Calculating flux via divergence theorem.

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dustbin
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Homework Statement


Compute the flux of [itex]\vec{F}[/itex] through [itex]z=e^{1-r^2}[/itex] where [itex]\vec{F} = [x,y,2-2z]^T[/itex] and [itex]r=\sqrt{x^2+y^2}[/itex].

EDIT: the curve must satisfy [itex]z\geq 0[/itex].

Homework Equations


Divergence theorem: [tex]\iint\limits_{\partial X} \Phi_{\vec{F}} = \iiint\limits_X \nabla\cdot\vec{F}\,dx\,dy\,dz[/tex]

The Attempt at a Solution



For the given [itex]\vec{F}[/itex], we have [itex]\nabla\cdot\vec{F} = 0[/itex]. So isn't the flux just zero by the divergence theorem? I am confused because there is a hint saying that I should change the given surface to a simpler one.
 
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hi dustbin! :wink:
dustbin said:
For the given [itex]\vec{F}[/itex], we have [itex]\nabla\cdot\vec{F} = 0[/itex]. So isn't the flux just zero by the divergence theorem?

correct :smile:

but that's only for a closed surface …

so find another (simpler) surface that you can join to this surface to make a closed surface :wink:
 
Thanks for the tip tiny-tim! I should note that I forgot to put the restriction [itex]z\geq 1[/itex] on the given surface. I will think about your suggestion and post back!
 
Since [itex]X[/itex] must be a compact domain in [itex]\mathbb{R}^3[/itex], we must bound from below the region bounded above by the given surface. Since [itex]z\geq 1[/itex], setting [itex]1=e^{1-r^2}[/itex] gives the (simpler) surface [itex]x^2+y^2=1[/itex]. The union of this disc and the given surface form the boundary, [itex]\partial X[/itex], of a compact region [itex]X[/itex] of [itex]\mathbb{R}^3[/itex]. Hence we may now apply the divergence theorem.
 
I meant [itex]x^2+y^2 = 1[/itex] to be confined to the plane [itex]z=1[/itex]. Thank you! :redface:

To take it all the way:

Call [itex]S_1[/itex] the given surface and [itex]S_2[/itex] the new surface so that [itex]S_1\cup S_2 = \partial X[/itex]. Observe that [itex]\Phi_{\vec{F}} = x\,dy\wedge dz - y\,dx\wedge dz + (2-2z)\,dx\wedge dy[/itex]. Parametrize [itex]S_2[/itex] via [itex]x=r\cos\theta, \ y=r\sin\theta, \ z=1[/itex] such that [itex]\theta \in [0,2\pi) \ , \ 0\leq r \leq 1[/itex]. Call this parametrization [itex]\gamma[/itex]. Then [itex]\Phi_{\vec{F}}(\gamma) = (2-2)r = 0.[/itex] Applying the theorem, we have

[tex] 0 = \iiint\limits_X \nabla\cdot\vec{F}\,dx\,dy\,dz = \iint\limits_{S_1} \Phi_{\vec{F}} + \iint\limits_{S_2} \Phi_{\vec{F}} = \iint\limits_{S_1} \Phi_{\vec{F}}.[/tex]

Thus the flux of [itex]\vec{F}[/itex] across [itex]S_1[/itex] is 0.
 
The way that I did it is the only way I know to calculate flux. :redface:
 
dustbin said:
The way that I did it is the only way I know to calculate flux. :redface:

flux is just F·ñ

why do you need to convert to polar coordinates to calculate what (on this surface) is obviously 0 ?? :wink:
 
Is [itex]\hat{\textbf{n}}[/itex] the orienting normal?
 
I see. The text I use doesn't use standard notation, so when I look at other books or sites about vector calculus, I feel hopelessly lost with the notation!

Thank you for your help :-)