Line integral where a vector field is given in cylindrical coordinates

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The discussion focuses on evaluating a line integral of a vector field given in cylindrical coordinates, specifically along a half-circle curve centered at (0, 1). The user initially parameterizes the curve but encounters difficulties transforming the vector field from cylindrical to Cartesian coordinates. After some corrections, the parameterization is clarified, and the limits of integration are adjusted to reflect the correct bounds. There is uncertainty about the necessity of parametrization, but the user ultimately arrives at a potential solution for the integral. The conversation emphasizes the challenges of coordinate transformation in vector calculus.
goohu
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Homework Statement
see image
Relevant Equations
equation of circles; radius = x^2 + y^2
What I've done so far:

From the problem we know that the curve c is a half-circle with radius 1 with its center at (x,y) = (0, 1).

We can rewrite x = r cos t and y = 1 + r sin t, where r = 1 and 0<t<pi. z stays the same, so z=z.

We can then write l(t) = [x(t), y(t), z ] and solve for dl/dt.

The integral can be rewritten as integral A dot l(t) dt, with the limits as 0 and pi.Now everything would be fine if the vector field A was given in cartesian coordinates but its not. You could transform different coordinate systems but I can't figure it out. Could someone please show me how to start on the last steps?

I know how to transform specific coordinates but I'm having trouble transforming a whole function. If we can express A in cartesian form then we can use scalar multiplication in the last step to solve the problem.
 

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goohu said:
We can rewrite x = r cos t and y = r sin t, where r = 1 and 0<t<pi.
No, that does not put the centre of the arc at (0,1,0). Did you mean y=1+ r sin(t)?
 
yes, my bad.
 
I made a mistake during the parameterization.
t should be : ## -\pi / 2 < t < \pi / 2 ##

So the limits should be ## \int_\frac{-\pi}{2}^\frac{\pi}{2} A(t) ⋅ l(t) \ dt##
 
EDIT: scratch my last post. Maybe should stay in cylindrical. Still don't see why parametrize.
 
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I have my doubts about this one but I got zero for an answer.
EDIT: I think I at least have the right procedure even if I'm capable of math errors: $$ \int \mathbf A \cdot d\mathbf l = \frac { (8z + 2)} {3} $$.
 
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The book claims the answer is that all the magnitudes are the same because "the gravitational force on the penguin is the same". I'm having trouble understanding this. I thought the buoyant force was equal to the weight of the fluid displaced. Weight depends on mass which depends on density. Therefore, due to the differing densities the buoyant force will be different in each case? Is this incorrect?

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