Gauss teorem is demonstrated.<br />

Gauss theorem is often used in conjunction with following mathematical<br />

theorem<br />

d<br />

dt<br />

<br />

V<br />

<br />

φ(r, t)dV =<br />

V<br />

∂<br />

φ(r, t)dV,<br />

∂t<br />

where t is time <strong>and</strong> φ is a time dependent scalar field (The theorem works in<br />

arbitrary spatial dimension). The two theorems are central in deriving partial<br />

differential equations for dynamical systems, in particular the so called continuity<br />

equations, linking a flow field <strong>to</strong> the time changes of scalar field advected<br />

by the flow. For instance if ρ(r, t) is a density <strong>and</strong> v(r, t), is the velocity field<br />

of a fluid then the vec<strong>to</strong>r j(r) = ρ(r)v(r) gives the density current. It can then<br />

by shown (try it) that under mass conservation then<br />

∂ρ<br />

+ ∇ · j = 0.<br />

∂t<br />

The divergence of a vec<strong>to</strong>r field therefore has the physical meaning of giving the<br />

net “outflux” of a scalar advected by the field within an infinitesimal volume.<br />

S<strong>to</strong>kes theorem<br />

S<strong>to</strong>kes theorem states that if S is the “curl analogue” of the divergence theorem<br />

<strong>and</strong> relates the integral of the curl of a vec<strong>to</strong>r field over an open surface S <strong>to</strong> the<br />

line integral of the vec<strong>to</strong>r field around the perimeter C bounding the surface.<br />

<br />

<br />

<br />

∇ × a (r) · dS = a(r) · dr (2.60)<br />

S<br />

Following the same lines as for the derivation of the divergence theorem the<br />

surface S can be divided in<strong>to</strong> many small areas Si with boundaries Ci <strong>and</strong> unit<br />

normals ni. For each small area one can show that<br />

<br />

(∇ × a) · niSi ≈ a · dr.<br />

Summing over i one finds that on the rhs. all parts of all interior boundaries<br />

that are not part of C are included twice, being traversed in opposite directions<br />

on each occasion <strong>and</strong> thus cancelling each other. Only contributions from line<br />

elements that are also part of C survive. If each Si is allows <strong>to</strong> <strong>to</strong> tend <strong>to</strong> zero,<br />

S<strong>to</strong>kes theorem, Eq. (2.60), is obtained.<br />

25<br />

C<br />

Ci

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