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9—Vector Calculus 1 225

This agrees with equation (9.15).
Similarly you can use the results of problem8.15to find the derivatives of the corresponding
vectors in spherical coordinates. The non-zero values are


dˆr



=φˆsinθ


dθˆ



=φˆcosθ


dφˆ



=−rˆsinθ−θˆcosθ


drˆ



=θˆ


dθˆ



=−ˆr (9.30)


The result is for spherical coordinates

∇.~v=


1

r^2


∂(r^2 vr)


∂r


+

1

rsinθ


∂(sinθvθ)


∂θ


+

1

rsinθ


∂vφ


∂φ


(9.31)


The expressions for the curl are, cylindrical:

∇×~v=ˆr


(

1

r


∂vz


∂φ



∂vφ


∂z


)

+φˆ


(

∂vr


∂z



∂vz


∂r


)

+ˆz


(

1

r


∂(rvφ)


∂r



1

r


∂vr


∂φ


)

(9.32)


and spherical:


∇×~v=ˆr


1

rsinθ


(

∂(sinθvφ)


∂θ



∂vθ


∂φ


)

+θˆ


(

1

rsinθ


∂vr


∂φ



1

r


∂(rvφ)


∂r


)

+φˆ


1

r


(

∂(rvθ)


∂r



∂vr


∂θ


)

(9.33)


9.7 Identities for Vector Operators
Some of the common identities can be proved simply by computing them in rectangular components.
These are vectors, and if you show that one vector equals another vector it doesn’t matter that you
used a simple coordinate system to demonstrate the fact. Of course there are some people who quite
properly complain about the inelegance of such a procedure. They’re called mathematicians.


∇.∇×~v= 0 ∇×∇f= 0 ∇×∇×~v=∇


(

∇.~v


)


(

∇.∇

)

~v (9.34)


There are many other identities, but these are the big three.



~v.dA~=



d^3 r∇.~v



~v.d~r=



∇×~v.dA~ (9.35)


are the two fundamental integral relationships, going under the names of Gauss and Stokes. See chapter
13 for the proofs of these integral relations.


9.8 Applications to Gravity
The basic equations to describe the gravitational field in Newton’s theory are


∇.~g=− 4 πGρ, and ∇×~g= 0 (9.36)


In these equations, the vector field~gis defined by placing a (very small) test massmat a point and


measuring the gravitational force on it. This force is proportional tomitself, and the proportionality


factor is called the gravitational field~g. The other symbol used here isρ, and that is the volume mass

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